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NARROW
GeoRef Subject
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all geography including DSDP/ODP Sites and Legs
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Africa (1)
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Alexander Island (17)
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Antarctica
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sulfides
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Primary terms
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Far East
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biogeography (21)
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carbon
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C-14 (7)
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Neoglacial
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upper Holocene
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Little Ice Age (1)
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Pleistocene
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upper Pleistocene
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upper Weichselian
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Younger Dryas (1)
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upper Quaternary (1)
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Tertiary
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Topopah Spring Member (1)
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Pliocene
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upper Pliocene (2)
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Paleogene
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Eocene
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lower Eocene (2)
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middle Eocene
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Bartonian (1)
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upper Eocene
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La Meseta Formation (20)
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Oligocene
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lower Oligocene (2)
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Paleocene
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lower Paleocene
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Danian (1)
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K-T boundary (4)
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-
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Sobral Formation (3)
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upper Cenozoic (1)
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Chordata
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Vertebrata
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Pisces
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Chondrichthyes
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Neoselachii (1)
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Osteichthyes
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Actinopterygii
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Teleostei (1)
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Mammalia
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Theria
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Metatheria
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Marsupialia (1)
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Reptilia
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Diapsida
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Lepidosauria
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Squamata
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climate change (8)
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deformation (8)
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diagenesis (8)
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earthquakes (2)
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Europe
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Fossil barnacles from the Antarctic Peninsula: refining ways of exploring the nature of rare and/or delicate specimens employing X-ray Computer Tomography (CT)
Phylogeny of the Eocene Antarctic Tapetinae Gray, 1851 (Bivalvia, Veneridae) from the La Meseta and Submeseta formations
Subannual stable isotope records reveal climate warming and seasonal anoxia associated with two extinction intervals across the Cretaceous-Paleogene boundary on Seymour Island, Antarctica
Calcium isotope evidence for environmental variability before and across the Cretaceous-Paleogene mass extinction
Dinoflagellate cysts of the La Meseta Formation (middle to late Eocene), Antarctic Peninsula: implications for biostratigraphy, palaeoceanography and palaeoenvironment
Terrestrial and marine floral response to latest Eocene and Oligocene events on the Antarctic Peninsula
Spatially coherent late Holocene Antarctic Peninsula surface air temperature variability
Variations in ice-sheet dynamics along the Amundsen Sea and Bellingshausen Sea West Antarctic Ice Sheet margin
Estimating the number of pulses in a mass extinction
Episodicity within a mid-Cretaceous magmatic flare-up in West Antarctica: U-Pb ages of the Lassiter Coast intrusive suite, Antarctic Peninsula, and correlations along the Gondwana margin
Abstract The Gebra–Magia Complex is an important example of a submarine mass-movement composite located on the lower continental slope of the Antarctic Peninsula (Central Bransfield Basin). Continuous instability dynamics over time is inferred to have affected the palaeo-trough-mouth fans present in the study area. The depositional architecture and the outstanding relief of the Gebra Valley, which is the most striking morphological feature in the area, determine the asymmetrical morphology of the complex. This complex is characterized, from east to west, by an open-slope margin flanking the sidewall of the Gebra Valley, the Gebra Valley itself and a SW margin that is connected to the Magia area by a large scar approximately 7.8 km to the SW. The Gebra Valley is a Quaternary debris valley resulting from repeated large-scale mass-transport and cut-and-fill processes. In contrast, the Magia area is dominated by unchannelized sedimentary instability processes, resulting in a different sedimentary architecture and morphology. The near-surface sediments in the Gebra–Magia Complex document the continuous occurrence of recent mass movements, as also evidenced by flows transported downslope as unchannelized or channelized flows. Climate and tectonic activity are considered the primary factors controlling the development of the complex.