Late Pleistocene Shelf-Perched Lowstand Wedges on the Rhône Continental Shelf

The major Pleistocene deposits and landforms on southwestern Vancouver Island are the result of the Late Wisconsin (Fraser) Glaciation. Cordilleran glaciers formed in the Vancouver Island Mountains and in the Coast Mountains had advanced down Strait of Georgia to southeastern Vancouver Island after 19 000 years BP. The ice split into the Puget and Juan de Fuca lobes, the latter damming small lakes along the southwestern coastal slope of the island. During the maximum of the glaciation (Vashon Stade), southern Vancouver Island lay completely under the cover of an ice-sheet which flowed in a south-southwesterly direction across Juan de Fuca Strait, eventually terminating on the edge of the continental shelf. Deglaciation was by downwasting during which ice thinned into major valleys and the strait. Most upland areas were free of ice down to an elevation of 400 m by before 13 000 years BP. A possible glacier standstill and (or) resurgence occurred along Juan de Fuca Strait and in some interior upland valleys before deglaciation was complete. Glacial lakes occupied major valleys during later stages of deglaciation.

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Influence of late Pleistocene glaciations on the hydrogeology of the continental shelf offshore Massachusetts, USA

Geochemistry Geophysics Geosystems ◽

10.1002/2014gc005569 ◽

2014 ◽

Vol 15 (12) ◽

pp. 4651-4670 ◽

Cited By ~ 10

Author(s):

Jacob Siegel ◽

Mark Person ◽

Brandon Dugan ◽

Denis Cohen ◽

Daniel Lizarralde ◽

...

Keyword(s):

Continental Shelf ◽

Late Pleistocene ◽

Pleistocene Glaciations

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Late-Pleistocene evolution of the continental shelf of central Israel, a case study from Hadera

Geomorphology ◽

10.1016/j.geomorph.2016.03.008 ◽

2016 ◽

Vol 261 ◽

pp. 200-211 ◽

Cited By ~ 11

Author(s):

Gilad Shtienberg ◽

Justin Dix ◽

Nicolas Waldmann ◽

Yizhaq Makovsky ◽

Arik Golan ◽

...

Keyword(s):

Continental Shelf ◽

Late Pleistocene

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Coastal occupation and foraging during the last glacial maximum and early Holocene at Waterfall Bluff, eastern Pondoland, South Africa

Quaternary Research ◽

10.1017/qua.2020.26 ◽

2020 ◽

Vol 97 ◽

pp. 1-41 ◽

Cited By ~ 2

Author(s):

Erich C. Fisher ◽

Hayley C. Cawthra ◽

Irene Esteban ◽

Antonieta Jerardino ◽

Frank H. Neumann ◽

...

Keyword(s):

South Africa ◽

Continental Shelf ◽

Last Glacial Maximum ◽

Late Pleistocene ◽

Marine Fish ◽

Hunter Gatherers ◽

The Holocene ◽

Last Glacial ◽

The Last Glacial Maximum ◽

The Last Glacial

AbstractWaterfall Bluff is a rock shelter in eastern Pondoland, South Africa, adjacent to a narrow continental shelf that limited coastline movements across glacial/interglacial cycles. The archaeological deposits are characterized by well-preserved stratigraphy, faunal, and botanical remains alongside abundant stone artifacts and other materials. A comprehensive dating protocol consisting of 5 optically stimulated luminescence ages and 51 accelerator mass spectrometry 14C ages shows that the record of hunter-gatherer occupations at Waterfall Bluff persisted from the late Pleistocene to the Holocene, spanning the last glacial maximum and the transition from the Pleistocene to the Holocene. Here, we provide detailed descriptions about the sedimentary sequence, chronology, and characteristics of the archaeological deposits at Waterfall Bluff. Remains of marine mollusks and marine fish also show, for the first time, that coastal foraging was a component of some hunter-gatherer groups’ subsistence practices during glacial phases in the late Pleistocene. The presence of marine fish and shellfish further demonstrates that hunter-gatherers selectively targeted coastal resources from intertidal and estuarine habitats. Our results therefore underscore the idea that Pondoland's coastline remained a stable and predictable point on the landscape over the last glacial/interglacial transition being well positioned for hunter-gatherers to access resources from the nearby coastline, narrow continental shelf, and inland areas.

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