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Ocean driven retreat of the Northeast Greenland Ice Stream following the Last Glacial Maximum. [PDF]
Callard SL +6 more
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Sequence stratigraphy of the syn-rift miocene succession in the Abu Rudeis-Sidri Field, Gulf of Suez, Egypt. [PDF]
Assal EM +4 more
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Relatively warm deep-water formation persisted in the Last Glacial Maximum. [PDF]
Wharton JH +6 more
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Contrasting evolution of the Arabian Sea and Pacific Ocean oxygen minimum zones during the Miocene. [PDF]
Hess AV +4 more
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Ecology of Benthic Foraminifera
Notes for a Short Course: Studies in Geology, 1982Benthic foraminifera live in a wide variety of marine habitats, from marshes to abyssal plains. Both epifaunal and infaunal adaptations are present. The distribution of species is controlled by a complex of abiotic and biotic variables of the environment, usually resulting in a depth-zonation of assemblages on continental margins.The composition of the
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Benthic Foraminifera: Response to Environment
1984As pointed out in the previous chapter, the response of each benthic species to the abiotic and biotic conditions in its environment is a specific one, reflected by its particular life history. An attempt is made in the following to summarize and integrate in situ observations, experimental evidence and assumptions based on circumstantial evidence ...
Zeev Reiss, Lukas Hottinger
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Benthic behavior of planktic foraminifera
Geology, 1996In culture containers with sediment on the bottom, two of six species of planktic foraminifera reveal characteristic benthic activities, such as reorientation, crawling, and burrowing. Globigerinella siphonifera creates well-organized burrows and excavated sediment on a circular pile.
Heinz Hilbrecht, Hans R. Thierstein
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Biogeography of Modern Benthic Foraminifera
Notes for a Short Course: Studies in Geology, 1982Biogeography is concerned with recording and explaining the distribution of organisms in space and time. In their search for patterns of distribution, biogeographers have classified the surface of the earth into a hierarchical scheme of ecological units (e.g. Kauffman and Scott, 1976). The basic biogeographic units are realms and provinces.
Martin A. Buzas, Stephen J. Culver
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Biogeography of neritic benthic Foraminifera
1999Large-scale biogeographic distributions of benthic Foraminifera of the world’s shelves exhibit a pattern that indicates a major controlling role for temperature at this scale. Cold-, temperate-, and warm-water groupings of provinces have been recognized around the world, with a greater number of provinces delineated in warmer regions. Modern provincial
Stephen J. Culver, Martin A. Buzas
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Benthic foraminifera assemblages at Great Meteor Seamount
Marine Biology, 2004Foraminiferal assemblages found at Great Meteor Seamount were studied in August 1998. Communities of living foraminifera in surface sediments from the plateau (290–325 m water depth) and from the surrounding base (2,300–4,096 m) were compared in abundances, diversity, and species composition.
Heinz, Petra, Ruepp, D., Hemleben, C.
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