“Every piece of land has our blood”: Pataxó people face violence and abandonment in the far south of Bahia
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leaders are calling for help — and justice.
“This land has been ours since before 1500. We are not invading anyone’s property. Every corner of this territory is sacred. It is where our enchanted ones live,” said the Suruí Pataxó chief to the Socioenvironmental Institute (ISA), shortly after his people have been targeted by Operation Pacificar
when 150 civil and military police officers from Bahia entered the Barra Velha do Monte Pascoal TI to serve 12 arrest warrants and seven search and seizure warrants
after a request from the State Public Defender's Office
The remaining four have not yet had their request granted
the Civil Police stated that the action sought to dismantle armed groups of “supposed indigenous people” who
“under the pretext of acting in the ‘retaking’ of their ancestral territories
act with violence and serious threats against workers and rural landowners”.
There are several of our people with arrest warrants
That we took the land to steal things from the ruralists,” he explains
“But the story is different: we are not invading anyone’s property
which is ancestral land of the Pataxó community,” says the chief
“The public and political agents involved in this operation must be investigated and held accountable; including for their failure to observe and respect our rights
As well as for the violations against the rights of children and the most vulnerable people
victims of the violence we are suffering,” reads an excerpt from the letter
the Pataxó are back in Brasília to participate in the 21st Free Land Camp (ATL) and denounce the violence that afflicts them
“Let’s dance Pataxó / For the relative who died / We thank father Tupã / For the view he gave us,” they sang as they occupied the main tent of the camp that began on Monday (07/04)
was eagerly awaited by the Pataxó delegation that went to Brasília — but it ended in frustration and revolt
to ask the government to do what the Constitution requires
And we left there with more pain,” says indigenous leader Uruba Pataxó
the meeting with the minister was marked by a lack of listening
The leader says that the minister arrived late
stayed for a short time and seemed more concerned with another commitment he had after the meeting than with the murders and conflicts reported by the Pataxó
“He said he could only stay for 30 minutes because he had an appointment
He went straight to saying that he couldn’t sign the demarcation
that it could end up in court,” said Uruba
This Tuesday (08/04), the 6th Chamber of the Federal Public Ministry (MPF) released a technical note recommending that the ministry led by Lewandowski immediately sign the declaratory orders for three Indigenous Lands in the South of Bahia
including Barra Velha do Monte Pascoal and two others belonging to the Tupinambá people
Violence against the Pataxó was also the subject of a meeting of the National Human Rights Council (CNDH)
in addition to recommending the declaration of the area by the MJSP
indicated the deployment of the National Force to the region
at the March meeting the minister justified the government's inertia in advancing the demarcation process by stating that the invaders of Indigenous Lands are very influential people with great economic power
capable of hiring the best lawyers to reverse any administrative act
“I told him that our land is bathed in blood
and that what should rule Brazil is the Constitution
The Barra Velha Indigenous Territory was administratively demarcated in 1981 and ratified in 1991 with an area of just 8.627 hectares — where eight villages are currently concentrated
the Pataxó have claimed that the area does not correspond to the entirety of their traditional territory
According to anthropologist José Augusto Sampaio
this first demarcation did not respect legal criteria nor did it take into account the history and territoriality of the Pataxó
Brazil was still under a military dictatorship
and the process was led by two agencies linked to the regime: the National Foundation for Indigenous Peoples (FUNAI)
and the now-defunct Brazilian Institute for Forestry Development (IBDF)
“The delimitation was decided by Funai and the IBDF
it does not meet the constitutional requirements of what constitutes Indigenous Lands
The area was defined for administrative convenience
not based on technical or historical criteria
who is a professor at the State University of Bahia (Uneb) and president of the board of directors of the National Association for Indigenous Action (Anaí)
Signed in 1980, this agreement between federal agencies involved the overlapping of Barra Velha by Monte Pascoal National Park — created in 1961
when the Pataxó were restricted to an area of just 210 hectares
Everything was done without respecting the rights of indigenous peoples
as if they were dealing with common squatters,” explains Sampaio
According to an article by anthropologist Sheila Brasileiro published by ISA in 2004
the attempt to regularize the Barra Velha Indigenous Land
contravening the indigenous legislation of the time and resulting in half of the territory traditionally occupied by the Pataxó – already identified by researchers from the Federal University of Bahia (UFBA) – being ceded to the National Park
The Pataxó were left with a land of sandy marshes around Monte Pascoal and a long history of disputes with environmental agencies.
Remember: The Pataxó and Monte Pascoal
“Indigenous people suffered many forms of violence at the hands of IBDF employees
These violations have left their mark on generations,” explains Milene Maia Oberlaender
coordinator of the ISA Socio-Environmental Policy and Law Program.
who worked for eight years as manager of the Monte Pascoal National Park
says that families were prevented from harvesting their own crops
which led to hunger among a large part of the Pataxó population
“They were forced to collect food at night
so that they would not be ‘caught’ by the inspectors; they felt like thieves in their own home
These psychological attacks still scar the Pataxó today,” she explains
It was only after the promulgation of the 1988 Constitution
which explicitly recognized the original rights of indigenous peoples over their traditional territories
with the support of the Federal Public Ministry (MPF) and the university
the process of regularizing their true land
with the Pataxó retaking the Monte Pascoal National Park and actions by the MPF
Funai finally began the technical studies necessary to repair past deeds and correct the boundaries of the Barra Velha Indigenous Territory.
The work was completed in 2008, resulting in the identification of the Barra Velha do Monte Pascoal IT, an area of 52.748 hectares, distributed across the municipalities of Itabela, Itamaraju, Prado and Porto Seguro. technical report confirmed that the area corresponds to the territory of traditional occupation of the Pataxó
encompassing and significantly expanding the limits of the portion of land demarcated in 1991
Approved and published by the presidency of Funai
the identification and delimitation report was sent to the Ministry of Justice for the issuance of the declaratory ordinance — but it got stuck there
due to the change in political stance in the Temer and Bolsonaro governments regarding the demarcation of Indigenous Lands
the Pataxó have once again put pressure on the process
The process reached the Ministry of Justice in November 2023
after being approved by the Ministry of Indigenous Peoples (MPI)
In 2024, a decision of the Federal Court determined that Funai and the Federal Government complete the procedures for reviewing the boundaries and demarcating the Barra Velha do Monte Pascoal TI within two years
no concrete measures have been taken to date
“This land has been on the minister’s desk for over a year
He just keeps stalling,” concludes Sampaio
The land is ours and we are already occupying it
The State needs to do what the Constitution requires,” says Chief Suruí
“They took our relatives away with bullets
Both lived in a village on Fazenda Condessa
a rural property located within the boundaries of the same TI
was killed with a shot to the back of the head during an attack in the same territory.
The Comexatiba IT, also known as Cahy-Pequi, is a territory traditionally occupied by the Pataxó that faces the same logic of exclusion and racism: deforestation, illegal subdivision and the State's failure to finalize the demarcation. Learn more.
There are constant reports of armed sieges imposed by gunmen, which include burning houses and intimidation against women. The land also overlaps with a Conservation Unit, the Discovery National Park.
These murders are part of an even larger number. A document addressed to Lewandowski by Deputy Attorney General Eliana Peres Torelly de Carvalho, obtained by Sumaúma
74 Pataxó people have been murdered in the extreme south of Bahia
Only then will these conflicts cease,” emphasizes Suruí
Faced with the historical omission of the Brazilian State and the escalation of violence suffered in the territories, the Pataxó leaders turned to the international sphere. In March 2025, the Council of Chiefs of the Barra Velha do Monte Pascoal Indigenous Land submitted to the United Nations (UN) a complete dossier denouncing murders
connivance of local authorities and the halt in land demarcation
the repression of Pataxó self-demarcations is not a coincidence
but the result of actions orchestrated by groups with a strong economic interest in maintaining illegal possession of the lands
Among the main actors opposing the demarcation of Pataxó lands are farmers
land grabbers and militiamen who work in collusion to prevent the advancement of self-demarcation
indigenous leaders are constantly threatened by representatives of local agribusiness and by gunmen hired to intimidate and attack the communities.
