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Main Authors: Heck, Philipp R, Anselmetti, Flavio S, Isern, Alexandra R
Format: Dataset Open Access
Language:en
Published: PANGAEA 2004
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Online Access:https://doi.org/10.1594/PANGAEA.778715
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author Heck, Philipp R
Anselmetti, Flavio S
Isern, Alexandra R
author_facet Heck, Philipp R
Anselmetti, Flavio S
Isern, Alexandra R
collection Datos científicos de ciencias marinas y ambientales
contents Biostratigraphic, sedimentologic, and geochemical analyses of hemipelagic periplatform sediments from shallow gravity cores taken during the Ocean Drilling Program Leg 194 site survey reveal that, despite the strong currents and almost infilled intraplatform bathymetric depressions, recent sedimentation at the location of the Leg 194 drill sites recorded glacial-interglacial cycles. Sediment analyses included determination of sediment type, carbonate content, bulk stable oxygen isotope composition, and calcareous nannofossil zones. Glacial periods, identified by elevated bulk d18O, are characterized by darker sediment color, coarser grain size, and lower carbonate content, whereas interglacial periods yield lighter-colored, finer, and carbonate-rich sediments. These data from the shallowmost few meters of Marion Plateau sediments complement the subsurface information of Leg 194 holes, in which the top few meters have not been analyzed in such a high-resolution fashion. In addition, these gravity cores are more likely to have recovered the sediments closest to the sediment/water interface as compared to the hydraulic piston cores collected during Leg 194.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_778715
institution PANGAEA
language en
publishDate 2004
publisher PANGAEA
record_format pangaea
spellingShingle Major nannofossils, carbon and oxygen isotopes and carbon composition of ODP leg 194 site survey gravity cores
Heck, Philipp R
Anselmetti, Flavio S
Isern, Alexandra R
CS-03; CS-05/1198; CS-08/1197; CS-09; GC; GC-03; GC-06; GC-08; GC-09; GC-10; Gravity corer; Marion Plateau
Biostratigraphic, sedimentologic, and geochemical analyses of hemipelagic periplatform sediments from shallow gravity cores taken during the Ocean Drilling Program Leg 194 site survey reveal that, despite the strong currents and almost infilled intraplatform bathymetric depressions, recent sedimentation at the location of the Leg 194 drill sites recorded glacial-interglacial cycles. Sediment analyses included determination of sediment type, carbonate content, bulk stable oxygen isotope composition, and calcareous nannofossil zones. Glacial periods, identified by elevated bulk d18O, are characterized by darker sediment color, coarser grain size, and lower carbonate content, whereas interglacial periods yield lighter-colored, finer, and carbonate-rich sediments. These data from the shallowmost few meters of Marion Plateau sediments complement the subsurface information of Leg 194 holes, in which the top few meters have not been analyzed in such a high-resolution fashion. In addition, these gravity cores are more likely to have recovered the sediments closest to the sediment/water interface as compared to the hydraulic piston cores collected during Leg 194.
title Major nannofossils, carbon and oxygen isotopes and carbon composition of ODP leg 194 site survey gravity cores
topic CS-03; CS-05/1198; CS-08/1197; CS-09; GC; GC-03; GC-06; GC-08; GC-09; GC-10; Gravity corer; Marion Plateau
url https://doi.org/10.1594/PANGAEA.778715