(Table 3) Foraminiferal 87Sr/86Sr ratios and ages of ODP Hole 162-986D sediments
Site 986 was drilled to 965 meters below seafloor (mbsf) on the western Svalbard margin to record the onset of glaciations and to date and document the glacial evolution in the Svalbard-Barents Sea region during the Pliocene-Pleistocene. In this paper, results of sedimentological analyses are discus...
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ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.805206 2024-09-15T17:57:54+00:00 (Table 3) Foraminiferal 87Sr/86Sr ratios and ages of ODP Hole 162-986D sediments Forsberg, Carl Fredrik Solheim, Anders Elverhoi, Anders Jansen, Eystein Channell, James E T Andersen, Espen Sletten LATITUDE: 77.340000 * LONGITUDE: -9.077500 * DATE/TIME START: 1995-08-14T15:05:00 * DATE/TIME END: 1995-08-20T20:45:00 * MINIMUM DEPTH, sediment/rock: 668.42 m * MAXIMUM DEPTH, sediment/rock: 892.42 m 1999 text/tab-separated-values, 60 data points https://doi.pangaea.de/10.1594/PANGAEA.805206 https://doi.org/10.1594/PANGAEA.805206 en eng PANGAEA https://doi.pangaea.de/10.1594/PANGAEA.805206 https://doi.org/10.1594/PANGAEA.805206 CC-BY-3.0: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted info:eu-repo/semantics/openAccess Supplement to: Forsberg, Carl Fredrik; Solheim, Anders; Elverhoi, Anders; Jansen, Eystein; Channell, James E T; Andersen, Espen Sletten (1999): The depositional environment of the western Svalbard margin during the late Pliocene and the Pleistocene: sedimentary facies changes at Site 986. In: Raymo, ME; Jansen, E; Blum, P; Herbert, TD (eds.) Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 162, 1-14, https://doi.org/10.2973/odp.proc.sr.162.032.1999 162-986D Age dated dated material maximum/old minimum/young strontium isotope LOWESS fit Howarth & McArthur (1997) DEPTH sediment/rock DRILL Drilling/drill rig DSDP/ODP/IODP sample designation Joides Resolution Leg162 North Greenland Sea Ocean Drilling Program ODP Sample code/label Strontium-87/Strontium-86 ratio dataset 1999 ftpangaea https://doi.org/10.1594/PANGAEA.80520610.2973/odp.proc.sr.162.032.1999 2024-07-24T02:31:32Z Site 986 was drilled to 965 meters below seafloor (mbsf) on the western Svalbard margin to record the onset of glaciations and to date and document the glacial evolution in the Svalbard-Barents Sea region during the Pliocene-Pleistocene. In this paper, results of sedimentological analyses are discussed in light of seismic stratigraphy and new age determinations. The latter were difficult to obtain in the glacial deposits, and datums are sparse. Through combined paleomagnetic data, biostratigraphy, and Sr isotopes, however, an overall chronology for the main evolutionary steps is suggested. The cored sequence at Site 986 is younger than 2.6 Ma, and the lower 60 m of the section contains no evidence of a major glacial influence. An initial glaciation is interpreted to have occurred at ~2.3 Ma, resulting in increased sand deposition from debris flows at Site 986 and forming a prominent seismic reflector, R7. However, glaciers probably did not reach the shelf break until ~1.6-1.7 Ma (Reflector R6), after which the depositional environment was dominated by diamictic debris flows. A gradual change in source area from the Barents Sea to Svalbard is recorded primarily by changes in carbonate and smectite content, ~355 mbsf (Reflector R5), at an interpolated age of 1.4-1.5 Ma. During the last ~1 m.y., Site 986 has undergone more distal deposition as the main depocenters have shifted laterally. This has resulted in less frequent debris flows and more turbidites and hemipelagic deposits, with a slight fining upward of the cored sediments. Dataset Barents Sea Greenland Greenland Sea North Greenland Svalbard Svalbard margin PANGAEA - Data Publisher for Earth & Environmental Science ENVELOPE(-9.077500,-9.077500,77.340000,77.340000) |
institution |
Open Polar |
collection |
PANGAEA - Data Publisher for Earth & Environmental Science |
op_collection_id |
ftpangaea |
language |
English |
topic |
162-986D Age dated dated material maximum/old minimum/young strontium isotope LOWESS fit Howarth & McArthur (1997) DEPTH sediment/rock DRILL Drilling/drill rig DSDP/ODP/IODP sample designation Joides Resolution Leg162 North Greenland Sea Ocean Drilling Program ODP Sample code/label Strontium-87/Strontium-86 ratio |
spellingShingle |