The document points out that sectors of the State — including public servants
representatives of the judicial system and bodies protecting indigenous peoples — have been silent or even actively acting against indigenous peoples
favoring private interests under the guise of legality
armed militias linked to drug trafficking have consolidated a parallel power structure in the most vulnerable areas of the territory
These groups impose fear through aggression
and attempt to control the daily life of the villages
including interfering in the cultural and spiritual life of the Pataxó
and many families live in a constant state of alert,” Uruba denounces
The document demands that the federal government be held accountable and asks for international support to ensure the protection of the leaders and the completion of the demarcation process
“We are tired of asking the government for help
The UN was the last way we found to say: they are killing our people
remains in the hands of the farmers,” Uruba Pataxó complained
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The escalation of violence in Brazil’s northeastern region with the murders of two young Pataxó Indigenous leaders this week triggered the newly created Ministry of Indigenous Peoples to set up a crisis office to monitor land conflicts in the region
17-year-old Nawir Brito de Jesus and 25-year-old Samuel Cristiano do Amor Divino were shot dead in the district of São João do Monte
between the towns of Itabela and Itamaraju
“It is unacceptable that Indigenous people continue to be persecuted and threatened within their own territories. This crime cannot go unpunished,” Minister of Indigenous Peoples Sonia Guajajara said in a news release. She said the ministry will work with the Ministry of Justice and other entities
including the country’s Indigenous affairs agency
the Federal Public Ministry and authorities in Bahia “to guarantee the rigorous investigation and punishment of the criminals
the protection of the Pataxó people.”
The crimes occurred when the two Indigenous leaders were returning on a motorcycle to the Condessa farm, a resettlement established earlier in the month amid ownership disputes in the region, the Indigenous Missionary Council (CIMI), an advocacy group affiliated with the Catholic Church, said in a news release
is located within the limits of the Barra Velha Indigenous Territory
an area recognized in 2008 as being traditionally occupied by the Pataxó people but has awaited full demarcation since then
In September, Gustavo Silva da Conceição, a 14-year-old Pataxó boy, was killed and another Pataxó boy
was wounded in the arm by gunfire reportedly by gunmen as group of Indigenous Pataxó sought to retake land within the Comexatibá Indigenous Territory
said “it was immediately determined the priority in the investigation,” with civil police teams going on site to conduct investigations in search of the perpetrators of the crime and the Military Police reinforcing the task force teams in the region
the state’s superintendent of policies for Indigenous peoples
the state management is seeking articulation with the federal government
which is responsible for the demarcation of Indigenous territories
We have been in the area listening to the communities and making ourselves available to the leaders
we are drawing up plans to manage this conflict,” she said in a news release
the Federal Public Ministry in Bahia said it is investigating the actions of an armed group against the Indigenous community through a previously opened procedure
It added that it has requested information from the government of Bahia and the Ministry of Justice about what measures have been or will be adopted to safeguard the integrity of the communities living in the Barra Velha Indigenous Territory
The Federal Police in Bahia did not respond to Mongabay’s requests for comment
Violence against Indigenous people this year is not isolated to Bahia
two Indigenous Guajajara were shot in the head in northeastern Maranhão state
as confirmed by the state’s civil police in an emailed statement
The civil police said the two attempted murders are being investigated by the police station in the town of Arame and accompanied by the Federal Police
It added that it has already heard statements from witnesses and family members of the victims who “are still in a serious condition in the ICU of the Municipal Hospital of Grajaú.” So far
The Federal Police said the case is being investigated by the civil police. The Federal Public Ministry in Maranhão did not respond to Mongabay’s requests for comment.
Maranhão was the stage of three murders and one attempted murder of Guajajara Indigenous
Unknown perpetrators reportedly ran over Jael Carlos Miranda Guajajara
in a vehicle and killed him in Arame; gunmen also shot dead Antônio Cafeteiro Silva Guajajara
Janildo Oliveira Guajajara was shot and killed by unknown assailants in an apparent ambush
where the perpetrators also shot and injured a 14-year-old Guajajara boy
more than 50 Guajajara individuals have been killed in Maranhão
with none of the alleged perpetrators ever going on trial
Banner image: A member of the Pataxó community. Image by Karenalmeid via Wikimedia Commons (CC BY-SA 4.0)
Karla Mendes is a staff contributing editor for Mongabay in Brazil. Find her on Twitter: @karlamendes
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Indigenous Brazilians demand justice as 4 killed in escalating violence
With plantation takeover, Brazil’s Indigenous Pataxó move to reclaim their land
The “fortress conservation” model is under pressure in East Africa
as protected areas become battlegrounds over history
and global efforts to halt biodiversity loss
Mongabay’s Special Issue goes beyond the region’s world-renowned safaris to examine how rural communities and governments are reckoning with conservation’s colonial origins
and trying to forge a path forward […]
There are wide lessons to be learned from the controversy over the origins of the enigmatic Cretaceous lacustrine carbonate reservoirs of offshore Brazil
Figure 1: Location of Santos and Campos Basins
Much of the interest in Brazil’s autumn bid rounds will again be on the Santos and Campos Basins with their lacustrine carbonate reservoirs (Figure 1)
In the Santos Basin over 30 discoveries have been made in such reservoirs since the Tupi (now Lula) discovery in 2006
with combined recoverable reserves estimated at >30 Bboe in the Cretaceous (Aptian) Barra Velha Formation (known as the ‘Microbialite’)
Discoveries have also been made in the adjacent Campos Basin
where the same unit is known as the Macabu Formation
The Barra Velha Formation can reach thicknesses of over 550m
with some wells producing in excess of 28,000 bopd
It occurs beneath a cover of marine salt (the Ariri) and represents a later rift-to-sag interval of South Atlantic opening
Deeper in the section are the mainly Barremian coquina (shelly limestone) reservoirs of the Itapema Formation
well documented from the Campos Basin where they constitute the Coqueiros
The Barra Velha and its correlatives represent a lake system that covered an area of at least 335,000 km2: a similar size to the present-day Caspian Sea
While debate continues over the origins of the coquina reservoirs
the main controversy relates to the Barra Velha and its equivalents
The implications of the different interpretations for this unit are quite fundamental in terms of both exploration strategies and reservoir modelling
which was clearly associated with relatively deep lakes during active rifting
the Barra Velha was deposited during the latter stages of rifting but shows clear evidence of syn-depositional control on stratal patterns
Localized deformation continued through the later ‘sag’ phase
Figure 2a: Main components of the Barra Velha reservoirs: Calcite shrubs with inter-shrub porosity (blue) and some mouldic porosity within the shrubs
Figure 2b: Main components of the Barra Velha reservoirs: Same image under cross-polarized light with distinctive sweeping extinction patterns reflecting the fibrous microstructure
Figure 2c: Main components of the Barra Velha reservoirs: Spherulites set in a talc-stevensite matrix within which are dolomite crystals and elongate bridge-like dolomites
Figure 2d: Main components of the Barra Velha reservoirs: Spherulites with pore spaces
after the dissolution of the stevensite; the internal structure of the spherulites is clearly seen in cross-polarized light
The Barra Velha carbonates are very simple in their composition
They consist of just two main primary components (Figure 2): millimeter to centimeter-sized crystalline
fibrous calcitic shrub-like structures resembling features found in present-day abiotic travertines (thermal spring deposits); and millimeter-sized spherulites made of fibrous calcite
resulting in much reduced reservoir quality
they can be porous and constitute the most widespread reservoir facies
the in-situ examples can also be non-reservoir if the carbonate features occur within magnesium-silicate matrices (talc-stevensite)
What is unique about these reservoirs is that some of the clays
which initially formed as gels precipitated out of the lake waters and were deposited on the lake floor
later dissolved to produce a previously unrecorded type of mouldic porosity
some microbial carbonates occur but represent very little of the formation in terms of thickness
Although many academic researchers have interpreted the spherulites as probably microbial in origin
to date no actual evidence has been presented to justify that conclusion
Finely laminated carbonate muds formed as thin units during deepening events in the lakes caused by increased run-off
bringing in fresher waters as indicated by fish and invertebrate remains
In deeper parts of the lakes somewhat different laminites
There are meter-scale cyclic packages with thin fish-bearing laminites
overlain by in situ shrub units (Figure 3)
These have been interpreted as reflecting freshening and deepening of the shallow lakes by run-off to produce the laminites
a view supported by geochemical studies using C and O stable isotope analyses as well as thermodynamic modeling
The occurrence of what was originally stevensite suggests the pH of these alkaline lakes likely exceeded 10
and the surprising rarity of microbial carbonates implies that the pH may have been even higher during the evaporation phases
Figure 3: Shallow lake geological model for the Barra Velha Formation based on a tilt-block setting
On the gentler dip slopes localized wave-dominated shorefaces developed with possible spit complexes
Coarser sediments accumulated on the scarp slopes
Meter-scale cycles developed locally as the shallow lakes expanded with increased rainfall
when the carbonates and magnesium-silicates formed
Mound-like features occasionally developed in Santos Basin
(Based on multiple sources including Barnett et al.
