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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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 |