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NARROW
GeoRef Subject
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all geography including DSDP/ODP Sites and Legs
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Africa
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East Africa
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Kenya (1)
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Lake Malawi (1)
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Tanzania (1)
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East African Lakes
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Lake Malawi (1)
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North Africa
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Tunisia (1)
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Southern Africa
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South Africa
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Cape Province region (1)
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Antarctica
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Brachiopoda (1)
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Protista
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Foraminifera
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Cassidulinacea
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Globigerinacea
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Orbitoidacea
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Cibicides (1)
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Textulariina
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Thecamoeba (1)
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microfossils (36)
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palynomorphs
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pollen (19)
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Plantae
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algae
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Spermatophyta
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geologic age
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Cenozoic
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upper Pleistocene
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upper Weichselian
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upper Wisconsinan (8)
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upper Quaternary
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Brunhes Chron (2)
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Stone Age
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Tertiary
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Paleozoic
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Permian
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Unayzah Formation (1)
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Silurian
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upper Paleozoic (1)
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upper Precambrian
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Tapley Hill Formation (1)
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igneous rocks
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metamorphic rocks
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Primary terms
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absolute age (68)
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Africa
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East Africa
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East African Lakes
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postglacial environment
Abstract Analyses of high-resolution multibeam and sub-bottom profiling data, acquired during marine geological field cruises between 2017 and 2019 in the eastern Gulf of Finland (Baltic Sea), enabled the detailed mapping of Quaternary deposits, and revealed diverse submerged glacial and post-glacial landforms (e.g. streamlined moraine ridges, large retreat moraine ridges, De Geer moraines and kettle holes). The morphology of these glacial features provides evidence of the ice-sheet retreat direction and rate throughout the deglaciation of the region, which occurred between 13.8 and 13.3 ka BP (Pandivere–Neva Stage) and 12.25 ka BP (Salpausselkä I Stage). Analysis of sub-bottom profiling, supported by piston long-core sampling, indicates periods of bottom erosion/non-deposition during the Holocene caused by relative water-level regressions. Significant negative relief features are also observed in the area for the first time. These linear and curved V-shaped furrows are several kilometres long and 5 m deep, and are tentatively ascribed to bottom current and gas-seepage processes.
The sulfur isotopic consequence of seawater sulfate distillation preserved in the Neoproterozoic Sete Lagoas post-glacial carbonate, eastern Brazil
Late Ordovician mass extinction caused by volcanism, warming, and anoxia, not cooling and glaciation: COMMENT
The Ichnological and Sedimentological Signature of a Late Paleozoic, Postglacial Marginal-Marine and Shallow-Marine, Tidally Influenced Setting: The Wudayhi Member of the Nuayyim Formation (Unayzah Group) in the Subsurface of Central and Eastern Saudi Arabia
Coral faunal turnover through the Ordovician–Silurian transition in South China and its global implications for carbonate stratigraphy and macroevolution
Abstract This paper focuses on the continental shelf of NW Australia, and on models for change in littoral and offshore environments of relevance to human occupation over the last 50 kyr. Major island groups occur on the shelf including the Montebello and Barrow islands, and those of the Dampier Archipelago. At lowest sea level around 22 ka, these would have been uplands that then became progressively isolated by subsequent sea-level rise. By integrating archaeological and zooarchaeological records from excavations on these islands with the geology and geomorphology, we interpret palaeoeconomic resource potential in relation to changing sea level and coastline morphology. The preservation potential for submerged archaeological sites and features is also assessed. Current archaeological evidence from these offshore islands indicates that the submerged coastal landscape is likely to have been a potentially rich environment for resources and human occupation, even at times of lowest sea level and regional aridity. Should any exploration of submerged archaeology be carried out in this region, it is likely to be rewarding, offering unique insights into Late Pleistocene coastal occupation.