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Situating prehistoric sites in their past environment helps us to understand their functionality and the organization of early sedentary human societies
this is a challenge as the natural environment constantly evolves through time and erases these constructions
This study introduces a reassessment of the paleo-landscape evolution around the Neolithic enclosures at the Noyen-sur-Seine site based on new field observations as well as the synthesis of (un)published and new radiocarbon dating
our results show that the Noyen enclosures were not built along a Neolithic Seine River: the nearby channels were active in the Middle Age and Early Modern periods
the results show that the enclosures were originally much larger: only a fraction that survived river erosion (lateral migration rates up to 2–3 m yr−1 estimated during the nineteenth century) has been preserved
an abandoned Mesolithic Seine River served as a natural delimitation of the SE part of the Neolithic enclosures
These results indicate that Neolithic enclosures in alluvial settings are often only partly preserved and that societies from that period lived farther away from active rivers than originally thought
the perception of archaeological sites in their current landscape may be different from their original configurations
a careful reconstitution of the landscape evolution dynamics based on geomorphic and sedimentary analyses is necessary before proceeding to further interpretations of the dynamics of early settlement
Note that (a) and (b) have a circular shape and that the limit of (c)
(d) and (e) correspond to erosional boundaries
(e′) early reconstruction of the Noyen-sur-Seine landscape
it is assumed that the B enclosure was delimited by a Neolithic Seine River
which implied the implantation of early sedentary societies by the river
this model is challenged by showing that the erosional boundaries occurred in Noyen-sur-Seine much later than the Neolithic
crescent bars (dashed white lines) and Neolithic enclosures (orange dashed lines)
A chronology with the relative and absolute dating of channels a to h
as well as the two monoxyle pirogues are presented
The white dots correspond to locations where field observations and/or radiocarbon sampling were performed
hypotheses on the age of channels at Noyen-sur-Seine were behind the suggestion that a first Neolithic enclosure took advantage of the meander as a natural delimitation and that a second
later Neolithic enclosure was built along the Seine River
the age of these channels was never determined
and the early interpretation remained entrenched in the community
A reassessment of the chronologies of channels migration and abandonment seems therefore necessary
both directly—by dating the organic infill of the abandoned using radiocarbon techniques—and indirectly—by assessing the lateral migration rate and paths of the paleo-Seine River based on the analysis of historical maps
We show that the Neolithic configuration of the site was different than originally thought and we discuss the broader implications for the location and size of enclosures in alluvial settings
(b) Distribution of the estimated migration distance for the left bank (thin black curve) and right bank (thin blue curve) as well as the total (thick black curve)
Some corresponding lateral migration rates are indicated in red
The migration rates are calculated by dividing the distance by the time between maps (i.e.
It seems more plausible that they would have been at least partly eroded
A radiocarbon age calculated on a 40 cm deep sample within the channel d sediment returned a date of 1811–1917 yrs cal
historical maps and radiocarbon dating of the sediment infill of the abandoned channels demonstrated that the abandonment of the channel to the north of the enclosure is much more recent than the Neolithic period
the northern d channel was never a boundary for the Neolithic enclosure as it was abandoned much more recently (i.e.
whose bankfull activity dated back to the Mesolithic
was much shallower during the Neolithic period
no bankfull active Neolithic Seine River could be identified in the vicinity of the Neolithic enclosures
it is possible to estimate the southward lateral migration rate of the Seine River after the cutoff event from ca
The two values are relatively close and consistent with modern and centennial estimates
They further indicate that the d and f channels were eroded over a distance of at least several hundreds of meters along the enclosure perimeter before being abandoned
Reconstructed evolution of the landscape since the Mesolithic showing the progressive erosion of the Neolithic enclosures due to the migration of the Seine River
The reconstruction supports the hypothesis that a system of large
circular enclosures was progressively eroded along the bank of the laterally migrating Seine River
The locus where the two pirogues were abandoned is also reported
near the h channel) were therefore more likely to be occupied as shown by the enclosures of Noyen-sur-Seine
the more likely it is to have been mostly eroded away
we suggest that they most likely have the same preservation bias as in Noyen-sur-Seine
and that the edges of these enclosures correspond to erosional boundaries
Systematic dating of abandoned alluvial channels in their surroundings should make it possible to differentiate between the channels that were contemporaneous with these edifices and those that postdated and eroded them
These results should encourage a more systematic use of regional geomorphological investigations in archeology
in particular via the dating of paleochannels
the palimpsest of alluvial traces (channels from different periods) must be subjected to a diachronic analysis to reconstruct the contemporary paleo-landscape of the Neolithic occupations
this geo-archaeological approach makes it possible to address the question of how these environments were perceived and managed by ancient societies given that the sedimentary and archaeological archives are systematically incomplete
The two maps were georeferenced based on reference points that are still observed on the current cadaster (e.g.
