Comment on "Deep-Sea Temperature and Ice Volume Changes Across the Pliocene-Pleistocene Climate Transitions"

Sosdian and Rosenthal (Reports, 17 July 2009, p. 306) used magnesium/calcium ratios in benthic foraminifera from the North Atlantic to reconstruct past bottom-water temperatures. They suggested that both ice volume change and ice-sheet dynamics played important roles during the late Pliocene and mid...

Full description

Bibliographic Details
Main Authors: Yu, Jimin, Broeker, Wally S.
Format: Article in Journal/Newspaper
Language:unknown
Published: American Association for the Advancement of Science 2015
Subjects:
Online Access:http://hdl.handle.net/1885/53859
id ftanucanberra:oai:digitalcollections.anu.edu.au:1885/53859
record_format openpolar
spelling ftanucanberra:oai:digitalcollections.anu.edu.au:1885/53859 2023-05-15T16:40:29+02:00 Comment on "Deep-Sea Temperature and Ice Volume Changes Across the Pliocene-Pleistocene Climate Transitions" Yu, Jimin Broeker, Wally S. 2015-12-10T22:26:40Z http://hdl.handle.net/1885/53859 unknown American Association for the Advancement of Science 0036-8075 http://hdl.handle.net/1885/53859 Science Journal article 2015 ftanucanberra 2015-12-21T23:33:42Z Sosdian and Rosenthal (Reports, 17 July 2009, p. 306) used magnesium/calcium ratios in benthic foraminifera from the North Atlantic to reconstruct past bottom-water temperatures. They suggested that both ice volume change and ice-sheet dynamics played important roles during the late Pliocene and mid-Pleistocene climate transitions. We present evidence that their record of deep ocean temperature is not reliable, thus raising doubts about their conclusions. Article in Journal/Newspaper Ice Sheet North Atlantic Australian National University: ANU Digital Collections Rosenthal ENVELOPE(-64.283,-64.283,-64.600,-64.600)
institution Open Polar
collection Australian National University: ANU Digital Collections
op_collection_id ftanucanberra
language unknown
description Sosdian and Rosenthal (Reports, 17 July 2009, p. 306) used magnesium/calcium ratios in benthic foraminifera from the North Atlantic to reconstruct past bottom-water temperatures. They suggested that both ice volume change and ice-sheet dynamics played important roles during the late Pliocene and mid-Pleistocene climate transitions. We present evidence that their record of deep ocean temperature is not reliable, thus raising doubts about their conclusions.
format Article in Journal/Newspaper
author Yu, Jimin
Broeker, Wally S.
spellingShingle Yu, Jimin
Broeker, Wally S.
Comment on "Deep-Sea Temperature and Ice Volume Changes Across the Pliocene-Pleistocene Climate Transitions"
author_facet Yu, Jimin
Broeker, Wally S.
author_sort Yu, Jimin
title Comment on "Deep-Sea Temperature and Ice Volume Changes Across the Pliocene-Pleistocene Climate Transitions"
title_short Comment on "Deep-Sea Temperature and Ice Volume Changes Across the Pliocene-Pleistocene Climate Transitions"
title_full Comment on "Deep-Sea Temperature and Ice Volume Changes Across the Pliocene-Pleistocene Climate Transitions"
title_fullStr Comment on "Deep-Sea Temperature and Ice Volume Changes Across the Pliocene-Pleistocene Climate Transitions"
title_full_unstemmed Comment on "Deep-Sea Temperature and Ice Volume Changes Across the Pliocene-Pleistocene Climate Transitions"
title_sort comment on "deep-sea temperature and ice volume changes across the pliocene-pleistocene climate transitions"
publisher American Association for the Advancement of Science
publishDate 2015
url http://hdl.handle.net/1885/53859
long_lat ENVELOPE(-64.283,-64.283,-64.600,-64.600)
geographic Rosenthal
geographic_facet Rosenthal
genre Ice Sheet
North Atlantic
genre_facet Ice Sheet
North Atlantic
op_source Science
op_relation 0036-8075
http://hdl.handle.net/1885/53859
_version_ 1766030875463516160