Median grain size and distribution of sand in ODP Hole 108-660A (Fig. 5)

50 m of Middle Eocene pure radiolarian ooze were drilled at ODP Site 660 in the equatorial East Atlantic, 80 km northeast of the Kane Gap. The oozes comprise a 10 m high and 2 km broad mound of seismic reverberations, covered by manganese-rich sediment, and contain trace amounts of sponge spicules a...

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Main Authors: Sarnthein, Michael, Faugeres, Jean-Claude
Format: Dataset
Language:English
Published: PANGAEA 1993
Subjects:
ODP
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.763684
https://doi.org/10.1594/PANGAEA.763684
id ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.763684
record_format openpolar
spelling ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.763684 2024-09-15T17:47:29+00:00 Median grain size and distribution of sand in ODP Hole 108-660A (Fig. 5) Sarnthein, Michael Faugeres, Jean-Claude LATITUDE: 10.013500 * LONGITUDE: -19.245600 * DATE/TIME START: 1986-03-15T00:30:00 * DATE/TIME END: 1986-03-16T10:30:00 * MINIMUM ELEVATION: -4343.0 m * MAXIMUM ELEVATION: -4343.0 m 1993 text/tab-separated-values, 90 data points https://doi.pangaea.de/10.1594/PANGAEA.763684 https://doi.org/10.1594/PANGAEA.763684 en eng PANGAEA https://doi.pangaea.de/10.1594/PANGAEA.763684 https://doi.org/10.1594/PANGAEA.763684 CC-BY-3.0: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted info:eu-repo/semantics/openAccess Supplement to: Sarnthein, Michael; Faugeres, Jean-Claude (1993): Radiolarian contourites record Eocene AABW circulation in the equatorial East Atlantic. Sedimentary Geology, 82(1-4), 145-155, https://doi.org/10.1016/0037-0738(93)90118-O 108-660A DRILL Drilling/drill rig DSDP/ODP/IODP sample designation Joides Resolution Leg108 Median grain size North Atlantic Ocean Ocean Drilling Program ODP Sample code/label Size fraction > 0.063 mm sand dataset 1993 ftpangaea https://doi.org/10.1594/PANGAEA.76368410.1016/0037-0738(93)90118-O 2024-08-21T00:02:27Z 50 m of Middle Eocene pure radiolarian ooze were drilled at ODP Site 660 in the equatorial East Atlantic, 80 km northeast of the Kane Gap. The oozes comprise a 10 m high and 2 km broad mound of seismic reverberations, covered by manganese-rich sediment, and contain trace amounts of sponge spicules and diatoms, negligible organic carbon (0.15%), clay, and variable amounts of pyrite. The yellow to pale brown silty sediments are relatively coarse-grained (30–45% coarser than 6 µm), little bioturbated, and commonly massive or laminated on a cm-scale. The unlithified radiolarian ooze may indicate an interval of high oceanic productivity, probably linked to a palaeoposition of Site 660 close to the equatorial upwelling belt during Middle Eocene time. The absence of organic matter, however, and both the laminated bedding and the mound-like structure of the deposit on the lower slope of a continental rise indicate deposition by relatively intense contour currents of oxygen-rich deep water, which passed through the Kane Gap, winnowed the fine clay fraction, and prevented the preservation of organic carbon. The ooze may be either a contourite-lag deposit, or a contourite accumulation of displaced radiolarians, originating south of the Kane Gap and being deposited in its northern lee, thus documenting the passage of a strong cross-equatorial bottom-water current formed near Antarctica. These Eocene contourites may be an analogue for ancient radiolarites in the Tethyan Ocean. Dataset Antarc* Antarctica North Atlantic PANGAEA - Data Publisher for Earth & Environmental Science ENVELOPE(-19.245600,-19.245600,10.013500,10.013500)
institution Open Polar
collection PANGAEA - Data Publisher for Earth & Environmental Science
op_collection_id ftpangaea
language English
topic 108-660A
DRILL
Drilling/drill rig
DSDP/ODP/IODP sample designation
Joides Resolution
