Benthic foraminiferal fauna in the Ionian Sea

Fuente: PANGAEA
Enregistré dans:
Détails bibliographiques
Auteurs principaux: Schmiedl, Gerhard, Hemleben, Christoph, Keller, Jörg, Segl, Monika
Format: Dataset Open Access
Langue:en
Publié: PANGAEA 1998
Sujets:
Accès en ligne:
Tags: Ajouter un tag
Pas de tags, Soyez le premier à ajouter un tag!
_version_ 1867167662538227712
author Schmiedl, Gerhard
Hemleben, Christoph
Keller, Jörg
Segl, Monika
author_facet Schmiedl, Gerhard
Hemleben, Christoph
Keller, Jörg
Segl, Monika
collection Datos científicos de ciencias marinas y ambientales
contents To reconstruct paleoceanographic changes in the eastern Mediterranean during the last 330,000 years, we studied benthic foraminifera in a piston core from the Ionian Sea. The fauna exhibits large fluctuations in foraminiferal number, diversity, and species composition. Interglacials are characterized by low foraminiferal number and diversity indicating oligotrophic conditions. Directly below or above interglacial sapropels, increased numbers of low-oxygen-tolerant species indicate a strong reduction of deep water circulation. Glacials are characterized by increased foraminiferal number and diversity and faunas that are dominated by shallow infaunal species indicating mesotrophic conditions. Around glacial sapropel S6 very high foraminiferal numbers and the dominance of shallow and deep infaunal species suggest enhanced organic matter fluxes. These faunal results provide information about changes in the African and North Atlantic climate systems (monsoon and westerlies) controlling the humidity and wind stress in the Mediterranean region.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_732318
institution PANGAEA
language en
publishDate 1998
publisher PANGAEA
record_format pangaea
spellingShingle Benthic foraminiferal fauna in the Ionian Sea
Schmiedl, Gerhard
Hemleben, Christoph
Keller, Jörg
Segl, Monika
25/4-13; GeoTü; KL; M25/4; M25/4-KL13; Meteor (1986); Paleoceanography at Tübingen University; Piston corer (BGR type); SESAME; Southern European Seas: Assessing and Modelling Ecosystem Changes
To reconstruct paleoceanographic changes in the eastern Mediterranean during the last 330,000 years, we studied benthic foraminifera in a piston core from the Ionian Sea. The fauna exhibits large fluctuations in foraminiferal number, diversity, and species composition. Interglacials are characterized by low foraminiferal number and diversity indicating oligotrophic conditions. Directly below or above interglacial sapropels, increased numbers of low-oxygen-tolerant species indicate a strong reduction of deep water circulation. Glacials are characterized by increased foraminiferal number and diversity and faunas that are dominated by shallow infaunal species indicating mesotrophic conditions. Around glacial sapropel S6 very high foraminiferal numbers and the dominance of shallow and deep infaunal species suggest enhanced organic matter fluxes. These faunal results provide information about changes in the African and North Atlantic climate systems (monsoon and westerlies) controlling the humidity and wind stress in the Mediterranean region.
title Benthic foraminiferal fauna in the Ionian Sea
topic 25/4-13; GeoTü; KL; M25/4; M25/4-KL13; Meteor (1986); Paleoceanography at Tübingen University; Piston corer (BGR type); SESAME; Southern European Seas: Assessing and Modelling Ecosystem Changes
url https://doi.org/10.1594/PANGAEA.732318