Why should the Barra Velha and its equivalents be so unique when there are many carbonate-bearing rift successions in the geological record
The extreme thinning of crust during the opening of the South Atlantic may have led to exhumation of the mantle
creating hydrothermal conditions linked to serpentinization
although there is no geochemical evidence for elevated temperatures in the lakes and 87Sr/86Sr data does not indicate a significant input from the alteration of the mantle or ocean basalts
More intriguing is the possibility that the extreme alkalinity in the lakes was due to high CO2 input
The current controversy over the Barra Velha Formation involves two distinct interpretations
The first was the ‘top-down’ microbialite-platform model
This uses seismic data to identify high relief platforms with seemingly hundreds of meters of relief
which have been compared to present-day and older marine carbonate platforms
The attribution of the Barra Velha carbonates to a microbial origin has led to some companies making direct analogies with the high relief Carboniferous marine microbial platforms of the Pre-Caspian basin in Kazakhstan
where marine carbonate platforms are differentiated into margins (commonly the preferred targets for exploration) and protected interior facies
Some companies have developed reservoir models based on this concept
but there are no analogs for the key rock types in the Barra Velha and
there is currently little evidence for the carbonates being largely microbial
The alternative ‘bottom-up model’ for the Barra Velha was based on the recognition that no viable analogs have been identified
The strategy was to start by understanding the basic components making the reservoir rock and assessing them using basic science
such as establishing the chemical conditions in which the unusual mineral suite formed
combined with integrating crystal growth data
multiple interpretations were deliberately sought
modified and rejected as more data allowed a clearer understanding of the chemical environment
Only once the fundamental controls were understood
the main conclusion being that the Barra Velha formed in shallow lakes
was the seismic data evaluated; without information on lacustrine carbonate seismic facies or marine analogs
the seismic-first approach was considered unjustified
running de-risking workflows on the seismic features also showed little likelihood that they were analogous to marine carbonate build-ups
Many high relief features were subsequently interpreted as reflecting post-Barra Velha
a package in the uppermost 30m of the formation characterized by a series of prominent spikes on the gamma log
The carbonates in this interval contain a series of very distinctive cycles
including all the typical Barra Velha rock types as well as clear microbial carbonates and reliable water depth indicators proving a very shallow water origin
correlatable for 180km across the Santos Basin
were affected by hundreds of meters of differential local displacement prior to the main phase of salt deposition (Figure 4)
Figure 4: West-east correlation across the Santos Basin showing the unit at the top of the Barra Velha Formation known as ‘Lula’s Fingers’
Its thickness varies from 20.8 to 28.5m (mean 24.3m)
within which 9 gamma-defined cycles (mean thickness 2.7m) can be identified
These comprise shallowingupwards cycles defined by basal laminites
These cycles are well sampled and the facies are very similar in all wells
and include a range of unequivocally shallow water sediments
Even though these cycles were deposited at comparable water depths they are now separated by over 1 km of vertical relief
the highly unusual composition of the lacustrine carbonate reservoirs in the South Atlantic are especially challenging
Interpreting these reservoirs has presented a challenge to the accepted wisdom based on marine carbonate analogs and has required a bottom-up approach relying on first understanding the chemistry of extreme lake environments
which were heavily influenced by highly thinned crust and the effects of the mantle
and then seeking a wider range of explanations for the seismic features
Resolving this controversy has huge implications for future exploration and development programs in the wider region
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Brazil (AP) — Brazil President Luiz Inácio Lula da Silva on Friday granted official recognition of nearly 800 square miles of Indigenous lands
following through on a campaign promise in a move that also protects critical Amazon rainforest from commercial exploitation
the world’s largest tropical forest and an important carbon sink that helps moderate climate change
The total area of recognized lands in the biome is 161,500 hectares (620 square miles)
Lula’s action was welcomed by the Indigenous movement
but not without some frustration that it was limited in size
his government had pledged to create 14 new territories in the short term
At an encampment of Indigenous people in capital Brasilia
Lula addressed a packed crowd that included workers from the federal government’s Indigenous affairs agency
who chanted and held banners during the ceremony
The encampment itself includes hundreds of tents on the city’s main esplanade with Indigenous people of various ethnicities
sell handicrafts and hold political demonstrations
READ MORE: Bolsonaro hands over undeclared jewels to Brazilian authorities
“We are going to legalize Indigenous lands
because it has to go through many hands,” Lula said
“I don’t want any Indigenous territory to be left without demarcation during my government
executive coordinator at Indigenous people’s organization Apib
called the demarcation a welcome shift after four years of threats and invasions targeting Indigenous territories under Lula’s predecessor Jair Bolsonaro
it is a very significant process of restarting
there are still other lands that can be advanced,” he said
Among lands that missed out was the Barra Velha territory of the Pataxó people in southern Bahia state
that we helped build” must demarcate their land as soon as possible to prevent invasions by outsiders
Already there are conflicts involving agribusiness and land-grabbers
Atxuab said he has met with the Indigenous Peoples minister — a newly created position under Lula’s government — but has not been given any date for his land’s demarcation
The largest new area is located in the Amazonas state
The Nadöb people’s Uneiuxi Indigenous Territory has been expanded by 37% to 554,000 hectares (2,100 square miles) of primary rainforest
It is in a remote area — from the main village
it takes four days to travel to the closest city in a low-powered motor boat
the most common mode of transportation in the region
“The demarcation will make the Nadöb people feel safe and protected within our territory
like our ancestors,” chief Eduardo Castelo
told The Associated Press in a phone interview
“We don’t want the impact of the whites on our territory.”
Indigenous demarcation had been halted since 2018 following Bolsonaro’s promise to the agribusiness sector
Studies have shown that Indigenous-controlled forests are the best preserved in the Brazilian Amazon. But deforestation grew by 195% between 2019 and 2021 in comparison with the four previous years, according to a recent study published in the journal Nature. This destruction has been largely caused by non-Indigenous people
The Amazon rainforest covers an area twice the size of India and is a crucial buffer against climate change as it absorbs a significant amount of carbon dioxide
has caused almost half of its carbon emissions
The eastern Amazon’s destruction is so extensive that it has now become a carbon source instead of a carbon sink for the Earth
His government also created the Ministry of Indigenous Peoples
responding to a demand from the grassroots movement
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The violence the Pataxó are experiencing is emblematic of what Indigenous peoples are facing in the country
from the south of Brazil to the northeast to the northern Amazonian region
The crime occurred when the two young residents of Barra Velha Indigenous Land were traveling to a farm in a contested region claimed by the Pataxó people
Barra Velha is the site of intense conflicts with local ranchers
as Indigenous communities claim the region as their land
Chief Zeca Pataxó stated that “the situation certainly has to do with our process of retaking our lands.”
This type of brutality affects all Indigenous peoples in the country and is a consequence of the climate of violence and impunity fostered by the Bolsonaro administration
with major implications for Indigenous peoples and their lands
The response by the federal government under President Lula da Silva is notable because government agencies are now proactive in responding to these attacks
According to Eloy Terena
Executive Secretary of the Ministry of Indigenous Peoples
an Emergency Office was created to monitor the conflicts in the region
With this office and the combined efforts of various ministries and the government of Bahia state
they have committed to monitoring the investigations and response measures
The president of Brazil’s National Foundation of Indigenous Peoples (FUNAI)
expressed her solidarity with the Pataxó people for the loss of the two youths
“The situation of violence in the south of Bahia needs to be stopped urgently,” Wapichana said
stating that she asked FUNAI to carry out “due monitoring of the case
with support and protection from the federal police.” “In the same way
I requested measures to ensure the protection of the Indigenous peoples of this region of Bahia and measures to guarantee that justice is served,” she concluded
Amazon Watch Legal Advisor and Defend the Defenders Program Coordinator
“We are appalled at these horrific killings and the continued threats that Indigenous Peoples in Brazil continue to face
Violence against Indigenous peoples in Brazil will not stop automatically with the new administration
as criminals were protected and strengthened throughout the Bolsonaro administration in various regions of Brazil
and Joenia today acting strongly as the public power for the protection of Indigenous peoples and guaranteeing their rights is a great and fundamental step.”
“How are we going to eliminate illegal deforestation by 2030 with a project that demands more deforestation
It's not possible to talk about being a leader against climate change with a project to destroy the Amazon."
Munduruku ancestral territory Sawré Muybu advanced to the final stage of demarcation
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the Pataxó have resisted the colonization of their lands — the struggle to protect their language
There was an elder who was seated on a rock on the seashore
The first wave hit the rock and made the sound “pa,” the second wave made the sound “ta” and when both waves retreated back to the sea they made the sound “xó.” “Pa-ta-xó.” That’s why Pataxó means the “sound of water.”
whose name means “wolf-warrior.”
