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Main Authors: Meier, K J Sebastian, Zonneveld, Karin A F, Kasten, Sabine, Willems, Helmut
Format: Dataset Open Access
Language:en
Published: PANGAEA 2004
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Online Access:https://doi.org/10.1594/PANGAEA.736594
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author Meier, K J Sebastian
Zonneveld, Karin A F
Kasten, Sabine
Willems, Helmut
author_facet Meier, K J Sebastian
Zonneveld, Karin A F
Kasten, Sabine
Willems, Helmut
collection Datos científicos de ciencias marinas y ambientales
contents Comparison of calcareous dinoflagellate cyst assemblages with Ba, Al, Mn, and Fe records from three sediment cores collected in the eastern Mediterranean Sea indicate that calcareous dinoflagellate cysts are generally resistant to postdepositional dissolution. Cyst association changes during and after sapropel S1 formation can therefore be closely related to variability in surface water productivity. Two groups of cysts are defined: those having highest abundances within the sapropelic and postsapropelic sediments. The temporal cyst distributions suggest increased freshwater input mainly from the Nile and a shallowing of the pycnocline as the most important processes increasing nutrient concentration in the photic zone, thus leading to increased productivity and organic carbon fluxes during sapropel formation. Furthermore, a general warming trend at the beginning of S1 formation and a slight salinity decrease are reconstructed.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_736594
institution PANGAEA
language en
publishDate 2004
publisher PANGAEA
record_format pangaea
spellingShingle Calcareous dinoflagellate cysts and geochemistry of Mediterranean Sea sediments
Meier, K J Sebastian
Zonneveld, Karin A F
Kasten, Sabine
Willems, Helmut
562; 569; Cyprus; GeoB; Geosciences, University of Bremen; GeoTü; Lybia; M51/3; M51/3_562-5; M51/3_569-3; Meteor (1986); MUC; MultiCorer; Paleoceanography at Tübingen University; SESAME; Southern European Seas: Assessing and Modelling Ecosystem Changes
Comparison of calcareous dinoflagellate cyst assemblages with Ba, Al, Mn, and Fe records from three sediment cores collected in the eastern Mediterranean Sea indicate that calcareous dinoflagellate cysts are generally resistant to postdepositional dissolution. Cyst association changes during and after sapropel S1 formation can therefore be closely related to variability in surface water productivity. Two groups of cysts are defined: those having highest abundances within the sapropelic and postsapropelic sediments. The temporal cyst distributions suggest increased freshwater input mainly from the Nile and a shallowing of the pycnocline as the most important processes increasing nutrient concentration in the photic zone, thus leading to increased productivity and organic carbon fluxes during sapropel formation. Furthermore, a general warming trend at the beginning of S1 formation and a slight salinity decrease are reconstructed.
title Calcareous dinoflagellate cysts and geochemistry of Mediterranean Sea sediments
topic 562; 569; Cyprus; GeoB; Geosciences, University of Bremen; GeoTü; Lybia; M51/3; M51/3_562-5; M51/3_569-3; Meteor (1986); MUC; MultiCorer; Paleoceanography at Tübingen University; SESAME; Southern European Seas: Assessing and Modelling Ecosystem Changes
url https://doi.org/10.1594/PANGAEA.736594