Palynological and geochemical results of middle Eocene sediments of ODP Hole 159-959D, equatorial Atlantic Ocean

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Hauptverfasser: Cramwinckel, Margot J, Van der Ploeg, Robin, Bijl, Peter K, Peterse, Francien, Bohaty, Steven M, Röhl, Ursula, Schouten, Stefan, Middelburg, Jack J, Sluijs, Appy
Format: Dataset Open Access
Sprache:en
Veröffentlicht: PANGAEA 2019
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author Cramwinckel, Margot J
Van der Ploeg, Robin
Bijl, Peter K
Peterse, Francien
Bohaty, Steven M
Röhl, Ursula
Schouten, Stefan
Middelburg, Jack J
Sluijs, Appy
author_facet Cramwinckel, Margot J
Van der Ploeg, Robin
Bijl, Peter K
Peterse, Francien
Bohaty, Steven M
Röhl, Ursula
Schouten, Stefan
Middelburg, Jack J
Sluijs, Appy
collection Datos científicos de ciencias marinas y ambientales
contents New palynological, sedimentological, and geochemical records spanning the Middle Eocene climatic optimum (MECO; ca. 40 Ma) in the equatorial Atlantic Ocean indicate that peak warming was associated with upper-ocean stratification, decreased export production, and possibly harmful algal blooms, followed by slight oxygen minimum zone expansion. Combining these findings with published MECO records suggests that export production collapse and benthos starvation during the zenith of MECO warmth were widespread in the Atlantic. Furthermore, comparison to records across the Paleocene-Eocene thermal maximum (ca. 56 Ma) at the same site suggests a similar system response to warming, but with different impact on benthic communities.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_898089
institution PANGAEA
language en
publishDate 2019
publisher PANGAEA
record_format pangaea
spellingShingle Palynological and geochemical results of middle Eocene sediments of ODP Hole 159-959D, equatorial Atlantic Ocean
Cramwinckel, Margot J
Van der Ploeg, Robin
Bijl, Peter K
Peterse, Francien
Bohaty, Steven M
Röhl, Ursula
Schouten, Stefan
Middelburg, Jack J
Sluijs, Appy
159-959D; Eocene; MECO; Middle Eocene Climatic Optimum; Ocean Drilling Program; ODP; ODP Site 959
New palynological, sedimentological, and geochemical records spanning the Middle Eocene climatic optimum (MECO; ca. 40 Ma) in the equatorial Atlantic Ocean indicate that peak warming was associated with upper-ocean stratification, decreased export production, and possibly harmful algal blooms, followed by slight oxygen minimum zone expansion. Combining these findings with published MECO records suggests that export production collapse and benthos starvation during the zenith of MECO warmth were widespread in the Atlantic. Furthermore, comparison to records across the Paleocene-Eocene thermal maximum (ca. 56 Ma) at the same site suggests a similar system response to warming, but with different impact on benthic communities.
title Palynological and geochemical results of middle Eocene sediments of ODP Hole 159-959D, equatorial Atlantic Ocean
topic 159-959D; Eocene; MECO; Middle Eocene Climatic Optimum; Ocean Drilling Program; ODP; ODP Site 959
url https://doi.org/10.1594/PANGAEA.898089