Benthic foraminiferal assemblages in surface sediments of the Elbe estuary

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Auteur principal: Wang, Pinxian
Format: Dataset Open Access
Langue:en
Publié: PANGAEA 1983
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author Wang, Pinxian
author_facet Wang, Pinxian
collection Datos científicos de ciencias marinas y ambientales
contents Two foraminiferal assemblages are observed in surface sediments of the Elbe estuarv. an Elphidium excavatum assemblaae and an Ahmonia/Protelphidium assemblage. They are the result of test-size sorting in accordance to the grain size of the sediments. These assemblages of mainly empty tests differ basically from the living population, which is dominated exclusively by E. excavatum. The average test size is decreasing when advancing from the Open sea into the estuary and the living fauna disappears near the entrance of the Kiel Canal. In the dead assemblage the diversity is distinctively higher and the average test size varies with the grain size of the sediment. The assemblages found in plankton tows are nearly identical with those in corresponding bottom samples. This indicates the distribution pattern to be caused by transport in currents (mainly in suspension). This type of foraminiferal assemblages characterize macro- and mesotidal estuaries and might indicate a high tidal range when observed in sediments of fossil estuaries.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_786406
institution PANGAEA
language en
publishDate 1983
publisher PANGAEA
record_format pangaea
spellingShingle Benthic foraminiferal assemblages in surface sediments of the Elbe estuary
Wang, Pinxian
GIK/IfG; Institute for Geosciences, Christian Albrechts University, Kiel
Two foraminiferal assemblages are observed in surface sediments of the Elbe estuarv. an Elphidium excavatum assemblaae and an Ahmonia/Protelphidium assemblage. They are the result of test-size sorting in accordance to the grain size of the sediments. These assemblages of mainly empty tests differ basically from the living population, which is dominated exclusively by E. excavatum. The average test size is decreasing when advancing from the Open sea into the estuary and the living fauna disappears near the entrance of the Kiel Canal. In the dead assemblage the diversity is distinctively higher and the average test size varies with the grain size of the sediment. The assemblages found in plankton tows are nearly identical with those in corresponding bottom samples. This indicates the distribution pattern to be caused by transport in currents (mainly in suspension). This type of foraminiferal assemblages characterize macro- and mesotidal estuaries and might indicate a high tidal range when observed in sediments of fossil estuaries.
title Benthic foraminiferal assemblages in surface sediments of the Elbe estuary
topic GIK/IfG; Institute for Geosciences, Christian Albrechts University, Kiel
url https://doi.org/10.1594/PANGAEA.786406