This photo essay is not published under ROAR’s regular Creative Commons license
Please secure permission from the author before reproducing this content
where the first Portuguese colonizers landed in 1500
are still suffering from the consequences of that fateful day
traversing the forests and living off what nature provided
in the mid-19th century they were forced to settle down and form the aldeia (village) of Barra Velha
Txag’ru Mirawê cultural center in Barra Velha
amidst all the things the government has tried to do to oppress us
the Pataxó has the ability to keep his head up and continue ahead with his ideals and culture
Kids playing at the Txag’ru Mirawê cultural center
“Many Indigenous peoples were raped and killed,” Ubiranan continues
More than five hundred years have passed and we exist
looking to destroy Indigenous peoples and our fauna and flora.”
resulting in the Pataxó dispersing and fleeing to other places to seek refuge
“Many Pataxó fled to the extreme South of Bahia
where they became slaves in exchange for food or a place to sleep,” says Nitynawã
And today we’re fighting to win back our lands that were taken from us
we have to see the spilt blood of our relatives fall to the ground.”
the Pataxó were banned from speaking their native language
it’s our secret that our great God left us and now we’ve lost a lot of that,” laments Ubiranan
he goes on to explain that today the language is being revived and taught at Pataxó schools
Nitynawã went on to achieve her dream of being able to read and write without going to school
“And sometimes even today we go through this in schools
in whichever place we are in we face discrimination and prejudices — not as much as in the past
While many Pataxó have to endure all kinds of prejudice simply for being Indigenous
“I personally have suffered a lot from prejudice because as well as being Pataxó I’m also mixed-race
So many people tell me that I’m not Indigenous
but unfortunately these people continue thinking I’m not Indigenous.”
Wêha does not let their ignorance defeat him
I beat my chest and say that I’m Pataxó and whoever wants to disagree
I know where I come from and where I was brought up
my roots and for me that is what’s important.”
Ytxêwá (savior) and Gwanãnhí (happy hummingbird)
This complex question of identity — of being mixed or Indigenous — has been weighing down on the Pataxó for years
“The Aldeia Jaqueira was founded in 1997 by three women
in order to demonstrate to ourselves who we are
in order for them to be accepted in that other society
had to take on the identity of the caboclo (a person with mixed Indigenous and European ancestry),” says Nitynawã
“So this is a way for us to show that we’re not cabolco
the biggest difficulty the Pataxó face today is the question of land: “Our right to get our land demarcated as indigenous land
15 are demarcated and 25 are still in the process of being demarcated.”
“We often hear the president say that the Indigenous have too much land
grandchildren and great-grandchildren to think about
and we depend on nature to survive.”
cities are being flooded because there’s no more forest to protect the rivers
We believe that the earth is not just for agriculture
but she needs to be preserved for future generations.”
because everyday she is being born and growing
grandchildren and for me to absorb good energies
Help ROAR cultivate the radical imagination
Sonum is an independent filmmaker and photographer based in London
She has been making visual stories on marginalized communities for the past ten years and is particularly drawn to the themes of identity
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Source URL — https://roarmag.org/essays/resist-protect-revive-being-pataxo-in-brazil/
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“Our Atlantic Forest has several very important living beings
species that are already endangered and that we need to bring back,” says the Pataxó Matias Santana
president of the Foresters and Reforesters Work Cooperative of the Pataxó Boca da Mata Indigenous village (Cooplanjé)
“We created the work cooperative to bring jobs to the community
Cooplanjé worked on restoring 210 hectares (519 acres) of degraded Atlantic Forest areas to increase forest connectivity between the Monte Pascoal National and Historical Park — the first piece of land sighted by Portuguese colonizers — and the Pau Brasil National Park
also integrating the Barra Velha Monte Pascoal Indigenous Territory of the Pataxó ethnic group
“It was the first time that BNDES financed an AFS [agroforestry system] project in the Atlantic Forest biome,” says Marcos Lemos from the Natureza Bela Environmental Group
Fifty hectares (123 acres) out of 210 were restored within the Boca da Mata village
“We use this AFS as a restoration strategy for Monte Pascoal.”
In addition to the productive agroforestry system forming a kind of green belt sorrounding the reforested area
it is a way to strengthen the survival of Indigenous communities
“The conservation unit has an overlap with the communities of the Barra Velha of Monte Pascoal Indigenous Territory
which consists of 16 villages surrounding the park,” explains Lemos
“Today I imagine that we have about 2,000 hectares [4,942 acres] or more going through a restoration process in the Monte Pascoal-Pau Brasil Ecological Corridor
most of them concentrated on the edges of the parks,” says researcher Paulo Dimas Rocha de Menezes from the Federal University of Southern Bahia
restoration projects have collaborated to form the ecological corridor
contributing to the gene flow of animals and plant species and also to implement economic activities that benefit the people of the region
“We have a history of deforestation and occupation of this region that was exclusively logging
first removing the Atlantic Forest and then entering with pastures,” says Lemos
“We are coming with a whole set of actions and institutions to maintain what exists and advance in preservation
considering that we are in a region with three national parks and we also have the Abrolhos Marine Park
which is influenced by these recharge areas.”
One of the largest remnants of Brazilwood forests (Paubrasilia echinata) survives in this region of water relevance and rich biodiversity
in a settlement of the Landless Workers Movement
the largest specimen of Brazilwood in the country was found in 2020
with an estimated age of 600 years and a circumference of more than 7 meters (23 feet)
which already covered the Bahian soil before the arrival of Portuguese colonizers
“We work with 132 endemic species and try to restore what used to be our flora
jacaranda — species that we don’t find anymore,” says Lemos
Besides conservation units and Indigenous villages
also known as the Mosaic of Protected Areas of the Extreme South of Bahia (Mapes)
includes private lands and suffers strong pressure from the use of native Atlantic Forest timber
“The devastation in the extreme south of Bahia is very recent,” says Dimas
“The first stretch that Europeans occupied on the coast was the last to be settled because colonization was forbidden here when they discovered Minas Gerais.”
To protect the gold discovered in the 17th century in Brazil’s interior
settlers were prohibited from the north of Espírito Santo to the south of Bahia
The Indigenous people there served as a shield
preventing non-Portuguese from entering the mining region
the construction of the Bahia-Minas Gerais Railroad exacerbated deforestation
intensified with the paving of the BR-101 highway in the 1970s
“With the incentive of the military dictatorship
more than 200 sawmills were installed here and they destroyed the forest in 20 years,” says Dimas
“By the 1990s there was almost no forest left
except for what was later transformed into national parks
If some accuse the Indigenous people of deforesting the area
experts say their use of wood for handicrafts is irrelevant compared with the region’s history of devastation
“Our history proves that it is not them
They are the ones who suffer the most and are exploited even today in this issue of wood extraction,” says Lemos
but there is still an inhumane exploitation for the man who cuts this wood
because it is done in a handmade way and sold at very low prices
which comes to be a degradation of the human condition.”
Cooplanjé and the productive agroforestry systems have emerged as an alternative to the use of wood in the Pataxó territory
“Several families have left the extraction and processing of wood for restoration and agroforestry,” says Paulo Dimas
the ideal would be to take all the families out of this activity and turn them into forest-living families.”
Despite the advance, the Pataxó people live in a situation of constant conflict with ranchers
“Here in the territory of Barra Velha
this area that the [Indigenous] community entered is a demarcated area that has already been ratified
but today it is occupied by ranchers,” says Santana
“We have already had a dispute with the government and with Funai to pay for the property that the ranchers have on the land and to liberate our territory
So the community makes the claim in this way
the amount of land in possession of the Pataxó in the Barra Velha do Monte Pascoal Indigenous Territory is very restricted
“They have the right here to more than 50,000 hectares (123,553 acres) of land already demarcated and they are in possession of 9,000 hectares (22,240 acres)
they cannot maintain traditional activities and have to live on tourism
Santana wanted to keep the 80 families who worked on the BNDES-funded restoration project within Cooplanjé
but it was not possible due to a lack of new projects
only five families remain working in the cooperative
“Our plan is to seek partners and funders directly
so we can have an independent Indigenous organization
We are looking for other partners so that we can bring jobs into the community,” says Santana
“Now we are happy because we are building a partnership for seed delivery and we are also partnering with a nursery in São Paulo to produce seedlings.”
