Sediment drifts on the continental rise are located proximal to the western side of the Antarctic Peninsula and recorded changes in glacial volume and thermal regime over the last ca. 15 m.y. At Ocean Drilling Program (ODP) Site 1101 (Leg 178), which recovered sediments back to 3.1 Ma, glacial -interglacial cyclicity was identified based on the biogenic component and sedimentary structures observed in X-radiographs, magnetic susceptibility and lithofacies descriptions. Glacial intervals are dominated by fine-grained laminated mud and interglacial units consist of bioturbated muds enriched in biogenic components. From 2.2 to 0.76 Ma, planktonic foraminifera and calcareous nannofossils dominate in the interglacials suggesting a shift of the A...
Grain size analysis of the terrigenous fraction of a laminated diatom ooze dating back to 11.4 kyr r...
Late Miocene to Recent sediments offshore from the Antarctic Peninsula are predominantly lithogenic,...
The presented sedimentological, geochemical and paleoceanographical work is intended to improve the ...
Sediment drifts on the continental rise are located proximal to the western side of the Antarctic Pe...
The continental rise west of the Antarctic Peninsula includes a number of large sediment mounds inte...
The effects of glaciation on sediment drifts is recognised from marked sedimentary facies variation ...
Sediment drifts on the continental rise west of the Antarctic Peninsula received fine-grained sedime...
The Pacific margin of the Antarctic Peninsula was drilled during Ocean Drilling Program (ODP) Leg 17...
Abstract On high‐latitude continental margins sediment is supplied from land to the deep sea through...
The Perseverance Drift, on the northern Antarctic Peninsula continental shelf, records changes in oc...
The area west of the Antarctic Peninsula is a key region for studying and understanding the history ...
Geologic studies of sediment deposited by glaciers can provide crucial insights into the subglacial ...
The SEDANO Project recovered 19 gravity cores on sediment drifts from the Pacific continental margin...
During the Pleistocene period Antarctica underwent cyclic variations in ice volume known as glacial ...
The direct record of Late Miocene-Early Pliocene Antarctic Peninsula Ice Sheet expansions from a pre...
Grain size analysis of the terrigenous fraction of a laminated diatom ooze dating back to 11.4 kyr r...
Late Miocene to Recent sediments offshore from the Antarctic Peninsula are predominantly lithogenic,...
The presented sedimentological, geochemical and paleoceanographical work is intended to improve the ...
Sediment drifts on the continental rise are located proximal to the western side of the Antarctic Pe...
The continental rise west of the Antarctic Peninsula includes a number of large sediment mounds inte...
The effects of glaciation on sediment drifts is recognised from marked sedimentary facies variation ...
Sediment drifts on the continental rise west of the Antarctic Peninsula received fine-grained sedime...
The Pacific margin of the Antarctic Peninsula was drilled during Ocean Drilling Program (ODP) Leg 17...
Abstract On high‐latitude continental margins sediment is supplied from land to the deep sea through...
The Perseverance Drift, on the northern Antarctic Peninsula continental shelf, records changes in oc...
The area west of the Antarctic Peninsula is a key region for studying and understanding the history ...
Geologic studies of sediment deposited by glaciers can provide crucial insights into the subglacial ...
The SEDANO Project recovered 19 gravity cores on sediment drifts from the Pacific continental margin...
During the Pleistocene period Antarctica underwent cyclic variations in ice volume known as glacial ...
The direct record of Late Miocene-Early Pliocene Antarctic Peninsula Ice Sheet expansions from a pre...
Grain size analysis of the terrigenous fraction of a laminated diatom ooze dating back to 11.4 kyr r...
Late Miocene to Recent sediments offshore from the Antarctic Peninsula are predominantly lithogenic,...
The presented sedimentological, geochemical and paleoceanographical work is intended to improve the ...