Macerals in sediments ...

The study of particulate organic matter (OM) in Arctic Ocean sediments from the Late Cretaceous to the Eocene (IODP Expedition 302) has revealed detailed information about the aquatic/marine OM fluxes, biological sources, preservation and export of terrestrial material. Here, we present detailed dat...

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Main Authors: Boucsein, Bettina, Stein, Ruediger
Format: Article in Journal/Newspaper
Language:English
Published: PANGAEA 2008
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.690523
https://doi.pangaea.de/10.1594/PANGAEA.690523
id ftdatacite:10.1594/pangaea.690523
record_format openpolar
spelling ftdatacite:10.1594/pangaea.690523 2023-05-15T14:57:23+02:00 Macerals in sediments ... Boucsein, Bettina Stein, Ruediger 2008 application/zip https://dx.doi.org/10.1594/pangaea.690523 https://doi.pangaea.de/10.1594/PANGAEA.690523 en eng PANGAEA https://dx.doi.org/10.1016/j.marpetgeo.2008.04.001 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Giant box corer Exp302 ARK-VIII/3 CCGS Captain Molly Kool Vidar Viking Polarstern Integrated Ocean Drilling Program / International Ocean Discovery Program IODP Paleoenvironmental Reconstructions from Marine Sediments @ AWI AWI_Paleo article Collection Supplementary Publication Series of Datasets 2008 ftdatacite https://doi.org/10.1594/pangaea.69052310.1016/j.marpetgeo.2008.04.001 2023-04-03T12:51:48Z The study of particulate organic matter (OM) in Arctic Ocean sediments from the Late Cretaceous to the Eocene (IODP Expedition 302) has revealed detailed information about the aquatic/marine OM fluxes, biological sources, preservation and export of terrestrial material. Here, we present detailed data from maceral analysis, vitrinite reflectance measurements and organic geochemistry.During the Campanian/Paleocene, fluxes of land-derived OM are indicated by reworked and oxidized macerals (vitrinite, inertinite) and terrigenous liptinite (cutinite, sporinite). In the Early Eocene, drastic environmental changes are indicated by peaks in aquatic OM (up to 40-45%, lamalginite, telalginite, liptodetrinite, dinoflagellate cysts) and amorphous OM (up to 50% bituminite). These events of increased aquatic OM flux, similar to conditions favoring black shale deposition, correlate with the global d13C events "Paleocene/Eocene Thermal Maximum" (PETM) and "Elmo-event". Freshwater discharge and proximity of the source area ... : Supplement to: Boucsein, Bettina; Stein, Ruediger (2008): Black shale formation in the late Paleocene/early Eocene Arctic Ocean and paleoenvironmental conditions: New results from a detailed organic petrological study. Marine and Petroleum Geology ... Article in Journal/Newspaper Arctic Arctic Ocean DataCite Metadata Store (German National Library of Science and Technology) Arctic Arctic Ocean
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
language English
topic Giant box corer
Exp302
ARK-VIII/3
CCGS Captain Molly Kool Vidar Viking
Polarstern
Integrated Ocean Drilling Program / International Ocean Discovery Program IODP
Paleoenvironmental Reconstructions from Marine Sediments @ AWI AWI_Paleo
spellingShingle Giant box corer
Exp302
ARK-VIII/3
CCGS Captain Molly Kool Vidar Viking
Polarstern
Integrated Ocean Drilling Program / International Ocean Discovery Program IODP
Paleoenvironmental Reconstructions from Marine Sediments @ AWI AWI_Paleo
Boucsein, Bettina
Stein, Ruediger
Macerals in sediments ...
topic_facet Giant box corer
Exp302
ARK-VIII/3
CCGS Captain Molly Kool Vidar Viking
Polarstern
Integrated Ocean Drilling Program / International Ocean Discovery Program IODP
Paleoenvironmental Reconstructions from Marine Sediments @ AWI AWI_Paleo
description The study of particulate organic matter (OM) in Arctic Ocean sediments from the Late Cretaceous to the Eocene (IODP Expedition 302) has revealed detailed information about the aquatic/marine OM fluxes, biological sources, preservation and export of terrestrial material. Here, we present detailed data from maceral analysis, vitrinite reflectance measurements and organic geochemistry.During the Campanian/Paleocene, fluxes of land-derived OM are indicated by reworked and oxidized macerals (vitrinite, inertinite) and terrigenous liptinite (cutinite, sporinite). In the Early Eocene, drastic environmental changes are indicated by peaks in aquatic OM (up to 40-45%, lamalginite, telalginite, liptodetrinite, dinoflagellate cysts) and amorphous OM (up to 50% bituminite). These events of increased aquatic OM flux, similar to conditions favoring black shale deposition, correlate with the global d13C events "Paleocene/Eocene Thermal Maximum" (PETM) and "Elmo-event". Freshwater discharge and proximity of the source area ... : Supplement to: Boucsein, Bettina; Stein, Ruediger (2008): Black shale formation in the late Paleocene/early Eocene Arctic Ocean and paleoenvironmental conditions: New results from a detailed organic petrological study. Marine and Petroleum Geology ...
format Article in Journal/Newspaper
author Boucsein, Bettina
Stein, Ruediger
author_facet Boucsein, Bettina
Stein, Ruediger
author_sort Boucsein, Bettina
title Macerals in sediments ...
title_short Macerals in sediments ...
title_full Macerals in sediments ...
title_fullStr Macerals in sediments ...
title_full_unstemmed Macerals in sediments ...
title_sort macerals in sediments ...
publisher PANGAEA
publishDate 2008
url https://dx.doi.org/10.1594/pangaea.690523
https://doi.pangaea.de/10.1594/PANGAEA.690523
geographic Arctic
Arctic Ocean
geographic_facet Arctic
Arctic Ocean
genre Arctic
Arctic Ocean
genre_facet Arctic
Arctic Ocean
op_relation https://dx.doi.org/10.1016/j.marpetgeo.2008.04.001
op_rights Creative Commons Attribution 3.0 Unported
https://creativecommons.org/licenses/by/3.0/legalcode
cc-by-3.0
op_doi https://doi.org/10.1594/pangaea.69052310.1016/j.marpetgeo.2008.04.001
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