About: Similar rates of modern and last-glacial ocean thermohaline circulation inferred from radiochemical data

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scientific article published in Nature

Attributes	Values
rdf:type	Item
description	artículu científicu (ast) wetenschappelijk artikel (nl) article publié dans la revue scientifique Nature (fr) im Februar 1996 veröffentlichter wissenschaftlicher Artikel (de) scientific article published in Nature (en) наукова стаття, опублікована в Nature в лютому 1996 (uk)
publication date	wds:Q59088380-5A38544C-CF4F-4719-97CC-17748FB66E03
publication date	1996-02-01 00:00:00Z (xsd:dateTime)
language of work or name	wds:Q59088380-35AF3732-CBA8-4558-BC45-FF8A12D39DFB
language of work or name	English
exact match	wds:Q59088380-F0328DA9-2F18-404B-B849-34947BB19563
exact match	https://scigraph.springernature.com/pub.10.1038/379689a0
cites work	wds:Q59088380-08DD2491-D55A-490B-8463-4E6C16D5362A wds:Q59088380-24FFA834-C737-47A0-A760-57A2889EE913 wds:Q59088380-4B7D35AD-4307-4718-A5A5-227BA661E780 wds:Q59088380-58E49F82-5ADA-4DB7-B85E-C8F2C7291035 wds:Q59088380-590C4831-F654-41A7-BA9E-FF0B23A9FDA8 wds:Q59088380-5B8CEB52-4349-4EE1-9934-3441428F74A4 wds:Q59088380-60B8EB32-0390-450F-A69A-817EA8D2D9CA wds:Q59088380-7C0A7A85-ECED-4732-862E-338663EB777F wds:Q59088380-7DEB7CAE-CFD3-4D13-86F0-1D77967CAEFE wds:Q59088380-87E33907-07A7-4692-A7A0-308026952641 wds:Q59088380-955AFF6B-E80C-42EA-9D0A-54507F8818D2 wds:Q59088380-966943BD-DCCD-4D8D-974A-3E86AC291F8C wds:Q59088380-9E11FA38-0126-4131-A35A-F7E008F2D70A wds:Q59088380-9F1314CD-15BD-4118-BDC4-D6E8D8CA98BF wds:Q59088380-B7C12FF4-FE35-42B1-8183-BB9528080E5A wds:Q59088380-CF064CDA-20D4-4960-8ADB-A4E126166A08 wds:Q59088380-D5BF2CEF-43BF-4836-9136-A763EC2ADCC0 wds:Q59088380-D5FEE651-1805-4F06-8245-0FA332C57069 wds:Q59088380-E44CBC3C-BAFA-4B25-8E08-2FD9BC667180
cites work	South Atlantic interbasin exchange An Oceanographic Explanation for the Apparent Carbon Isotope-Cadmium Discordancy in the Glacial Antarctic? Deglacial meltwater discharge, North Atlantic Deep Circulation, and abrupt climate change Abyssal water carbon-14 distribution and the age of the world oceans Correlations between climate records from North Atlantic sediments and Greenland ice Deep Circulation of the North Atlantic over the Last 200,000 Years: Geochemical Evidence. Mass-Spectrometric 230Th-234U-238U Dating of the Devils Hole Calcite Vein Variations in terrigenous input into the deep equatorial atlantic during the past 24,000 years. Evidence for lower productivity in the Antarctic Ocean during the last glaciation 238U, 234U and 232Th in seawater Evidence from Southern Ocean sediments for the effect of North Atlantic deep-water flux on climate A conservative tracer for glacial ocean circulation from carbon isotope and palaeo-nutrient measurements in benthic foraminifera Anomalous boundary scavenging in the Middle Atlantic Bight: evidence from 230Th, 231Pa, 10Be and 210Pb Boundary scavenging in the Pacific Ocean: a comparison of10Be and231Pa A revised estimate for the radiocarbon age of North Atlantic deep water Removal of 230Th and 231Pa from the open ocean The cause of the glacial to interglacial atmospheric CO2change: A Polar Alkalinity Hypothesis Increased production of cosmogenic 10Be during the Last Glacial Maximum Quaternary deepwater paleoceanography.
author name string	wds:Q59088380-23FDD49F-758C-4AAC-A3FA-1ABCCBB565AD wds:Q59088380-DCF5C8FC-B1DB-44CC-975F-33818E4B5299 wds:Q59088380-DD628F49-B52C-419C-8D33-A32143FE81F9