162-986D Age dated dated material maximum/old minimum/young strontium isotope LOWESS fit Howarth & McArthur (1997) DEPTH sediment/rock DRILL Drilling/drill rig DSDP/ODP/IODP sample designation Joides Resolution Leg162 North Greenland Sea Ocean Drilling Program ODP Sample code/label Strontium-87/Strontium-86 ratio Forsberg, Carl Fredrik Solheim, Anders Elverhoi, Anders Jansen, Eystein Channell, James E T Andersen, Espen Sletten (Table 3) Foraminiferal 87Sr/86Sr ratios and ages of ODP Hole 162-986D sediments |
topic_facet |
162-986D Age dated dated material maximum/old minimum/young strontium isotope LOWESS fit Howarth & McArthur (1997) DEPTH sediment/rock DRILL Drilling/drill rig DSDP/ODP/IODP sample designation Joides Resolution Leg162 North Greenland Sea Ocean Drilling Program ODP Sample code/label Strontium-87/Strontium-86 ratio |
description |
Site 986 was drilled to 965 meters below seafloor (mbsf) on the western Svalbard margin to record the onset of glaciations and to date and document the glacial evolution in the Svalbard-Barents Sea region during the Pliocene-Pleistocene. In this paper, results of sedimentological analyses are discussed in light of seismic stratigraphy and new age determinations. The latter were difficult to obtain in the glacial deposits, and datums are sparse. Through combined paleomagnetic data, biostratigraphy, and Sr isotopes, however, an overall chronology for the main evolutionary steps is suggested. The cored sequence at Site 986 is younger than 2.6 Ma, and the lower 60 m of the section contains no evidence of a major glacial influence. An initial glaciation is interpreted to have occurred at ~2.3 Ma, resulting in increased sand deposition from debris flows at Site 986 and forming a prominent seismic reflector, R7. However, glaciers probably did not reach the shelf break until ~1.6-1.7 Ma (Reflector R6), after which the depositional environment was dominated by diamictic debris flows. A gradual change in source area from the Barents Sea to Svalbard is recorded primarily by changes in carbonate and smectite content, ~355 mbsf (Reflector R5), at an interpolated age of 1.4-1.5 Ma. During the last ~1 m.y., Site 986 has undergone more distal deposition as the main depocenters have shifted laterally. This has resulted in less frequent debris flows and more turbidites and hemipelagic deposits, with a slight fining upward of the cored sediments. |
format |
Dataset |
author |
Forsberg, Carl Fredrik Solheim, Anders Elverhoi, Anders Jansen, Eystein Channell, James E T Andersen, Espen Sletten |
author_facet |
Forsberg, Carl Fredrik Solheim, Anders Elverhoi, Anders Jansen, Eystein Channell, James E T Andersen, Espen Sletten |
author_sort |
Forsberg, Carl Fredrik |
title |
(Table 3) Foraminiferal 87Sr/86Sr ratios and ages of ODP Hole 162-986D sediments |
title_short |
(Table 3) Foraminiferal 87Sr/86Sr ratios and ages of ODP Hole 162-986D sediments |
title_full |
(Table 3) Foraminiferal 87Sr/86Sr ratios and ages of ODP Hole 162-986D sediments |
title_fullStr |
(Table 3) Foraminiferal 87Sr/86Sr ratios and ages of ODP Hole 162-986D sediments |
title_full_unstemmed |
(Table 3) Foraminiferal 87Sr/86Sr ratios and ages of ODP Hole 162-986D sediments |
title_sort |
(table 3) foraminiferal 87sr/86sr ratios and ages of odp hole 162-986d sediments |
publisher |
PANGAEA |
publishDate |
1999 |
url |
https://doi.pangaea.de/10.1594/PANGAEA.805206 https://doi.org/10.1594/PANGAEA.805206 |
op_coverage |
LATITUDE: 77.340000 * LONGITUDE: -9.077500 * DATE/TIME START: 1995-08-14T15:05:00 * DATE/TIME END: 1995-08-20T20:45:00 * MINIMUM DEPTH, sediment/rock: 668.42 m * MAXIMUM DEPTH, sediment/rock: 892.42 m |
long_lat |
ENVELOPE(-9.077500,-9.077500,77.340000,77.340000) |
genre |
Barents Sea Greenland Greenland Sea North Greenland Svalbard Svalbard margin |
genre_facet |
Barents Sea Greenland Greenland Sea North Greenland Svalbard Svalbard margin |
op_source |
Supplement to: Forsberg, Carl Fredrik; Solheim, Anders; Elverhoi, Anders; Jansen, Eystein; Channell, James E T; Andersen, Espen Sletten (1999): The depositional environment of the western Svalbard margin during the late Pliocene and the Pleistocene: sedimentary facies changes at Site 986. In: Raymo, ME; Jansen, E; Blum, P; Herbert, TD (eds.) Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 162, 1-14, https://doi.org/10.2973/odp.proc.sr.162.032.1999 |
op_relation |
https://doi.pangaea.de/10.1594/PANGAEA.805206 https://doi.org/10.1594/PANGAEA.805206 |
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.80520610.2973/odp.proc.sr.162.032.1999 |
_version_ |
1810434117328699392 |