Banner image of maintenance work in the restored area around the Pau Brasil National Park
Image courtesy of Natureza Bela Environmental Group
This story was reported by Mongabay’s Brazil team and first published here on our Brazil site on Nov
From intimate seaside inns to lush tropical resorts
here are six Wallpaper*-approved winter sun escapes
No need to wait for summer when there’s such invigorating magic in the winter sun
From intimate seaside inns to sprawling tropical resorts
here are six Wallpaper*-approved escapes where you can reset and recharge
Auka Boipeba delivers a dual bliss of jungle and beach
cobogós (perforated bricks used to build walls)
The beachside spa taps into local botanicals
while the restaurant serves shrimp stew risotto and yellowtail snapper ceviche straight from the island’s waters
Velha Boipeba’s average February temperature: 29° / 26° (High / Low)
Read our full hotel review of Auka Boipeba
Minutes away from the beach of Los Naranjos and the lively village of La Punta in the Mexican municipality of Puerto Escondido, Casa Yuma is a peaceful oceanfront oasis that celebrates its surroundings
designed the hotel to blend into the environment using native materials and locally sourced ceramics and furnishings
and soulful Mexican cuisine set the tone for a balmy escape
Casa Yuma is located at Ventanilla KM 153, Lote 10 Los Naranjos, Mexico; casayuma.com
escapism and design stories from around the world direct to your inbox
Puerto Escondido’s average February temperature: 29° / 22° (High / Low)
Read our full hotel review of Casa Yuma
A Caribbean jewel with Parisian poise, Cheval Blanc St-Barth offers palatial relaxation on the sun-drenched shores of Baie des Flamands
its 61 suites and villas embody the essence of plush island living
Jean Imbert’s vibrant menu sets the stage for long
while Guerlain’s spa rituals unfold in serene seclusion
or indulging in a private beachfront dinner
Cheval Blanc St-Barth is located at Baie des Flamands, Saint-Barthélemy 97133, St Barthélemy; chevalblanc.com
St-Barth’s average February temperature: 29° / 23° (High / Low)
Read our full hotel review of Cheval Blanc St-Barth
and bespoke ceramics with the comfort of integrated kitchens and Smeg coffee machines
From whale watching on the terrace to feasting on Clarence Valley’s finest produce
Il Delfino is an intimate inn of coastal passion
Il Delfino is located at 4 Ocean St, Yamba NSW 2464, Australia; ildelfino.com.au
Yamba’s average February temperature: 27° / 19° (High / Low)
Read our full hotel review of Il Delfino
Set within the 350,000 acres that make up Tanzania’s Grumeti Reserve, Singita Milele is a 1,200 sq ft buyout villa that redefines the modern safari retreat
its five distinct suites echo the Serengeti’s palette – natural textures dominate
with earthy hues combined with soft grassy shades
From a starlit infinity pool to a speakeasy-style bar and open-fire boma
the savannah isn’t just seen – it’s felt
with no barriers between guests and wilderness
Singita Milele is located in Natta, Tanzania; singita.com
Natta’s average February temperature: 29° / 17° (High / Low)
Read our full hotel review of Singita Milele
Ta’aktana puts the fishing village of Labuan Bajo on the luxury map
the 70-key retreat – including seven overwater sea villas – marries curved silhouettes and natural wood with a modern
from snorkelling at Taka Makassar to hikes on Padar Island
Ta’aktana’s five distinct food and beverage concepts continue with Taba’s Japanese robata cuisine
while Di’a Spa’s cave-inspired rituals offer a restorative experience
Labuan Bajo’s average February temperature: 29° / 24° (High / Low)
Read our full hotel review of Ta’aktana Labuan Bajo
Travel EditorSofia de la Cruz is the Travel Editor at Wallpaper*
she feels most inspired when taking the role of a cultural observer – chronicling the essence of cities and remote corners through their nuances
often shaped by conversations with the photographers who capture these worlds through their lens
The Pre-Salt reservoirs in Brazil are home to some of the world’s largest oil and gas reserves and one of the most exciting exploration frontiers
until now the exceptional depth of more than 5,000 m below sea level with around 2,000 m of salt overlying the reservoir
has caused significant challenges to de-risk locations for drilling exploration wells
The industry therefore needs to capitalize on any data that already exists from these reservoirs
we describe how digital core data forms a key part of the solution
providing a continuous dataset along cored intervals in addition to the traditional plug measurements
exploration teams have had to make do with limited data types from core samples
The resolution of these data is usually low
They typically range from three to five core plug measurements per meter with or without essential metadata
Sparse resolution along with uncertain data quality can hinder any geological model
Data uncertainty can cloud precise decision-making
creating additional costs for acquiring new core
Without a centralized system for easy retrieval of these historical data
they are often scattered across numerous repositories
Professionals have to spend valuable time and resources locating the necessary information
There is also the challenge of how records are stored
The transition from paper to digital formats is time-consuming and prone to errors
often compromising the integrity of the data
These challenges underscore the need for innovative solutions – solutions that the Geotek-Solintec multiclient project now provides
spanning two scales of measurement: the core scale (mm to m) and the pore scale (<sub to mm)
the catalog provides data that was never before acquired from these complex rock formations
The core scale is represented by hyperspectral imaging and multi-sensor core logger (MSCL) measurements of 1,164 meters of core from 16 wells
Data acquired from the cores includes ultra-high definition visible and UV images
The pore-scale data is represented by digital high-resolution twins of 3,003 thin sections that correspond to the same intervals as the core samples
These thin sections offer a microscopic view of the rock’s composition and structure
providing critical insights into the reservoir’s characteristics
This level of detail is invaluable for understanding the geological and petrophysical properties of the pre-salt layers
It also perfectly complements the MSCL and hyperspectral datasets from the core
The pre-salt digital catalog has yielded a comprehensive suite of deliverables
transforming how operators approach pre-salt reservoir exploration
Discover the variability of the depositional system through well-to well correlations and apply to the reservoir model and characterization
Depth-coregistered data from multiple datatypes that are ready for the ML/AI revolution in geoscience studies
Data from the rock catalog enable early lithology classification within the Barra Velha Formation
They distinguish two facies and deliver an understanding of the geochemical and mineralogical distribution within and between these units
The upper section of this data example is a carbonate reservoir dominated by calcite with 1 m thick intervals of dolomite
These rocks are hydrocarbon-bearing with evidence of the dolomite-rich intervals having a lower proportion of hydrocarbons
A sharp contact at 5,643 m spells the introduction of a conglomerate
This is rich in volcanic lithoclasts interpreted from the reduction in carbonate mineralogy and the elevation of silicon (Si)
with a decrease in calcium (Ca) and magnesium (Mg)
The hyperspectral imaging shows that these facies of the Barra Velha Formation have 1-2 m thick clay intervals composed of smectite and montmorillonite
and lower amounts of illite dispersed throughout
The clay is derived from the volcanic clasts within this conglomerate
which were re-worked during its deposition
combined with generally erratic chemical and mineralogical downcore profiles
all support a heterogeneous conglomerate facies
The identification of pore-filling clay intervals
combined with the heterogeneous nature of the facies all contribute to a reduction in reservoir quality
This is why the hydrocarbon content is lower in this section
with their pore-filling clay and the nature of their clasts
could become an important marker bed and regional barrier to hydrocarbon production – essential for the geological model
The digital rock catalog is delivered with visualization software and represents significant progress in the geological evaluation of these pre-salt reservoirs
Exploration teams now have access to a wealth of high-quality
Geotek and Solintec have advanced the level at which geological data is available for pre-salt operators in Brazil
Learn more about the benefits to your specialist research work from the Geotek Solintec Pre-Salt Reservoir Digitalization Project
Bahia — Eliane de Oliveira Conceição heard the roar of gunfire before she could see who was firing
she could make out three vehicles that slowly approached the farm and opened fire indiscriminately
but the bullets pierced the barrier and killed him
It wasn’t until one of the rounds ricocheted off a steel gate back at the assailants that they retreated
speeding off as quickly as they had arrived
“That’s when they finally backed off because they came to kill us all,” she said
The farm where this attack occurred in September lies in one of around two dozen plots of land that members of her Indigenous group
have reclaimed from wealthy ranchers in the Brazilian state of Bahia
a state judge filed repossession orders against three of these reoccupations that will effectively evict the Pataxó
intensifying the violence that has been escalating against Indigenous people in the south of Bahia
which has claimed the lives of three Pataxó youth
The crisis the Pataxó are facing adds to growing pressure on President Luiz Inácio Lula da Silva and the new Ministry of Indigenous Peoples to demarcate Indigenous lands and solidify protections for Indigenous people in Brazil
Whether or not the new ministry can curb violence and mitigate the land conflicts will be a test in standing up to powerful moneyed interests that pervade regional politics
as state and local authorities have been connected to recent murders and violence in the region
The Pataxó were among the first Indigenous people to encounter the Portuguese and have since been dispossessed of all but a few small remaining areas of their ancestral land. The state-run company, Brasil Holanda de Industria S.A., cleared thousands of hectares of native Atlantic forest
one of the world’s most ecologically diverse regions where the Pataxó lived
effectively evicting them and giving much of the cleared land to cattle ranchers and farmers
The state then declared one of the remaining swaths of Atlantic Forest that the Pataxó occupied as a national park
They have been awaiting formal demarcation of the two largest Indigenous territories
Barra Velha do Monte Pascoal and Comexatiba
in the south of Bahia where Conceição da Silva lived
Although the federal agency responsible for demarcating Indigenous territories
the National Foundation of Indigenous Peoples (Funai) has already declared both as Indigenous territories
which grants them certain constitutional rights
several additional steps have to happen for the land to be officially handed over to the Pataxó in a legally binding way
multinational agribusiness and farmers continue to encroach on their land
“Land-grabbing and the tourism industry are the biggest threats to the Pataxó,” Paulo Lugon Arantes
an international consultant for the Indigenous Missionary Council (CIMI)
The Pataxó territories overlap not only with eucalyptus plantations sold to multinational companies
but also with multimillion-dollar beachfront properties in one of the last relatively pristine coastal areas in Bahia
“We experience a lot of violence from the agribusiness on our land,” Mãdy Pataxó
a leader who has helped reoccupy several farms
told Mongabay when we visited the Comexatiba Indigenous Territory in February
“This irregular urbanization process has been killing our people — drug trafficking
This has been disqualifying and mischaracterizing our territory.”