author name string	Roger Francois Michael P. Bacon Ein-Fen Yu
rdfs:label	Similar rates of modern and last-glacial ocean thermohaline circulation inferred from radiochemical data (en) Similar rates of modern and last-glacial ocean thermohaline circulation inferred from radiochemical data (nl)
skos:prefLabel	Similar rates of modern and last-glacial ocean thermohaline circulation inferred from radiochemical data (en) Similar rates of modern and last-glacial ocean thermohaline circulation inferred from radiochemical data (nl)
name	Similar rates of modern and last-glacial ocean thermohaline circulation inferred from radiochemical data (en) Similar rates of modern and last-glacial ocean thermohaline circulation inferred from radiochemical data (nl)
title	wds:Q59088380-A96D154E-228B-4093-A41F-AFA4D37B53F4
title	Similar rates of modern and last-glacial ocean thermohaline circulation inferred from radiochemical data (en)
page(s)	wds:Q59088380-4C9C400B-B573-47F4-8423-B8DFBD6298A8
page(s)	689-694
instance of	wds:Q59088380-30E463D3-6205-468F-BB89-DFC6F36F21C0
instance of	scholarly article
main subject	wds:Q59088380-EB556CE7-08FC-4D08-8174-3C98BD385254
main subject	thermohaline circulation
published in	wds:Q59088380-E22C65FC-4BFD-417A-BFE3-EBD0115CA4B0
published in	Nature
issue	wds:Q59088380-07798E80-8C3C-47FA-BC15-472700D44C3A
volume	wds:Q59088380-1F77AC67-EA65-4453-BD97-BA504597771B
issue	6567
volume	379
DOI	wds:Q59088380-0F5BE3E5-52E6-4552-A50A-37270A368295
DOI	http://dx.doi.org/10.1038/379689A0
DOI	10.1038/379689A0
Dimensions Publication ID	wds:Q59088380-57E05CEE-FFCC-4BF8-84F9-E407E18FE7BA
Dimensions Publication ID	1009942151
is about of	https://www.wikidata.org/wiki/Special:EntityData/Q59088380
is cites work of	Characteristics of the deep ocean carbon system during the past 150,000 years: SigmaCO2 distributions, deep water flow patterns, and abrupt climate change Late Quaternary paleoproductivity and deep water circulation in the eastern South Atlantic Ocean: Evidence from benthic foraminifera Weaker Gulf Stream in the Florida Straits during the Last Glacial Maximum Strong and deep Atlantic meridional overturning circulation during the last glacial cycle The role of the thermohaline circulation in abrupt climate change Old radiocarbon ages in the southwest Pacific Ocean during the last glacial period and deglaciation Reduced North Atlantic Deep Water flux to the glacial Southern Ocean inferred from neodymium isotope ratios Inherently unstable climate behaviour due to weak thermohaline ocean circulation Influence of ocean heat transport on the climate of the Last Glacial Maximum Last Glacial Maximum ocean thermohaline circulation: PMIP2 model intercomparisons and data constraints Ocean circulation and climate during the past 120,000 years Collapse and rapid resumption of Atlantic meridional circulation linked to deglacial climate changes Contribution of Southern Ocean surface-water stratification to low atmospheric CO2 concentrations during the last glacial period Sea-ice switches and abrupt climate change Intensified deep Pacific inflow and ventilation in Pleistocene glacial times Forcing of the deep ocean circulation in simulations of the Last Glacial Maximum Evidence from the high-latitude North Atlantic for variations in Antarctic Intermediate water flow during the last deglaciation

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