Age determination and grwoth rates of stalagmites and stalactites from the Okshola cave, Fauske, northern Norway, supplement to: Linge, Henriette; Lauritzen, Stein-Erik; Andersson, Carin; Hansen, J K; Skoglund, Rannveig O; Sundqvist, H S (2009): Stable isotope records for the last 10000 years from Okshola cave (Fauske, northern Norway) and regional comparisons. Climate of the Past, 5(4), 667-682
The sensitivity of terrestrial environments to past changes in heat transport is expected to be manifested in Holocene climate proxy records on millennial to seasonal timescales. Stalagmite formation in the Okshola cave near Fauske (northern Norway) began at about 10.4 ka, soon after the valley was...
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ftdatacite:10.1594/pangaea.728964 2023-05-15T17:43:22+02:00 Age determination and grwoth rates of stalagmites and stalactites from the Okshola cave, Fauske, northern Norway, supplement to: Linge, Henriette; Lauritzen, Stein-Erik; Andersson, Carin; Hansen, J K; Skoglund, Rannveig O; Sundqvist, H S (2009): Stable isotope records for the last 10000 years from Okshola cave (Fauske, northern Norway) and regional comparisons. Climate of the Past, 5(4), 667-682 Linge, Henriette Lauritzen, Stein-Erik Andersson, Carin Hansen, J K Skoglund, Rannveig O Sundqvist, H S 2009 application/zip https://dx.doi.org/10.1594/pangaea.728964 https://doi.pangaea.de/10.1594/PANGAEA.728964 en eng PANGAEA - Data Publisher for Earth & Environmental Science https://dx.doi.org/10.5194/cp-5-667-2009 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 CC-BY Speleothem sample article Supplementary Collection of Datasets Collection 2009 ftdatacite https://doi.org/10.1594/pangaea.728964 https://doi.org/10.5194/cp-5-667-2009 2022-02-09T13:33:23Z The sensitivity of terrestrial environments to past changes in heat transport is expected to be manifested in Holocene climate proxy records on millennial to seasonal timescales. Stalagmite formation in the Okshola cave near Fauske (northern Norway) began at about 10.4 ka, soon after the valley was deglaciated. Past monitoring of the cave and surface has revealed stable modern conditions with uniform drip rates, relative humidity and temperature. Stable isotope records from two stalagmites provide time-series spanning from c. 10380 yr to AD 1997; a banded, multi-coloured stalagmite (Oks82) was formed between 10380 yr and 5050 yr, whereas a pristine, white stalagmite (FM3) covers the period from ~7500 yr to the present. The stable oxygen isotope (delta18Oc), stable carbon isotope (delta13Cc), and growth rate records are interpreted as showing i) a negative correlation between cave/surface temperature and delta18Oc, ii) a positive correlation between wetness and delta13Cc, and iii) a positive correlation between temperature and growth rate. Following this, the data from Okshola show that the Holocene was characterised by high-variability climate in the early part, low-variability climate in the middle part, and high-variability climate and shifts between two distinct modes in the late part.A total of nine Scandinavian stalagmite delta18Oc records of comparable dating precision are now available for parts or most of the Holocene. None of them show a clear Holocene thermal optimum, suggesting that they are influenced by annual mean temperature (cave temperature) rather than seasonal temperature. For the last 1000 years, delta18Oc values display a depletion-enrichment-depletion pattern commonly interpreted as reflecting the conventional view on climate development for the last millennium. Although the delta18Oc records show similar patterns and amplitudes of change, the main challenges for utilising high-latitude stalagmites as palaeoclimate archives are i) the accuracy of the age models, ii) the ambiguity of the proxy signals, and iii) calibration with monitoring data. Article in Journal/Newspaper Northern Norway DataCite Metadata Store (German National Library of Science and Technology) Fauske ENVELOPE(15.392,15.392,67.259,67.259) Norway Skoglund ENVELOPE(12.753,12.753,65.913,65.913) |
institution |
Open Polar |
collection |
DataCite Metadata Store (German National Library of Science and Technology) |
op_collection_id |
ftdatacite |
language |
English |
topic |
Speleothem sample |
spellingShingle |
Speleothem sample Linge, Henriette Lauritzen, Stein-Erik Andersson, Carin Hansen, J K Skoglund, Rannveig O Sundqvist, H S Age determination and grwoth rates of stalagmites and stalactites from the Okshola cave, Fauske, northern Norway, supplement to: Linge, Henriette; Lauritzen, Stein-Erik; Andersson, Carin; Hansen, J K; Skoglund, Rannveig O; Sundqvist, H S (2009): Stable isotope records for the last 10000 years from Okshola cave (Fauske, northern Norway) and regional comparisons. Climate of the Past, 5(4), 667-682 |