President Lula’s administration has stated that it will work to defend Indigenous people’s rights and has made important steps toward that promise
He created the country’s first Ministry of Indigenous Peoples under the helm of Sonia Guajajara
who in January established a crisis desk to deal with the increased violence toward the Pataxó
But the strategy required to address this crisis differs from other crises the new ministry is also dealing with
like the Yanomami who have been poisoned by illicit mining in a remote territory
Defending against these aggressions boils down to having legal grounds for claiming the land belongs to them
“What we need is this: demarcation and security and that the federal government direct its gaze towards us,” said Chief Mãdy Pataxó
a key leader involved in the land recovery efforts
Demarcation is the key demand from Indigenous people on Lula’s government across Brazil
many of the existing legal challenges faced by the Pataxó would be halted or even reversed
“Local judges have been giving eviction orders to the Pataxó
they will be required to give eviction orders against the invaders,” says Lugon Arantes
While the two southernmost Pataxó territories have had their boundaries determined and have been identified as Indigenous
Funai still has to respond to the objections made by farmers and business owners in 2015 before the formal demarcation process can progress
But Barra Velha do Monte Pascoal has gone through all legal hurdles and awaits the final document that would give full control of the territory to the Pataxó: a declaratory ordinance signed by President Lula
leader of Quero-Ver village in the Barra Velha Territory
that letter could be coming out at any time — potentially in a matter of weeks
This has not prevented a state judge in Bahia from ordering the repossession of Quero-Ver and two other Indigenous reoccupations in mid-March
siding with farmers and ordering the Pataxó communities to leave their land again
The Pataxó people and the Union Public Defender’s Office have appealed to the courts against the rulings
which they fear could further intensify the violence in the region
According to Lethicia Reis, a lawyer at CIMI who represents one of the communities, that decision violates a concept enshrined in the Brazilian constitution called Indigenato
which recognizes the inherent right of Indigenous peoples to use their ancestral lands and the jurisprudence of the Supreme Court
agricultural development and real estate speculation
With little sign of advancement throughout the years
the Pataxó have turned to a different tactic; last summer they began occupying and reappropriating areas from which they were historically expelled
gunned down on a highway while driving back to a reoccupation site in the Barra Velha Territory
Their deaths happened just a matter of weeks after assassins had invaded another nearby community in the territory
Gustavo Conceição da Silva was the first of three Pataxó youth to be killed in a period of five months
Conceição da Silva posted a photo on social media with a sign that read: “The Pataxó ask for help.” It is the only picture that de Oliveira Conceição still has of her son
a part of our tribe,” Oliveira Conceição told Mongabay
we get more fervent with the will to not lose anyone again
I feel like screaming so that people hear the Indigenous cause
That they know Indigenous people have rights.”
and most still live in fear of perpetual attacks and violence
Some of the violence can be attributed to the hangover from the previous president
“We are still feeling the echo of the Bolsonaro government
where attacks against Indigenous people were structurally encouraged,” CIMI’s Lugon Arantes said
Other measures face road blocks by state officials
“Because of the escalation of violence in Bahia
the Ministry of Indigenous Peoples asked the national force to be sent there to protect them,” said Edson Krenak
Brazil’s program director for Cultural Survival
has not allowed for the national force to come in
State and local authorities have been connected to the recent murders
Three MPs were arrested on suspicion of involvement in Conceição da Silva’s death in October
suspected of killing two Indigenous Pataxó youth in Itabela as they were returning to a reoccupation in the Barra Velha Indigenous Territory
presented himself to the police in Teixeira de Freitas
He is a Military Police soldier who provided private security services in the region
the Pataxó and experts say that formal demarcation is the only lasting solution to what for many Pataxó seems like never-ending waves of violence
Chief Patiburi Pataxó and several other members of the Quero-Ver village were harassed by a group of men brandishing guns and threatening them when they left to get food
we want to know what we are going to do,” Chief Patiburi told Mongabay in a voice message
“Our people don’t sleep anymore; our people don’t eat anymore; we’re scared to even take a moment to drink
Banner image: Chief Patiburi Pataxó stands on the beach of the reclaimed Quero-Ver community
Murders of 2 Pataxó leaders prompt Ministry of Indigenous Peoples to launch crisis office
The authors propose an approach that uses machine learning to characterize carbonate facies in a wildcat (Gato do Mato) prospect in the Santos basin
We analyzed different seismic attributes and selected those that best responded to the seismic patterns identified in the study area as input for an unsupervised classification
The classification method used is the self-growing neural network (SGNN) technique that consists of the following steps:
we associated the classified seismic facies with the patterns identified in the amplitude data
The seismic facies allowed us to differentiate the carbonate platforms from the build-up facies
the classification encountered difficulties in identifying the patterns associated with lake bottom facies and the chaotic seismic pattern of debris facies
Seismic attributes are efficient tools for highlighting stratigraphic and structural features
Seismic attributes are highly effective in emphasizing stratigraphic features that can be easily detected (or not) in seismic amplitudes
Taner (2000) defines a seismic attribute as any information extracted from seismic data
whether logical or based on geological/geophysical knowledge
seismic attributes are combined to identify seismic patterns that can be associated with depositional environments and diagenetic processes
Machine learning algorithms have proven to be a powerful tool in solving problems involving large volumes of data
these techniques have been used in seismic facies classification for reservoir characterization
They have been a key element in a better understanding of reservoirs
allowing more detailed analyses and more reliable results
reducing the uncertainties inherent in the exploratory process
seismic pattern analysis uses this type of technology in combination with geostatistical methods for facies probability volumes
It is the primary hydrocarbon producer in the country with an average 2.8 MMboed
out of total Brazilian production of 3.8 MMboed
The reservoirs are described as lacustrine carbonates of Aptian age (Buckley 2015)
Given the importance of understanding and analyzing these reservoirs
we propose an approach for the identification and characterization of carbonate facies in the wildcat prospect
which is in the outer high that is the main region of the pre-salt reservoirs of the Santos basin
we chose stratigraphic and structural seismic attributes and performed an unsupervised facies classification
using the self-growing neural network (SGNN)
a machine learning algorithm based on growing neural gas
The main Brazilian pre-salt reservoirs are in the Barra Velha formation
This formation can be divided into two tectonic sequences by the Intra-Alagoas unconformity
with the basal belonging to the rift section and the upper belonging to the sag phase
The Barra Velha formation is characterized by the occurrence of in-situ (shrub
spherulite and laminate) and reworked facies deposited in a lacustrine environment during the Aptian
1) represents an uplifted structure from the basement and marks the transition from volcanoclastic deposition to almost continuous deposition of carbonate during Barremian and Aptian (Buckley 2015)
The structure of this high is delineated by NE-SW trend faults
Structural highs influenced the pattern of Cretaceous carbonate accumulation over Neogene sedimentary strata
These highs conditioned the accumulation of pre-salt carbonates
isolating them from the continental clastic sediment region
The seismic data available for analysis is a PSDM (pre-stack depth migration) volume of approximately 1,100 km2
We interpreted the horizons and faults on this seismic amplitude for interval definition
analysis of seismic patterns and facies classification
To analyze the main geological configurations and characterize carbonate facies
3: 1) carbonate seismic pattern identification through seismic amplitude; 2) seismic attribute generation and analysis; 3) principal component analysis (PCA); and 4) unsupervised seismic classification
Carbonate seismic pattern identification through seismic amplitude
Recent studies on the characterization of seismic patterns in pre-salt reservoirs show that the main configurations found are build-ups (carbonate mounds)
with the carbonate mounds representing the facies with the best porosity and permeability
Figure 4 illustrates the seismic patterns identified in the Barra Velha Formation
between the Pre-Alagoas unconformity and the base of salt horizon
Build-up facies are characterized by chaotic seismic textures with a conical external geometry
Debris exhibits prograde geometry with a chaotic internal texture
The carbonate platform facies show well-defined flat parallel reflectors
The bottom lake facies do not have specific geometry
The following seismic attributes were generated to assist the seismic characterization
Dip-steered enhancement (DSE) is performed as a seismic filter oriented to dip and azimuth
which executes lateral filtering along the surfaces
This filtering enhances the lateral continuity of reflectors and removes noises
we apply the DSE before generating the Coherence Cube attribute