27 reference points were used with uncertainties for position ranging from 4 to 40 m with an average of 18 m
The right and left bank were manually calculated for the 1785 and 1848 paths of the Seine River using the ArcGIS software
The fit for the migration distribution for the left and right banks is shown for comparison
The migration rates were computed by dividing the migration distances by the time span between the two maps
Field sampling to carry out radiocarbon dating of the abandoned channel sediment infill was conducted using a hand auger
or a peat borer in the organic-rich levels
grainsize) were described directly in the field in the form of sedimentary logs
The cross-section of the f channel was constructed by interpolation between the sedimentary logs
Radiocarbon dating was performed on organic sediment or plant found along these logs in two laboratories: Beta Analytic Inc
in the USA and Poznan Radiocarbon Laboratory in Poland
The datasets used and/or analyzed during the current study are available from the corresponding author upon reasonable request
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Enclosures in Neolithic Europe: Essays on Causewayed and Non-causewayed Sites (Oxbow Books
Fortifications and enclosures in European prehistory: a cross-cultural perspective
The role of enclosures in territorial organization in the Paris Basin between 4500 and 3800 BC
Genèse et évolution des enceintes du bassin Seine-Yonne au cours du Néolithique moyen et récent 144–157 (Conseil départemental de l’Aube; Éditions Snoeck
Geomorphological assessment of the preservation of archaeological tell sites
Evolution of the Rhône delta plain in the Holocene
The topography and excavation of Heracleion-Thonis and East Canopus (1996–2006)
Palaeolithic geoarchaeology: Palaeolandscape modelling and scales of investigation
Counter-intuitive influence of Himalayan river morphodynamics on Indus Civilisation urban settlements
Nile waterscapes facilitated the construction of the Giza pyramids during the 3rd millennium BCE
Dating the landscape evolution around the Chauvet-Pont d’Arc cave
Interpreting avulsion process from ancient alluvial sequences: Guadalope-Matarranya system (northern Spain) and Wasatch Formation (western Colorado)
Preservation and completeness of fluvial meandering deposits influenced by channel motions and overbank sedimentation
Cardenas, B. T., Lamb, M. P., Jobe, Z. R., Mohrig, D. & Swartz, J. M. Morphodynamic Preservation of Fluvial Channel Belts. Sediment. Rec. https://doi.org/10.2110/001c.66285 (2023)
Sediment accumulation rates and the completeness of stratigraphic sections
Les enceintes «néolithiques» du Bassin parisien
Place dans l’évolution socio-économique du Néolithique régional
‘Very like the Neolithic’: The everyday and settlement in the European Neolithic
In The Neolithic of Europe: papers in honour of Alasdair Whittle 7–23 (Oxbow Books
Sur Habitats Plein Air Entre Loire Neckar Actes Table Ronde Int
recherche sur les périodes paléolithiques antérieures au Dernier Maximum Glaciaire en archéologie preventive
Spatial and temporal patterns of the upper Pleistocene alluvial fill deposits of the upstream Seine River alluvial plain
Possibilité aquifère des alluvions du val de seine entre Nogent-sur-Seine et Montereau
River system evolution and environmental changes during the Lateglacial in the Paris Basin (France)
Le Tardiglaciaire des fonds de vallée du Bassin parisien (France)
Les remplissages sédimentaires des chenaux du Tardiglaciaire de la Bassée à Bazoches-lès-Bray (77): nouveau bilan d’étape
Paléolithique Final Mésolithique Dans Bassin Paris
Caractérisation des hétérogénéités sédimentaires d’une plaine alluviale: Exemple de l’évolution de la Seine supérieure depuis le dernier maximum glaciaire
L’enceinte néolithique de Noyen-sur-Seine (Seine-et-Marne)
et al 229–258 (Paléoenvironnement et pirogue carolingienne à Noyen-sur-Seine
Dix années de recherches à Noyen-sur-Seine (Seine-et-Marne)
site mésolithique en milieu humide fluviatile in L’Homme et l’eau au temps de la Préhistoire
Noyen-sur-Seine: a Mesolithic waterside settlement
Nouveau regard sur les occupations du second Mésolithique du «Haut des Nachères» à Noyen-sur-Seine (Seine et Marne)
The evolution of the Seine basin water bodies through historical maps
Computing and visualizing dynamic time warping alignments in R: The dtw package
Large sinuous rivers are slowing down in a warming Arctic
Submarine channel stacking patterns controlled by the autogenic 3D kinematics of meander bends
Flood plain and channel dynamics of the Quinault and Queets Rivers
Quantifying the effect of riparian forest versus agricultural vegetation on river meander migration rates
A tenfold slowdown in river meander migration driven by plant life
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La barque monoxyle carolingienne de Noyen-sur-Seine (Seine-et-Marne)
Bedload infilling and depositional patterns in chute cutoffs channels of a gravel-bed river: The Ain River
site néolithique du" Champ de bataille" à l’Etoile (Somme): Une enceinte à fossé interrompu
L’implantation de l’enceinte monumentale de La Villeneuve-au-Châtelot (Aube) du Néolithique récent à la confluence Seine-Aube: premiers résultats géoarchéologiques
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Carte géologique de la France à 1/1 000 000
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This research was part of the PIREN Seine program
