(Table 2) Radiocarbon content and 14C AMS ages of planktonic foraminifera from sediment cores Louis_1900 and Louis_2023 ...

North American freshwater runoff records have been used to support the case that climate flickers were caused by shutdowns of the ocean thermohaline circulation (THC) resulting from reversals of meltwater discharges. Inconsistencies in the documentation of these meltwater switches, however, continue...

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Bibliographic Details
Main Author: Aharon, Paul
Format: Dataset
Language:English
Published: PANGAEA 2003
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.841362
https://doi.pangaea.de/10.1594/PANGAEA.841362
id ftdatacite:10.1594/pangaea.841362
record_format openpolar
spelling ftdatacite:10.1594/pangaea.841362 2024-09-09T19:45:22+00:00 (Table 2) Radiocarbon content and 14C AMS ages of planktonic foraminifera from sediment cores Louis_1900 and Louis_2023 ... Aharon, Paul 2003 text/tab-separated-values https://dx.doi.org/10.1594/pangaea.841362 https://doi.pangaea.de/10.1594/PANGAEA.841362 en eng PANGAEA https://dx.doi.org/10.1029/2002pa000840 https://dx.doi.org/10.1130/0016-7606(1997)109<0568:rdoshs>2.3.co;2 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Event label DEPTH, sediment/rock Species Globigerinoides ruber, δ13C Δ14C Δ14C, standard deviation Age, dated Age, dated standard deviation Piston corer Age, 14C milieu/reservoir corrected -400 yr dataset Supplementary Dataset Dataset 2003 ftdatacite https://doi.org/10.1594/pangaea.84136210.1029/2002pa00084010.1130/0016-7606(1997)109<0568:rdoshs>2.3.co;2 2024-08-01T10:59:11Z North American freshwater runoff records have been used to support the case that climate flickers were caused by shutdowns of the ocean thermohaline circulation (THC) resulting from reversals of meltwater discharges. Inconsistencies in the documentation of these meltwater switches, however, continue to fuel the debate on the cause/s of the oscillatory nature of the deglacial climate. New oxygen and carbon isotope records from the northern Gulf of Mexico depict in exceptional detail the succession of meltwater floods and pauses through the southern routing during the interval 16 to 8.9 ka (14C years BP; ka, kiloannum). The records underscore the bimodal role played by the Gulf of Mexico as a destination of meltwater discharges from the receding Laurentide Ice Sheet. The evidence indicates that the Gulf of Mexico acted as the principal source of superfloods at 13.4, 12.6, and 11.9 ka that reached the North Atlantic and contributed significantly to density stratification, disruption of ocean ventilation, and ... : A 1 cm thick slice of sediment was used for sample processing. ... Dataset Ice Sheet North Atlantic Planktonic foraminifera DataCite
institution Open Polar
collection DataCite
op_collection_id ftdatacite
language English
topic Event label
DEPTH, sediment/rock
Species
Globigerinoides ruber, δ13C
Δ14C
Δ14C, standard deviation
Age, dated
Age, dated standard deviation
Piston corer
Age, 14C milieu/reservoir corrected -400 yr
spellingShingle Event label
DEPTH, sediment/rock
Species
Globigerinoides ruber, δ13C
Δ14C
Δ14C, standard deviation
Age, dated
Age, dated standard deviation
Piston corer
Age, 14C milieu/reservoir corrected -400 yr
Aharon, Paul
(Table 2) Radiocarbon content and 14C AMS ages of planktonic foraminifera from sediment cores Louis_1900 and Louis_2023 ...
topic_facet Event label
DEPTH, sediment/rock
Species
Globigerinoides ruber, δ13C
Δ14C
Δ14C, standard deviation
Age, dated
Age, dated standard deviation
Piston corer
Age, 14C milieu/reservoir corrected -400 yr
description North American freshwater runoff records have been used to support the case that climate flickers were caused by shutdowns of the ocean thermohaline circulation (THC) resulting from reversals of meltwater discharges. Inconsistencies in the documentation of these meltwater switches, however, continue to fuel the debate on the cause/s of the oscillatory nature of the deglacial climate. New oxygen and carbon isotope records from the northern Gulf of Mexico depict in exceptional detail the succession of meltwater floods and pauses through the southern routing during the interval 16 to 8.9 ka (14C years BP; ka, kiloannum). The records underscore the bimodal role played by the Gulf of Mexico as a destination of meltwater discharges from the receding Laurentide Ice Sheet. The evidence indicates that the Gulf of Mexico acted as the principal source of superfloods at 13.4, 12.6, and 11.9 ka that reached the North Atlantic and contributed significantly to density stratification, disruption of ocean ventilation, and ... : A 1 cm thick slice of sediment was used for sample processing. ...
format Dataset
author Aharon, Paul
author_facet Aharon, Paul
author_sort Aharon, Paul
title (Table 2) Radiocarbon content and 14C AMS ages of planktonic foraminifera from sediment cores Louis_1900 and Louis_2023 ...
title_short (Table 2) Radiocarbon content and 14C AMS ages of planktonic foraminifera from sediment cores Louis_1900 and Louis_2023 ...
title_full (Table 2) Radiocarbon content and 14C AMS ages of planktonic foraminifera from sediment cores Louis_1900 and Louis_2023 ...
title_fullStr (Table 2) Radiocarbon content and 14C AMS ages of planktonic foraminifera from sediment cores Louis_1900 and Louis_2023 ...
title_full_unstemmed (Table 2) Radiocarbon content and 14C AMS ages of planktonic foraminifera from sediment cores Louis_1900 and Louis_2023 ...
title_sort (table 2) radiocarbon content and 14c ams ages of planktonic foraminifera from sediment cores louis_1900 and louis_2023 ...
publisher PANGAEA
publishDate 2003
url https://dx.doi.org/10.1594/pangaea.841362
https://doi.pangaea.de/10.1594/PANGAEA.841362
genre Ice Sheet
North Atlantic
Planktonic foraminifera
genre_facet Ice Sheet
North Atlantic
Planktonic foraminifera
op_relation https://dx.doi.org/10.1029/2002pa000840
https://dx.doi.org/10.1130/0016-7606(1997)109<0568:rdoshs>2.3.co;2
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.84136210.1029/2002pa00084010.1130/0016-7606(1997)109<0568:rdoshs>2.3.co;2
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