as this attribute is sensitive to the presence of noise
Eigen coherence attribute is the ratio of the energy of the data’s coherent component to the energy of the original traces within the analysis window
The eigen structure method analyzes a window of traces and determines which wavelet best represents the waveform variability
This wavelet is scaled to fit each input trace
providing the coherence component of the data
The coherence attribute allows the analysis of structural characteristics
since it measures the similarity or non-similarity of seismic data
We use it to understand the lateral extent of geological features (seismic patterns) and to assist in the identification of more fractured regions
The relief attribute was developed by Bulhões and Amorim (2005)
It is called amplitude volume attribute (TecVA)
and it aims to increase the visualization of reflectors and faults
showing small variations in amplitude in a lateral trace-to-trace correlation
This attribute is very useful for highlighting the subsurface geology by detailing the discontinuities and lateral variations of the seismic facies and enhancing the lateral continuities of the reflectors
Relative acoustic impedance computation is based on seismic trace integration
This attribute is an indicator of acoustic impedance changes
This is a stratigraphic attribute that assists in identifying and delimiting layers
PCA is the process of computing the principal components on the data
It can be used before the seismic classification as a filter to reduce the input space dimension
The low variability of seismic data makes the PCA a very efficient method for reducing the samples in the input space
When applied in seismic multi-attribute facies classification workflows
the transformed data can identify and differentiate hidden features
The results can improve seismic pattern classification
PCA finds the principal directions in multi-dimensional data and determines the optimal shift and rotation of the data to be expressed in those principal directions
it classifies the directions according to a decrease in the greatest contribution of each component
which can be used to reduce dimensionality
the seismic attributes used as input for the PCA were the seismic amplitude filtered by the DSE
Unsupervised seismic facies classification with attribute clustering
Attribute clustering is a method for automatic unsupervised facies classification
such as Self-Growing Neural Network (SGNN) or Growing Neural Gas
This method uses a system based on neurons that behave as a gas during the training process
The SGNN technique builds a topology defined dynamically that maintains the neighborhood relationships of the data
Two principles are honored: i) two neighbor elements in data space continue as neighbors in the topology space
and ii) more neurons are assigned to regions with a dense level of information
based on the data similarity and propagated later into seismic using a Bayesian approach
Three steps are necessary to perform the seismic facies classification
The first is selection of the seismic attributes and the interval for the classification
The neural network is then trained on the input data
the algorithm identifies the main data trends that can be used to classify the data
a facies volume is generated with the related probability facies
The trained neural network will be used to estimate probabilities for each facies
we have a most probable facies volume and probability volumes for each facies
using dip-steered enhancement (seismic-driven structural filtering) to help improve continuity of the reflectors and reduce noise and migration smiles
This attribute was then used as input for the Eigen coherence computation
we can observe the results of the Eigen coherence
which emphasize the build-up and bottom lake facies
we observe an internal chaotic texture and a fractured central region in the debris facies
while the carbonate platform facies show flat parallel and well-defined reflectors
The relief attribute accentuates the reflectors’ continuities and chaotic zones and helps to identify the debris seismic facies and the carbonate platform
The debris patterns present a prograde geometry with a fault system in the proximal part and a chaotic pattern in the distal part
The relief attribute shows the carbonate platform as flat parallel and well-defined reflectors
We decided to compute the relative acoustic impedance to obtain a better resolution volume with information about acoustic impedance changes
The contribution of each component of the PCA was about 33%
We chose only two of the three components where the differentiation between build-ups and the carbonate platform was more evident
together with the relative acoustic impedance volume
were selected as input for the seismic classification
The interval for the unsupervised facies classification was defined by the base of salt horizon and the pre-Alagoas unconformity
Several training runs were carried out until we found an optimal number of neurons
a model with nine classes produced the best results to represent the carbonate seismic facies
Some quality controls were performed to guarantee more confidence in the results
a parallel plot allowed the assessment of every attribute contribution during the neuron training
there is a good distribution or variation of every class neuron for the different attributes
confirming that all the attributes contribute to the prediction
which allows the estimation of the most probable facies by defining the neuron influence area as a Gaussian function (weight = e-distance)
Smoothing was performed on the results from the seismic dip and azimuth volumes
we obtained a most probable facies volume and the probability for each class
We associated some seismic facies with the seismic patterns of the Barra Velha Formation
We obtained a clear differentiation between the carbonate platform and more fractured areas related to the build-ups
Facies in dark blue (class 8) and violet (class 9) are associated with the carbonate platform because of their continuity and flat behavior
The brown (class 1) and orange (class 3) facies are more concentrated in areas that show more discontinuities (fracturing) like the build-ups
These types of facies are more present in areas closer to the main faults
The debris facies were not detected in the interval used for the facies classification workflow
the bottom lake patterns did not appear very evident
impeding their association with one of the seismic classes
The facies occurrence probabilities are shown in Fig
The carbonate platform (dark blue and violet) and build-ups (brown and orange) present a high probability of occurrence
This type of information is extremely useful for uncertainty analysis associated with facies modeling
relief and relative acoustic impedance attributes help the identification and characterization of build-ups
which are the main seismic patterns found in the Brazilian pre-salt reservoir
Those patterns have the following characteristics: Build-up facies appear on the structural highs
with chaotic seismic texture and parallel and well-defined conic external geometry; the carbonate platform facies is located in horsts and presents flat-parallel and sub-parallel high amplitude reflectors; debris facies occur in the fault borders and exhibit a prograde geometry with chaotic internal texture
the bottom lake facies are found in structural lows and present transparent seismic facies
Principal component analysis before the seismic classification aids in the discretion of build-ups and carbonate platform facies
is an effective approach to differentiate the fractured zones mainly associated with build-up facies in the wildcat prospect
The prospectivity of the deepwater outboard Santos Basin is revealed by new 3D seismic
With a daily oil production in the region of 2.6 MMbo (ANP
Brazil is among the ten largest oil producers in the world
Just under half of Brazilian oil production comes from the pre-salt carbonate reservoirs of the Santos and Campos Basins
Production from sag-phase and syn-rift (Aptian and Neocomian) reservoirs dates back almost to the start of exploration and production in the Campos Basin
where Neocomian vesolitic and fractured basalt and Barremian coquinas were put into production in the Badejo and other fields
the pre-salt Lower Cretaceous carbonate reservoirs of the Santos and Campos Basins did not occur until the 2006 discovery of the giant Tupi/Lula field in the Santos Basin and the 2008 development of the pre-salt carbonates in the Campos Basin Jubarte field
Further discoveries of pre-salt fields in the Campos Basin (some below extant fields in Late Cretaceous to Miocene turbidite sands) followed
including the Parque das Baleias fields from 2010
Production from the Lula and Sapinhoa fields in the Santos Basin began in 2013
including Carioca/Lapa (2016) and Franco/Buzios (2018)
A fast-track sub-volume (3,370 km2) of the Santos 3D volume is now available for inspection before the upcoming license rounds
This sub-volume shows only a small portion of the larger study area
but it is sufficient to validate the main findings of the 2D seismic surveys:
South America and Africa were part of Gondwana until separated by Late Jurassic-Neocomian rifting
when horst and graben structures developed in trends roughly perpendicular to current coastlines
a transition is seen from proximal fluvial-alluvial clastic-dominated facies to widespread deposition of lacustrine facies
Shallow water lacustrine carbonate reservoirs developed locally on or around horsts
whilst coeval organic-rich shales (associated source rocks) accumulated in the grabens and halfgrabens
The end of major rifting is marked by a regional angular unconformity
with carbonates and shales infilling the late syn-rift to sag basins
Increasing salinity of the lacustrine environment culminated in deposition of thick salt
which ended with the start of seafloor spreading and the resulting opening up of the restricted rift basin
Late Aptian-Albian shallow marine carbonates were deposited on the salt
Platform carbonates and their deepwater equivalents dominate the Albian–Cenomanian
The Upper Cretaceous to Tertiary is mainly characterized by siliciclastic deposition
