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Paleoenvironmental events during the last 13,000 years in the central Red Sea as recorded by pteropoda

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Paleoenvironmental events during the last 13,000 years in the central Red Sea as recorded by pteropoda (English)

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Ahuva Almogi-Labin

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Christoph Hemleben

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2

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Dieter Meischner

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Helmut Erlenkeuser

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4

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publication date

February 1991

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Paleoceanography

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6

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1

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page(s)

83-98

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The surface of the ice-age Earth

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Climatic changes of the last 18,000 years: observations and model simulations

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Deglacial warming of the northeastern Atlantic ocean: correlation with the paleoclimatic evolution of the european continent

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Direct dating of the oxygen-isotope record of the last deglaciation by 14C accelerator mass spectrometry

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A 17,000-year glacio-eustatic sea level record: influence of glacial melting rates on the Younger Dryas event and deep-ocean circulation

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Evidence for two-step deglaciation and its impact on North Atlantic deep-water circulation

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A wetter climate in eastern Sudan 2,000 years ago?

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Sediment and pollen evidence for an early to mid-Holocene humid period in the eastern Sahara

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Glacio-eustatic sea-level control on Red Sea salinity

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Climatic conditions deduced from a 150-kyr oxygen isotope–pollen record from the Arabian Sea

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Seasonal variation in the flux of euthecosomatous pteropods collected in a deep sediment trap in the Sargasso Sea

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Stratigraphic and paleoceanographic significance of Late Quaternary pteropods from deep-sea cores in the Gulf of Aqaba (Elat) and northernmost Red Sea

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(Q107105127)

Paleoenvironmental events during the last 13,000 years in the central Red Sea as recorded by pteropoda

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