The radiolarian fauna during the Younger Dryas–Holocene transition in Andfjorden, northern Norway

We report on the changing radiolarian faunas from the Younger Dryas (ca.12.9 calibrated thousands of years BP [cal. Ky BP]) and into the Holocene (ca. 10.3 cal. Ky BP) in the core JM99-1200 from Andfjorden, northern Norway. Temperature reconstructions using both the Q-mode factor analysis and modern...

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Published in:Polar Research
Main Authors: Kjell R. Bjørklund, Svetlana B. Kruglikova, Øyvind Hammer
Format: Article in Journal/Newspaper
Language:English
Published: Norwegian Polar Institute 2019
Subjects:
Online Access:https://doi.org/10.33265/polar.v38.3444
https://doaj.org/article/d1dae13a4c4a46bd8fce2e9f8544e43f
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spelling ftdoajarticles:oai:doaj.org/article:d1dae13a4c4a46bd8fce2e9f8544e43f 2023-05-15T13:25:31+02:00 The radiolarian fauna during the Younger Dryas–Holocene transition in Andfjorden, northern Norway Kjell R. Bjørklund Svetlana B. Kruglikova Øyvind Hammer 2019-12-01T00:00:00Z https://doi.org/10.33265/polar.v38.3444 https://doaj.org/article/d1dae13a4c4a46bd8fce2e9f8544e43f EN eng Norwegian Polar Institute https://polarresearch.net/index.php/polar/article/view/3444/9586 https://doaj.org/toc/1751-8369 1751-8369 doi:10.33265/polar.v38.3444 https://doaj.org/article/d1dae13a4c4a46bd8fce2e9f8544e43f Polar Research, Vol 38, Iss 0, Pp 1-16 (2019) palaeoclimate biostratigraphy age models preboreal oscillation transfer functions Environmental sciences GE1-350 Oceanography GC1-1581 article 2019 ftdoajarticles https://doi.org/10.33265/polar.v38.3444 2022-12-30T21:58:28Z We report on the changing radiolarian faunas from the Younger Dryas (ca.12.9 calibrated thousands of years BP [cal. Ky BP]) and into the Holocene (ca. 10.3 cal. Ky BP) in the core JM99-1200 from Andfjorden, northern Norway. Temperature reconstructions using both the Q-mode factor analysis and modern analogue technique methods show stable, cold temperatures below ca. 410 cm core depth, followed by abrupt warming into a relatively stable Holocene temperature regime. Age-depth modelling with three different methods gives an age of ca. 11.9–12.0 cal. Ky BP at this core depth, clearly older than the Younger Dryas–Holocene transition at ca. 11.65 cal. Ky BP according to ice core chronology. Considering that the age models may be insufficiently informed in an interval without radiometric dates, it is possible that the base of the Holocene is indeed at 410 cm, as indicated by the radiolarian and other core data. Such a change in the chronology would have implications for previously published work on the JM99-1200 core. Alternatively, the abrupt warming in Andfjorden predated the Younger Dryas–Holocene transition by a few hundred years. A distinct cold pulse at ca. 315–335 cm, or 11.4–11.5 cal. Ky BP is interpreted as the Preboreal Oscillation. The Preboreal Oscillation has not previously been detected in temperature curves based on planktic foraminifera in the same core, indicating that Radiolaria may be a more sensitive temperature indicator in this region. Article in Journal/Newspaper Andfjorden ice core Northern Norway Polar Research Directory of Open Access Journals: DOAJ Articles Norway Andfjorden ENVELOPE(16.333,16.333,69.167,69.167) Polar Research 38 0
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic palaeoclimate
biostratigraphy
age models
preboreal oscillation
transfer functions
Environmental sciences
GE1-350
Oceanography
GC1-1581
spellingShingle palaeoclimate
biostratigraphy
age models
preboreal oscillation
transfer functions
Environmental sciences
GE1-350
Oceanography
GC1-1581
Kjell R. Bjørklund
Svetlana B. Kruglikova
Øyvind Hammer
The radiolarian fauna during the Younger Dryas–Holocene transition in Andfjorden, northern Norway
topic_facet palaeoclimate
biostratigraphy
age models
preboreal oscillation
transfer functions
Environmental sciences
GE1-350
Oceanography
GC1-1581
description We report on the changing radiolarian faunas from the Younger Dryas (ca.12.9 calibrated thousands of years BP [cal. Ky BP]) and into the Holocene (ca. 10.3 cal. Ky BP) in the core JM99-1200 from Andfjorden, northern Norway. Temperature reconstructions using both the Q-mode factor analysis and modern analogue technique methods show stable, cold temperatures below ca. 410 cm core depth, followed by abrupt warming into a relatively stable Holocene temperature regime. Age-depth modelling with three different methods gives an age of ca. 11.9–12.0 cal. Ky BP at this core depth, clearly older than the Younger Dryas–Holocene transition at ca. 11.65 cal. Ky BP according to ice core chronology. Considering that the age models may be insufficiently informed in an interval without radiometric dates, it is possible that the base of the Holocene is indeed at 410 cm, as indicated by the radiolarian and other core data. Such a change in the chronology would have implications for previously published work on the JM99-1200 core. Alternatively, the abrupt warming in Andfjorden predated the Younger Dryas–Holocene transition by a few hundred years. A distinct cold pulse at ca. 315–335 cm, or 11.4–11.5 cal. Ky BP is interpreted as the Preboreal Oscillation. The Preboreal Oscillation has not previously been detected in temperature curves based on planktic foraminifera in the same core, indicating that Radiolaria may be a more sensitive temperature indicator in this region.
format Article in Journal/Newspaper
author Kjell R. Bjørklund
Svetlana B. Kruglikova
Øyvind Hammer
author_facet Kjell R. Bjørklund
Svetlana B. Kruglikova
Øyvind Hammer
author_sort Kjell R. Bjørklund
title The radiolarian fauna during the Younger Dryas–Holocene transition in Andfjorden, northern Norway
title_short The radiolarian fauna during the Younger Dryas–Holocene transition in Andfjorden, northern Norway
title_full The radiolarian fauna during the Younger Dryas–Holocene transition in Andfjorden, northern Norway
title_fullStr The radiolarian fauna during the Younger Dryas–Holocene transition in Andfjorden, northern Norway
title_full_unstemmed The radiolarian fauna during the Younger Dryas–Holocene transition in Andfjorden, northern Norway
title_sort radiolarian fauna during the younger dryas–holocene transition in andfjorden, northern norway
publisher Norwegian Polar Institute
publishDate 2019
url https://doi.org/10.33265/polar.v38.3444
https://doaj.org/article/d1dae13a4c4a46bd8fce2e9f8544e43f
long_lat ENVELOPE(16.333,16.333,69.167,69.167)
geographic Norway
Andfjorden
geographic_facet Norway
Andfjorden
genre Andfjorden
ice core
Northern Norway
Polar Research
genre_facet Andfjorden
ice core
Northern Norway
Polar Research
op_source Polar Research, Vol 38, Iss 0, Pp 1-16 (2019)
op_relation https://polarresearch.net/index.php/polar/article/view/3444/9586
https://doaj.org/toc/1751-8369
1751-8369
doi:10.33265/polar.v38.3444
https://doaj.org/article/d1dae13a4c4a46bd8fce2e9f8544e43f
op_doi https://doi.org/10.33265/polar.v38.3444
container_title Polar Research
container_volume 38
container_issue 0
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