Initial development of the pre-salt play in the Santos Basin focused around the northern and central areas inboard of the Outer High of the Santos Basin
including Libra/Mero and Franco/Buzios in the north; Iara
Jupiter and Pau Brasil in the centre; and Sul de Guara and Peroba in the south
The primary reservoir for these fields is a high porosity and permeability sag-phase carbonate facies (K46-48: Barra Velha Formation) sealed by the overlying salt
This usually presents as horizontal to low angle
There is usually little to no evidence of major faulting of this formation in most of the Santos Basin
Bioclastic limestones (Itapema Formation/coquinas)
at the top of the major rift phase and in the lower part of the sag basin
are a potential secondary carbonate reservoir
They are typically present as stacked banks of reworked shelly fragments deposited along lake margins and are found in deep to shallow lacustrine environments
The corresponding seismic facies is moderate to good amplitude
Coqueiros reservoirs have been reported as oil-bearing at Seat and Pão de Açúcar in the Campos Basin
Buzios and Lula fields in the Santos Basin
The main source rock for the Santos Basin pre-salt fields occurs in the lower syn-rift (K36)
As these early discoveries have matured to producing fields
exploration has moved south and east into more outboard areas
Exploration interest has been sustained by improved understanding of the environment of deposition of the main pre-salt reservoir (the Barra Velha Formation)
and by innovations in the licensing regime
such as frequent licensing rounds and permanently offered blocks
Three exploration rounds in 2018 raised record bid amounts
lifting expectations for three more licensing rounds (Concession Round 16
Pre-Salt Production Sharing Contract Round 6 and the Transfer of Rights Surplus round) for which public bidding is scheduled for Q4 2019
The evaporite sequence is seen to comprise both ‘stratified’ and diapiric sections
signifying the presence of not just halite but additional evaporite minerals (e.g
The presence of this ‘dirty salt’ requires that a common offset RTM (COR) be applied to update the salt body velocity
Complex internal deformation (thrusting and folding) is evident in the salt sequences
A feature of particular interest in much of the study area is the apparent large fault-throws at base of salt level
This is not an anomalous feature of the present study area: similar features have been noted in the PSC Round 5 Saturno and Dione prospects (Petersohn
often larger at the pre-salt level than in the underlying syn-rift level
This suggests that syn-rift faults were re-activated during or very shortly after Late Aptian salt deposition
Note in the seismic foldout how reflectors in the hanging-wall salt (A) onlap the plane of the fault with high angle
This may suggest a significant degree of local rotation within the evaporite sequence caused by fault movement and/or salt dissolution
Figure 3 shows a map of the Base-Salt horizon throughout the fast-track sub-volume
It shows a series of small north-west to south-east trending four-way dip closures flanking a major high
Much larger four-way dip structural closures have been mapped on the Spectrum (now TGS) 2D seismic data throughout the study area (Spectrum
2013) outline the Barra Velha Formation immediately under the salt and confirm its minimum thickness throughout the fast-track subvolume to be greater than 200m
In much of the fast-track sub-volume the Barra Velha Formation unconformably overlies the syn-rift succession
it appears often to unconformably overlie basement
This has been a brief review of a fast-track sub-volume that constitutes a little more than an eighth of the greater TGS-Spectrum Santos 3D; any comments on such a small and intermediate sub-volume are necessarily limited
analysis of this data does support the findings of the 2D seismic data that large structural closures at Barra Velha Formation level are present throughout the project area
together with flanking grabens and half-graben areas filled by syn-rift sediments (prospective kitchen areas and secondary coquina facies secondary carbonate reservoirs)
These findings support the prospectivity of this entirely undrilled area of the southern Santos Basin and are essential viewing for any companies interested in the upcoming PSC 6 and future license rounds
opened up a new chapter for petroleum reservoirs: lacustrine carbonates capable of producing hydrocarbons at extremely high rates
consisting of shell fragments accumulated on lake margins
have been found in small fields in shallow water off Brazil
particularly in the Santos Basin deepwater
Referred to as ‘microbialites’ when first discovered
their origin has recently come into question
There is good evidence that these carbonates formed in shallow basins abiotically and the ‘microbialites’ do occur but make up a less important portion of these carbonates
While there are similarities in these reservoirs both across the South Atlantic and north-south along the margins
there is much variation between them as well
From area to area they exhibit distinct stratigraphic patterns and diagenetic histories
with modes of formation varying from distinctly biotic to abiotic
These differences may be explained by the variability in climate
and chemistry of the lakes where the carbonates were deposited
Knowing the depositional settings for contrasting lacustrine facies is necessary to help interpret and model these important reservoirs
Some of the best documented lacustrine deposits are located in the western United States and include the modern Great Salt Lake
Pyramid Lake and the Eocene Green River Formation
Utah and surrounding states have become one of the many destinations for several international groups looking to better understand lacustrine reservoirs
“Great Salt Lake is an excellent locale to study recent microbialite formation as well as abiotic carbonate deposits,” says Michael Vanden Berg
Energy and Minerals Program Manager for the Utah Geologic Survey
coated grains and shoreline tufas are widespread in and around Great Salt Lake
Two readily accessible areas for study are Rozel Point in the northern portion of the lake and Bridger Bay located at the northern tip of Antelope Island
The early Great Salt Lake shoreline deposits at Lakeside also provide accessible meter-scale travertine mounds and associated microbialites from past higher lake levels.”
Travertine terraces at Mammoth Hot Springs
now exposed along the shoreline of Great Salt Lake
Holocene microbialite domes along the current margin of Great Salt Lake
Offshore from the travertine deposits are the various forms of the microbialites
such as those shown in the introductory photographs
“The alkaline groundwater can promote growth of both onshore travertine and lacustrine microbialites in the same depositional system,” says Dr
Researchers also discovered that different carbonate minerals are closely linked with specific depositional environments
Major lake level changes drove the geothermal alkaline groundwater systems
with a wide range of temperatures recorded from the travertines due to progressive flushing from depth and mixing with surface water
Travertine cascade coating stepped mini-terracette
Vents propagated from bedrock through mounds to feed travertine layers
“The real tale here at Lakeside is that we have travertine and microbialites that were deposited adjacent to each other and during the same intervals
showing that they are not mutually exclusive,” concludes Dr
“Travertines and microbialites compete in opposing scenarios that are commonly used for interpreting reservoir facies observed in South Atlantic late sag phase pre-salt lacustrine carbonates
Early Great Salt Lake shoreline deposits at Lakeside provide spectacular outcrop analogs for these reservoir facies.”
Webster’s observations are backed up by recent publications of the National Agency of Petroleum (ANP) for Brazil on Brazil’s pre-salt reservoirs
they identify the Itapema and Barra Velha formations in the Santos Basin as “carbonate rocks formed by coquinas and /or microbialites.” Petrobras used the present-day carbonate rocks deposited at Lagoa Salgada (Salty Lake) in Rio de Janeiro State as analogs to the reservoirs in the Santos Basin
The microbial carbonates are found in both the Santos and Campos basins
on the sag (post-rift) and upper rift layers
Wright has authored several more recent papers on the pre-salt lacustrine carbonates and also has studied some of the Utah ‘analogs’
“What we have found is that there are different reservoir types in the South Atlantic pre-salt,” says Dr
“Lake deposystems are controlled by often highly complex hydrological factors reflecting the interaction of local climate
tectonics and the composition of the catchment geology
We have a much clearer picture now of their diversity and what was controlling their compositions
Pre-Salt South Atlantic Carbonate Reservoirs
For the pre-salt South Atlantic reservoirs
it would seem that analogs abound around the world and greatly vary in ways we are only beginning to understand
Great Salt Lake provides one place where some of this variety comes together
from abiotic travertine deposits to bioherms in the form of reefs and carbonate buildups
It has become important to properly characterize the environment that led to carbonate deposition in order to explore these carbonate reservoirs
The Barra Velha Formation and its equivalents
“represent shallow lake deposits with the potential for similar facies present off the main structural blocks,” Dr
“The same facies can be found in the West African basins and may extend well east of the explored areas in both the Santos and Campos Basins
“The problem is there is no direct analog for these complex and highly productive reservoirs and that has caused a controversy over their interpretation,” adds Dr Wright
“Conditions in the Cretaceous were unique to that period in creating vast
probably due to CO2 derived from the mantle.”
as Michael Vanden Berg points out “Even though there may be no direct analogs
the general study of lacustrine deposits is still very important to the understanding of all lacustrine reservoirs
including the Cretaceous pre-salt reservoirs found offshore Brazil.”