(Table 1) Age determination of sediment profile JM96-1225 ...

The paleoceanography in the Denmark Strait, North Atlantic, is reconstructed based on down core analysis of planktonic foraminifera, carbon and oxygen isotopes, carbonate, and ice rafted debris (IRD). The stratigraphy spans 57 to 6 calibrated (cal) ka years and reveals sea surface temperatures that...

Full description

Bibliographic Details
Main Authors: Hagen, Sveinung, Hald, Morten
Format: Dataset
Language:English
Published: PANGAEA 2002
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.842445
https://doi.pangaea.de/10.1594/PANGAEA.842445
id ftdatacite:10.1594/pangaea.842445
record_format openpolar
spelling ftdatacite:10.1594/pangaea.842445 2024-09-15T18:03:36+00:00 (Table 1) Age determination of sediment profile JM96-1225 ... Hagen, Sveinung Hald, Morten 2002 text/tab-separated-values https://dx.doi.org/10.1594/pangaea.842445 https://doi.pangaea.de/10.1594/PANGAEA.842445 en eng PANGAEA https://dx.doi.org/10.1029/2001pa000632 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Laboratory code/label Core DEPTH, sediment/rock Depth, top/min Depth, bottom/max Age, dated material Age, dated Age, dated standard error Calendar age Gravity corer Age, 14C AMS Age, 14C milieu/reservoir corrected -400 yr Age, 14C calibrated JM96 Jan Mayen dataset Supplementary Dataset Dataset 2002 ftdatacite https://doi.org/10.1594/pangaea.84244510.1029/2001pa000632 2024-08-01T10:56:44Z The paleoceanography in the Denmark Strait, North Atlantic, is reconstructed based on down core analysis of planktonic foraminifera, carbon and oxygen isotopes, carbonate, and ice rafted debris (IRD). The stratigraphy spans 57 to 6 calibrated (cal) ka years and reveals sea surface temperatures that covary with Greenland ice core temperatures throughout marine isotope stages (MIS) 3 and 2. Planktonic d18O minima, interpreted as meltwater events, follow sea surface warming. IRD from both the Greenland and Iceland Ice Sheets was delayed by ~2 ka relative to the North Atlantic Heinrich events. Ventilation of bottom water was mostly sustained through open ocean convection associated with North Atlantic Deep Water production or by convection of glacial North Atlantic Intermediate Water, except for two episodes at ~54 cal ka (MIS 3.31) and 18–15 cal ka (termination I). During these two periods we suggest that deep water ventilation was accomplished mainly by brine formation. ... : Supplement to: Hagen, Sveinung; Hald, Morten (2002): Variation in surface and deep water circulation in the Denmark Strait, North Atlantic, during marine isotope stages 3 and 2. Paleoceanography, 17(4), 13-1-13-16 ... Dataset Denmark Strait Greenland Greenland ice core ice core Iceland Jan Mayen North Atlantic Deep Water North Atlantic Planktonic foraminifera DataCite
institution Open Polar
collection DataCite
op_collection_id ftdatacite
language English
topic Laboratory code/label
Core
DEPTH, sediment/rock
Depth, top/min
Depth, bottom/max
Age, dated material
Age, dated
Age, dated standard error
Calendar age
Gravity corer
Age, 14C AMS
Age, 14C milieu/reservoir corrected -400 yr
Age, 14C calibrated
JM96
Jan Mayen
spellingShingle Laboratory code/label
Core
DEPTH, sediment/rock
Depth, top/min
Depth, bottom/max
Age, dated material
Age, dated
Age, dated standard error
Calendar age
Gravity corer
Age, 14C AMS
Age, 14C milieu/reservoir corrected -400 yr
Age, 14C calibrated
JM96
Jan Mayen
Hagen, Sveinung
Hald, Morten
(Table 1) Age determination of sediment profile JM96-1225 ...
topic_facet Laboratory code/label
Core
DEPTH, sediment/rock
Depth, top/min
Depth, bottom/max
Age, dated material
Age, dated
Age, dated standard error
Calendar age
Gravity corer
Age, 14C AMS
Age, 14C milieu/reservoir corrected -400 yr
Age, 14C calibrated
JM96
Jan Mayen
description The paleoceanography in the Denmark Strait, North Atlantic, is reconstructed based on down core analysis of planktonic foraminifera, carbon and oxygen isotopes, carbonate, and ice rafted debris (IRD). The stratigraphy spans 57 to 6 calibrated (cal) ka years and reveals sea surface temperatures that covary with Greenland ice core temperatures throughout marine isotope stages (MIS) 3 and 2. Planktonic d18O minima, interpreted as meltwater events, follow sea surface warming. IRD from both the Greenland and Iceland Ice Sheets was delayed by ~2 ka relative to the North Atlantic Heinrich events. Ventilation of bottom water was mostly sustained through open ocean convection associated with North Atlantic Deep Water production or by convection of glacial North Atlantic Intermediate Water, except for two episodes at ~54 cal ka (MIS 3.31) and 18–15 cal ka (termination I). During these two periods we suggest that deep water ventilation was accomplished mainly by brine formation. ... : Supplement to: Hagen, Sveinung; Hald, Morten (2002): Variation in surface and deep water circulation in the Denmark Strait, North Atlantic, during marine isotope stages 3 and 2. Paleoceanography, 17(4), 13-1-13-16 ...
format Dataset
author Hagen, Sveinung
Hald, Morten
author_facet Hagen, Sveinung
Hald, Morten
author_sort Hagen, Sveinung
title (Table 1) Age determination of sediment profile JM96-1225 ...
title_short (Table 1) Age determination of sediment profile JM96-1225 ...
title_full (Table 1) Age determination of sediment profile JM96-1225 ...
title_fullStr (Table 1) Age determination of sediment profile JM96-1225 ...
title_full_unstemmed (Table 1) Age determination of sediment profile JM96-1225 ...
title_sort (table 1) age determination of sediment profile jm96-1225 ...
publisher PANGAEA
publishDate 2002
url https://dx.doi.org/10.1594/pangaea.842445
https://doi.pangaea.de/10.1594/PANGAEA.842445
genre Denmark Strait
Greenland
Greenland ice core
ice core
Iceland
Jan Mayen
North Atlantic Deep Water
North Atlantic
Planktonic foraminifera
genre_facet Denmark Strait
Greenland
Greenland ice core
ice core
Iceland
Jan Mayen
North Atlantic Deep Water
North Atlantic
Planktonic foraminifera
op_relation https://dx.doi.org/10.1029/2001pa000632
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.84244510.1029/2001pa000632
_version_ 1810441088315424768