We thank Jacques Rivoirard for fruitful discussions on spatial uncertainties
The English was carefully revised by Sara Mullin and Michelle Elliott
We thank editor Randolph Donahue and two anonymous reviewers for their constructive comments
PSL University/MINES Paris/Centre de Géosciences
Département de Seine-et-Marne/Centre departemental d’archéologie de la Bassée
The authors declare no competing interests
Springer Nature remains neutral with regard to jurisdictional claims in published maps and institutional affiliations
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The Humans of Shuttle Time series from the Badminton World Federation shares the viewpoints of those who contribute to grassroots badminton development
shuttle time teacher from Wallis and Futuna
Badminton Oceania’s most recent member association shares her story of how she got into badminton and the influence she is having on the development within the region through the shuttle time program
I played many sports since I was 12: mainly gymnastics and athletics
I was in the scouts since I was eight and that gave me the opportunity to discover community life
I organised a project in 2003 to make a class for children in a small village in Burkina Faso
I’ve been a primary school teacher for 15 years in France but I live in Wallis and Futuna thanks to my husband’s job
I practiced badminton first when I was at college
I liked this sport but had no opportunity to practice badminton in a club
I discovered a club life because he was involved in his club (La Bassée Badminton Club)
I played the sport for two years and liked it
we involved the Uvea Badminton Club and started training children between the ages of 6 and 16
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Badminton is an individual and a collective sport and can be played at any age
I had the chance to develop badminton at school in Wallis with a dynamic team
we conducted badminton clinics for children in the Uvea Badminton Club
In Wallis and Futuna there was no badminton in primary school
Teachers never had any knowledge of this sport
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Shuttle Time allows you to discover an individual sport
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A protest by amusement park owners has seen trucks block traffic on several roads in France
The protesters are demanding a clear date from which they can reopen their attractions to the public
According to Northern French Newspaper lavoixdunord.fr
France’s amusement park industry want a firm reopening date set by the government
The earliest such attractions could reopen is June 9th
and it is expected that some regions wont allow amusement parks to open until July or even August
besides the danger of losing vital summer income
has thus motivated France’s 50,000 fairground and amusement professionals to protest
The protesters said this morning that the trucks would avoid city centres and that they do not aim to disrupt work
Disturbances are expected on the A16 (Boulogne-Calais)
the A25 (Dunkirk-Lille) and at the A2 toll (Valenciennes-Cambrai)
the truck protests were present in the following locations:
Pölös Zsófia Journalist Trans.info | 6.05.2025
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Forty feet below the fields in Northern France hides a secret history
one that dates back more than a hundred years
Tunnels were first dug during the First World War to mine under enemy positions and detonate bombs or attack in desperate and fierce fights
they developed another purpose: providing soldiers with safer accommodation and communication routes
Miners and engineers from Britain and Australia began tunnelling near Hulluch in 1916 in the wake of the Battle of Loos
“In 1918 these were all interlinked and it was possible to walk underground from the La Bassée canal
“Troops were accommodated in there but in particular it provided safe passage for the troops
“Call them underground communications trenches
off which you then had all the dugouts and rest of it.”
bomb disposal operators and archaeologists is now restoring the subway system and giving valuable insight into underground warfare
The Durand Group have big plans for the tunnels and the 3km they have uncovered bring an unseen part of First World War history to light
Soldiers did not live in the tunnels permanently
but they would often work underground for several days at a time
First World War graffiti remains engraved on the tunnel walls
acting as an insight into the soldiers’ lives who served there
The Durand Group said: “You’ve probably got several hundred men operating and living down here all the time
so you have that sweat and effort going on
in the living areas they would have had latrines
there were cookhouses down here as well so there would have been cooking smells
“Plus that constant risk of artillery fire coming in so the whole thing would vibrate… dust.”
the tunnels were used again when a redesign was started for a corps headquarters
before being abandoned due to the advancing German forces
Having painstakingly restored much of the tunnels
the Durand Group now want to invite people in to walk more than a kilometre underground
The Loos Big Walk is a 26-kilometre route across
the battlefields of the Western Front proposed by the Durand Group for interested members of the public
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