Leg108
Median
grain size
North Atlantic Ocean
Ocean Drilling Program
ODP
Sample code/label
Size fraction > 0.063 mm
sand
spellingShingle 108-660A
DRILL
Drilling/drill rig
DSDP/ODP/IODP sample designation
Joides Resolution
Leg108
Median
grain size
North Atlantic Ocean
Ocean Drilling Program
ODP
Sample code/label
Size fraction > 0.063 mm
sand
Sarnthein, Michael
Faugeres, Jean-Claude
Median grain size and distribution of sand in ODP Hole 108-660A (Fig. 5)
topic_facet 108-660A
DRILL
Drilling/drill rig
DSDP/ODP/IODP sample designation
Joides Resolution
Leg108
Median
grain size
North Atlantic Ocean
Ocean Drilling Program
ODP
Sample code/label
Size fraction > 0.063 mm
sand
description 50 m of Middle Eocene pure radiolarian ooze were drilled at ODP Site 660 in the equatorial East Atlantic, 80 km northeast of the Kane Gap. The oozes comprise a 10 m high and 2 km broad mound of seismic reverberations, covered by manganese-rich sediment, and contain trace amounts of sponge spicules and diatoms, negligible organic carbon (0.15%), clay, and variable amounts of pyrite. The yellow to pale brown silty sediments are relatively coarse-grained (30–45% coarser than 6 µm), little bioturbated, and commonly massive or laminated on a cm-scale. The unlithified radiolarian ooze may indicate an interval of high oceanic productivity, probably linked to a palaeoposition of Site 660 close to the equatorial upwelling belt during Middle Eocene time. The absence of organic matter, however, and both the laminated bedding and the mound-like structure of the deposit on the lower slope of a continental rise indicate deposition by relatively intense contour currents of oxygen-rich deep water, which passed through the Kane Gap, winnowed the fine clay fraction, and prevented the preservation of organic carbon. The ooze may be either a contourite-lag deposit, or a contourite accumulation of displaced radiolarians, originating south of the Kane Gap and being deposited in its northern lee, thus documenting the passage of a strong cross-equatorial bottom-water current formed near Antarctica. These Eocene contourites may be an analogue for ancient radiolarites in the Tethyan Ocean.
format Dataset
author Sarnthein, Michael
Faugeres, Jean-Claude
author_facet Sarnthein, Michael
Faugeres, Jean-Claude
author_sort Sarnthein, Michael
title Median grain size and distribution of sand in ODP Hole 108-660A (Fig. 5)
title_short Median grain size and distribution of sand in ODP Hole 108-660A (Fig. 5)
title_full Median grain size and distribution of sand in ODP Hole 108-660A (Fig. 5)
title_fullStr Median grain size and distribution of sand in ODP Hole 108-660A (Fig. 5)
title_full_unstemmed Median grain size and distribution of sand in ODP Hole 108-660A (Fig. 5)
title_sort median grain size and distribution of sand in odp hole 108-660a (fig. 5)
publisher PANGAEA
publishDate 1993
url https://doi.pangaea.de/10.1594/PANGAEA.763684
https://doi.org/10.1594/PANGAEA.763684
op_coverage LATITUDE: 10.013500 * LONGITUDE: -19.245600 * DATE/TIME START: 1986-03-15T00:30:00 * DATE/TIME END: 1986-03-16T10:30:00 * MINIMUM ELEVATION: -4343.0 m * MAXIMUM ELEVATION: -4343.0 m
long_lat ENVELOPE(-19.245600,-19.245600,10.013500,10.013500)
genre Antarc*
Antarctica
North Atlantic
genre_facet Antarc*
Antarctica
North Atlantic
op_source Supplement to: Sarnthein, Michael; Faugeres, Jean-Claude (1993): Radiolarian contourites record Eocene AABW circulation in the equatorial East Atlantic. Sedimentary Geology, 82(1-4), 145-155, https://doi.org/10.1016/0037-0738(93)90118-O
op_relation https://doi.pangaea.de/10.1594/PANGAEA.763684
https://doi.org/10.1594/PANGAEA.763684
op_rights CC-BY-3.0: Creative Commons Attribution 3.0 Unported
Access constraints: unrestricted
info:eu-repo/semantics/openAccess
op_doi https://doi.org/10.1594/PANGAEA.76368410.1016/0037-0738(93)90118-O
_version_ 1810496874310795264