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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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 |
_version_ |
1766329465452888064 |