Age model of ODP Site 113-697 (Table 2) ...

We examined diatom preservation patterns in Pliocene age sediments of Jane Basin (ODP Site 697) and compared them with diatom distribution in more northerly sites at various sectors of the Southern Ocean. Our data from Site 697, as well as other sites from around the Southern Ocean, support the view...

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Bibliographic Details
Main Authors: Burckle, Lloyd H, Gersonde, Rainer, Abrams, Nelson
Format: Dataset
Language:English
Published: PANGAEA 1990
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.53178
https://doi.pangaea.de/10.1594/PANGAEA.53178
id ftdatacite:10.1594/pangaea.53178
record_format openpolar
spelling ftdatacite:10.1594/pangaea.53178 2024-09-15T17:47:23+00:00 Age model of ODP Site 113-697 (Table 2) ... Burckle, Lloyd H Gersonde, Rainer Abrams, Nelson 1990 text/tab-separated-values https://dx.doi.org/10.1594/pangaea.53178 https://doi.pangaea.de/10.1594/PANGAEA.53178 en eng PANGAEA https://dx.doi.org/10.2973/odp.proc.sr.113.203.1990 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 DEPTH, sediment/rock Age model Ageprofile Datum Description Composite Core Age model, paleomagnetic Leg113 Joides Resolution Ocean Drilling Program ODP dataset Supplementary Dataset Dataset 1990 ftdatacite https://doi.org/10.1594/pangaea.5317810.2973/odp.proc.sr.113.203.1990 2024-08-01T11:03:26Z We examined diatom preservation patterns in Pliocene age sediments of Jane Basin (ODP Site 697) and compared them with diatom distribution in more northerly sites at various sectors of the Southern Ocean. Our data from Site 697, as well as other sites from around the Southern Ocean, support the view that there was significant ice growth on Antarctica during the late Pliocene. DSDP Site 514 in the Atlantic sector shows increased relative abundance of Eucampia antarctica, an ice-related form, in the upper part of the Gauss Chron with a larger increase just above it. With one exception, all sites included in the present study show increased relative abundance of E. antarctica in the upper part of the Gauss. Our view that there was ice growth on Antarctica during the late Gauss Chron is supported by the results from ODP Site 697. While diatoms are present and percent opal is high in the early and middle Gauss Chron (suggesting more open-ocean conditions), late Gauss sediments contain low percentages of opal and ... : Supplement to: Burckle, Lloyd H; Gersonde, Rainer; Abrams, Nelson (1990): Late Pliocene-Pleistocene paleoclimate in the Jane Basin region: ODP Site 697. In: Barker, PF; Kennett, JP; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 113, 803-812 ... Dataset Antarc* Antarctica E. Antarctica Southern Ocean DataCite
institution Open Polar
collection DataCite
op_collection_id ftdatacite
language English
topic DEPTH, sediment/rock
Age model
Ageprofile Datum Description
Composite Core
Age model, paleomagnetic
Leg113
Joides Resolution
Ocean Drilling Program ODP
spellingShingle DEPTH, sediment/rock
Age model
Ageprofile Datum Description
Composite Core
Age model, paleomagnetic
Leg113
Joides Resolution
Ocean Drilling Program ODP
Burckle, Lloyd H
Gersonde, Rainer
Abrams, Nelson
Age model of ODP Site 113-697 (Table 2) ...
topic_facet DEPTH, sediment/rock
Age model
Ageprofile Datum Description
Composite Core
Age model, paleomagnetic
Leg113
Joides Resolution
Ocean Drilling Program ODP
description We examined diatom preservation patterns in Pliocene age sediments of Jane Basin (ODP Site 697) and compared them with diatom distribution in more northerly sites at various sectors of the Southern Ocean. Our data from Site 697, as well as other sites from around the Southern Ocean, support the view that there was significant ice growth on Antarctica during the late Pliocene. DSDP Site 514 in the Atlantic sector shows increased relative abundance of Eucampia antarctica, an ice-related form, in the upper part of the Gauss Chron with a larger increase just above it. With one exception, all sites included in the present study show increased relative abundance of E. antarctica in the upper part of the Gauss. Our view that there was ice growth on Antarctica during the late Gauss Chron is supported by the results from ODP Site 697. While diatoms are present and percent opal is high in the early and middle Gauss Chron (suggesting more open-ocean conditions), late Gauss sediments contain low percentages of opal and ... : Supplement to: Burckle, Lloyd H; Gersonde, Rainer; Abrams, Nelson (1990): Late Pliocene-Pleistocene paleoclimate in the Jane Basin region: ODP Site 697. In: Barker, PF; Kennett, JP; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 113, 803-812 ...
format Dataset
author Burckle, Lloyd H
Gersonde, Rainer
Abrams, Nelson
author_facet Burckle, Lloyd H
Gersonde, Rainer
Abrams, Nelson
author_sort Burckle, Lloyd H
title Age model of ODP Site 113-697 (Table 2) ...
title_short Age model of ODP Site 113-697 (Table 2) ...
title_full Age model of ODP Site 113-697 (Table 2) ...
title_fullStr Age model of ODP Site 113-697 (Table 2) ...
title_full_unstemmed Age model of ODP Site 113-697 (Table 2) ...
title_sort age model of odp site 113-697 (table 2) ...
publisher PANGAEA
publishDate 1990
url https://dx.doi.org/10.1594/pangaea.53178
https://doi.pangaea.de/10.1594/PANGAEA.53178
genre Antarc*
Antarctica
E. Antarctica
Southern Ocean
genre_facet Antarc*
Antarctica
E. Antarctica
Southern Ocean
op_relation https://dx.doi.org/10.2973/odp.proc.sr.113.203.1990
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.5317810.2973/odp.proc.sr.113.203.1990
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