Age determination of sediment core V23-81 (Table 1)
Sharp jumps in climate punctuate the records from borings in the Greenland ice cap during the time interval 60,000 to about 20,000 yr ago. Rapid fluctuations are also seen in foraminifera records for cores from the northern Atlantic and in a pollen record from a core from a bog in the Vosges Mountai...
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ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.726285 2023-05-15T16:27:40+02:00 Age determination of sediment core V23-81 (Table 1) Broecker, Wallace S Andree, Michael Bonani, Georges Wolfli, Willy Oeschger, Hans Klas, Mieczyslawa LATITUDE: 54.250000 * LONGITUDE: -16.830000 * DATE/TIME START: 1966-10-18T00:00:00 * DATE/TIME END: 1966-10-18T00:00:00 * MINIMUM DEPTH, sediment/rock: 1.545 m * MAXIMUM DEPTH, sediment/rock: 4.995 m 1988-07-30 text/tab-separated-values, 68 data points https://doi.pangaea.de/10.1594/PANGAEA.726285 https://doi.org/10.1594/PANGAEA.726285 en eng PANGAEA https://doi.pangaea.de/10.1594/PANGAEA.726285 https://doi.org/10.1594/PANGAEA.726285 CC-BY-3.0: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted info:eu-repo/semantics/openAccess CC-BY Supplement to: Broecker, Wallace S; Andree, Michael; Bonani, Georges; Wolfli, Willy; Oeschger, Hans; Klas, Mieczyslawa (1988): Can the Greenland climatic jumps be identified in records from ocean and land? Quaternary Research, 30(1), 1-6, https://doi.org/10.1016/0033-5894(88)90082-8 Age 14C AMS 14C milieu/reservoir corrected (-400 yr) dated dated standard deviation Depth bottom/max sediment/rock top/min PC Piston corer V23 V23-81 Vema Dataset 1988 ftpangaea https://doi.org/10.1594/PANGAEA.726285 https://doi.org/10.1016/0033-5894(88)90082-8 2023-01-20T08:49:19Z Sharp jumps in climate punctuate the records from borings in the Greenland ice cap during the time interval 60,000 to about 20,000 yr ago. Rapid fluctuations are also seen in foraminifera records for cores from the northern Atlantic and in a pollen record from a core from a bog in the Vosges Mountains in France. In this paper we present a new radiocarbon chronology for northern Atlantic deep-sea core V23-81 which permits comparison with the radiocarbon-dated Vosges Mountains pollen record. Because of the lack of a 14C chronology for the Greenland ice record and of distortions peculiar to each of the three records, it is not yet possible to say whether or not the events are genetically related. Dataset Greenland Ice cap PANGAEA - Data Publisher for Earth & Environmental Science Greenland ENVELOPE(-16.830000,-16.830000,54.250000,54.250000) |
institution |
Open Polar |
collection |
PANGAEA - Data Publisher for Earth & Environmental Science |
op_collection_id |
ftpangaea |
language |
English |
topic |
Age 14C AMS 14C milieu/reservoir corrected (-400 yr) dated dated standard deviation Depth bottom/max sediment/rock top/min PC Piston corer V23 V23-81 Vema |
spellingShingle |
Age 14C AMS 14C milieu/reservoir corrected (-400 yr) dated dated standard deviation Depth bottom/max sediment/rock top/min PC Piston corer V23 V23-81 Vema Broecker, Wallace S Andree, Michael Bonani, Georges Wolfli, Willy Oeschger, Hans Klas, Mieczyslawa Age determination of sediment core V23-81 (Table 1) |
topic_facet |
Age 14C AMS 14C milieu/reservoir corrected (-400 yr) dated dated standard deviation Depth bottom/max sediment/rock top/min PC Piston corer V23 V23-81 Vema |
description |
Sharp jumps in climate punctuate the records from borings in the Greenland ice cap during the time interval 60,000 to about 20,000 yr ago. Rapid fluctuations are also seen in foraminifera records for cores from the northern Atlantic and in a pollen record from a core from a bog in the Vosges Mountains in France. In this paper we present a new radiocarbon chronology for northern Atlantic deep-sea core V23-81 which permits comparison with the radiocarbon-dated Vosges Mountains pollen record. Because of the lack of a 14C chronology for the Greenland ice record and of distortions peculiar to each of the three records, it is not yet possible to say whether or not the events are genetically related. |
format |
Dataset |
author |
Broecker, Wallace S Andree, Michael Bonani, Georges Wolfli, Willy Oeschger, Hans Klas, Mieczyslawa |
author_facet |
Broecker, Wallace S Andree, Michael Bonani, Georges Wolfli, Willy Oeschger, Hans Klas, Mieczyslawa |
author_sort |
Broecker, Wallace S |
title |
Age determination of sediment core V23-81 (Table 1) |
title_short |
Age determination of sediment core V23-81 (Table 1) |
title_full |
Age determination of sediment core V23-81 (Table 1) |
title_fullStr |
Age determination of sediment core V23-81 (Table 1) |
title_full_unstemmed |
Age determination of sediment core V23-81 (Table 1) |
title_sort |
age determination of sediment core v23-81 (table 1) |
publisher |
PANGAEA |
publishDate |
1988 |
url |
https://doi.pangaea.de/10.1594/PANGAEA.726285 https://doi.org/10.1594/PANGAEA.726285 |
op_coverage |
LATITUDE: 54.250000 * LONGITUDE: -16.830000 * DATE/TIME START: 1966-10-18T00:00:00 * DATE/TIME END: 1966-10-18T00:00:00 * MINIMUM DEPTH, sediment/rock: 1.545 m * MAXIMUM DEPTH, sediment/rock: 4.995 m |
long_lat |
ENVELOPE(-16.830000,-16.830000,54.250000,54.250000) |
geographic |
Greenland |
geographic_facet |
Greenland |
genre |
Greenland Ice cap |
genre_facet |
Greenland Ice cap |
op_source |
Supplement to: Broecker, Wallace S; Andree, Michael; Bonani, Georges; Wolfli, Willy; Oeschger, Hans; Klas, Mieczyslawa (1988): Can the Greenland climatic jumps be identified in records from ocean and land? Quaternary Research, 30(1), 1-6, https://doi.org/10.1016/0033-5894(88)90082-8 |
op_relation |
https://doi.pangaea.de/10.1594/PANGAEA.726285 https://doi.org/10.1594/PANGAEA.726285 |
op_rights |
CC-BY-3.0: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted info:eu-repo/semantics/openAccess |
op_rightsnorm |
CC-BY |
op_doi |
https://doi.org/10.1594/PANGAEA.726285 https://doi.org/10.1016/0033-5894(88)90082-8 |
_version_ |
1766017113835700224 |