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An Early Neolithic Grave and Occupation, and an Early Bronze Age Hearth on the Thames Foreshore at Yabsley Street, Blackwall, London

Published online by Cambridge University Press:  18 February 2014

Sarah Coles
Affiliation:
Thames Valley Archaeological Services Ltd, 47–9 De Beauvoir Road, Reading, RG1 5NR
Steve Ford
Affiliation:
Thames Valley Archaeological Services Ltd, 47–9 De Beauvoir Road, Reading, RG1 5NR
Andy Taylor
Affiliation:
Thames Valley Archaeological Services Ltd, 47–9 De Beauvoir Road, Reading, RG1 5NR

Abstract

Excavation on the Thames floodplain in London revealed traces of Early Neolithic occupation and burial on a sand and gravel bar beneath alluvium. A large expanse of peat also buried by alluvium was recorded between these finds and the modern river Thames suggesting that the occupation was situated on or close to the foreshore. A single grave cut into the natural sand contained a poorly preserved crouched inhumation, possibly of a woman. The burial was accompanied by a fragment of carinated bowl, a flint knife, and other struck flints. A radiocarbon date from an oak retaining plank within the grave of 5252±28 BP (4220–3970 cal BC: KIA20157) makes this burial one of the earliest from the British Isles and the earliest known for London. A scatter of struck flint and pottery predominantly of Early Neolithic date was recovered from adjacent areas of the sand. A nearby hearth contained fragments of Early Bronze Age pottery pointing to later prehistoric activity nearby.

Charred plant remains indicate both the collection of wild plant foods and cultivated cereals in the Early Neolithic. Radiocarbon dating of the adjacent peat deposits indicated their rapid growth within the Middle Bronze Age with a marked decline in woodland cover at the start of the sequence and a rise in grassland and herb species. Cereal pollen then briefly became a significant component of the sequence before declining to more modest levels.

Résumé

Des fouilles sur la plaine inondable de la Tamise à Londres ont révélé des traces d'occupation et d'inhumation du néolithique primitif sur une bande de sable et de gravier sous les alluvions. On a répertorié une vaste étendue de tourbe également enterrée sous les alluvions entre ces trouvailles et le cours actuel de la Tamise, ce qui donne à penser que cette occupation se situait sur ou près de la grève. Une seule tombe taillée dans le sable naturel contenait une inhumation accroupie mal préservée, peut-être une femme. L'inhumation s'accompagnait d'un fragment de bol caréné, d'un poignard de silex et d'autres silex martelés. Une datation au carbone 14 à partir d'une planche de rétention en chêne à l'intérieur de la tombe de 5252±28 BP (4220–3970 av.J.-C.cal: KIA20157) situe cette inhumation parmi les plus anciennes des îles britanniques et la plus ancienne connue à Londres. On a recouvré des silex martelés et des céramiques éparpillés datant du néolithique primitif dans des zones adjacentes du sable. Un foyer proche contenait pour la plus grande partie des tessons de céramique de l'âge du bronze ancien indiquant la proximité d'une activité préhistorique plus tardive.

Des restes de plantes carbonisés témoignent à la fois de la collecte de plantes sauvages pour se nourrir et de la culture de céréales au néolithique primitif. La datation au carbone 14 des dépôts de tourbe adjacents démontra leur rapide expansion au cours de l'âge du bronze moyen associée à un déclin notoire de la couverture forestière au début de la séquence et une augmentation des prés et des espèces herbeuses. Puis le pollen de céréales est devenu, pour une brève période, un élément important de la séquence avant de revenir à des niveaux plus modestes.

Zusammenfassung

Ausgrabungen eines unter Alluvium liegenden Sand-und Kiesstreifens in der Themseaue in London erbrachten Spuren Frühneolithischer Besiedlung und Gräber. Eine große, ebenfalls unter Alluvium und zwischen diesen Befunden und dem modernen Flusslauf der Themse liegende Torffläche weist darauf hin, dass sich die Besiedlung entweder bis direkt ans Ufer oder mindestens bis in die Nähe des Flussufers erstreckte. Ein Einzelgrab, das in den anstehenden Sand eingegraben war, enthielt eine schlecht erhaltene, wahrscheinlich weibliche Körperbestattung in Hockerlage. Die Beigaben bestanden aus einem Fragment einer knickwandigen Schale, einem Feuersteinmesser und anderen Feuersteinabschlägen. Ein Radiokarbondatum von 5252±28 BP (4220–3970 cal BC: KIA20157), das von einem Eichen-Halterungsbretts aus diesem Grab stammt, macht dieses Grab zu einem der ältesten Gräber auf den Britischen Inseln und zum Ältesten in London. Weiterhin wurde eine Streuung von Feuersteinabschlägen und vornehmlich frühneolithischen Scherben in der unmittelbaren Umgebung dokumentiert. Aus diesem Bereich stammt auch ein Herd mit frühbronzezeitlichen Scherben, was auch eine spätere Nutzung des Platzes nahe legt. Verkohlte Pflanzenreste deuten auf das Sammeln von Wildpflanzen und die Nutzung von domestiziertem Getreide im frühen Neolithikum hin. Die Radiokarbondatierung der nahe gelegenen Torfdeponierungen zeigen ihren raschen Anstieg in der Mittleren Bronzezeit, die am Beginn der Abfolge mit einem merklichen Rückgang der Waldgebiete und gleichzeitigem Zuwachs an Weideland und Kräuterarten einhergeht. Danach lässt sich ein kurzzeitiges, aber starkes Ansteigen der Getreidepollen in der Abfolge verzeichnen, bevor sie wieder zu einem geringen Anteil zurückkehren.

Résumen

La excavación de la planicie aluvial del Támesis en Londres ha revelado indicios de ocupación y enterramiento en el Neolítico Inicial en un banco de arena y gravilla bajo el aluvión. Entre estos hallazgos y el río Támesis moderno se registró una amplia extensión de turba también enterrada por aluvión, lo que sugiere que la ocupación estaba emplazada en o cerca de la zona de mareas. Una única tumba cavada en la arena natural contenía una inhumación en posición fetal pobremente preservada, posiblemente de una mujer. El enterramiento estaba acompañado de un fragmento de un cuenco carinado, un cuchillo de sílex, y otras muescas de sílex. La fecha del carbono-14 de una plancha de sujeción de roble de dentro del enterramiento es de 5252±28 BP (4220–3970 cal BC: KIA20157) y hace de esta tumba una de las más tempranas en la Islas Británicas y la más temprana conocida en Londres. De las zonas adyacentes de la arena se recuperó una dispersión de restos de sílex trabajado y de cerámica predominantemente del Primer Neolítico. Un hogar cercano contenía fragmentos de cerámica de la Primera Edad del Bronce indicando actividad prehistórica tardía en las cercanías.

Restos carbonizados de plantas indican tanto la recolección de plantas salvajes comestibles como la presencia de cereales cultivados en el Primer Neolítico. La datación al carbono-14 de los depósitos de turba adyacentes indica su rápido desarrollo en el Bronce Medio con un marcado descenso de la población de árboles al comienzo de la secuencia y un aumento de las especies de pradera y herbáceas. El polen de cereales se convierte brevemente en un componente significativo de la secuencia antes de reducirse a niveles más modestos.

Type
Research Article
Copyright
Copyright © The Prehistoric Society 2008

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