topic_facet |
Speleothem sample |
description |
The sensitivity of terrestrial environments to past changes in heat transport is expected to be manifested in Holocene climate proxy records on millennial to seasonal timescales. Stalagmite formation in the Okshola cave near Fauske (northern Norway) began at about 10.4 ka, soon after the valley was deglaciated. Past monitoring of the cave and surface has revealed stable modern conditions with uniform drip rates, relative humidity and temperature. Stable isotope records from two stalagmites provide time-series spanning from c. 10380 yr to AD 1997; a banded, multi-coloured stalagmite (Oks82) was formed between 10380 yr and 5050 yr, whereas a pristine, white stalagmite (FM3) covers the period from ~7500 yr to the present. The stable oxygen isotope (delta18Oc), stable carbon isotope (delta13Cc), and growth rate records are interpreted as showing i) a negative correlation between cave/surface temperature and delta18Oc, ii) a positive correlation between wetness and delta13Cc, and iii) a positive correlation between temperature and growth rate. Following this, the data from Okshola show that the Holocene was characterised by high-variability climate in the early part, low-variability climate in the middle part, and high-variability climate and shifts between two distinct modes in the late part.A total of nine Scandinavian stalagmite delta18Oc records of comparable dating precision are now available for parts or most of the Holocene. None of them show a clear Holocene thermal optimum, suggesting that they are influenced by annual mean temperature (cave temperature) rather than seasonal temperature. For the last 1000 years, delta18Oc values display a depletion-enrichment-depletion pattern commonly interpreted as reflecting the conventional view on climate development for the last millennium. Although the delta18Oc records show similar patterns and amplitudes of change, the main challenges for utilising high-latitude stalagmites as palaeoclimate archives are i) the accuracy of the age models, ii) the ambiguity of the proxy signals, and iii) calibration with monitoring data. |
format |
Article in Journal/Newspaper |
author |
Linge, Henriette Lauritzen, Stein-Erik Andersson, Carin Hansen, J K Skoglund, Rannveig O Sundqvist, H S |
author_facet |
Linge, Henriette Lauritzen, Stein-Erik Andersson, Carin Hansen, J K Skoglund, Rannveig O Sundqvist, H S |
author_sort |
Linge, Henriette |
title |
Age determination and grwoth rates of stalagmites and stalactites from the Okshola cave, Fauske, northern Norway, supplement to: Linge, Henriette; Lauritzen, Stein-Erik; Andersson, Carin; Hansen, J K; Skoglund, Rannveig O; Sundqvist, H S (2009): Stable isotope records for the last 10000 years from Okshola cave (Fauske, northern Norway) and regional comparisons. Climate of the Past, 5(4), 667-682 |
title_short |
Age determination and grwoth rates of stalagmites and stalactites from the Okshola cave, Fauske, northern Norway, supplement to: Linge, Henriette; Lauritzen, Stein-Erik; Andersson, Carin; Hansen, J K; Skoglund, Rannveig O; Sundqvist, H S (2009): Stable isotope records for the last 10000 years from Okshola cave (Fauske, northern Norway) and regional comparisons. Climate of the Past, 5(4), 667-682 |
title_full |
Age determination and grwoth rates of stalagmites and stalactites from the Okshola cave, Fauske, northern Norway, supplement to: Linge, Henriette; Lauritzen, Stein-Erik; Andersson, Carin; Hansen, J K; Skoglund, Rannveig O; Sundqvist, H S (2009): Stable isotope records for the last 10000 years from Okshola cave (Fauske, northern Norway) and regional comparisons. Climate of the Past, 5(4), 667-682 |
title_fullStr |
Age determination and grwoth rates of stalagmites and stalactites from the Okshola cave, Fauske, northern Norway, supplement to: Linge, Henriette; Lauritzen, Stein-Erik; Andersson, Carin; Hansen, J K; Skoglund, Rannveig O; Sundqvist, H S (2009): Stable isotope records for the last 10000 years from Okshola cave (Fauske, northern Norway) and regional comparisons. Climate of the Past, 5(4), 667-682 |
title_full_unstemmed |
Age determination and grwoth rates of stalagmites and stalactites from the Okshola cave, Fauske, northern Norway, supplement to: Linge, Henriette; Lauritzen, Stein-Erik; Andersson, Carin; Hansen, J K; Skoglund, Rannveig O; Sundqvist, H S (2009): Stable isotope records for the last 10000 years from Okshola cave (Fauske, northern Norway) and regional comparisons. Climate of the Past, 5(4), 667-682 |
title_sort |
age determination and grwoth rates of stalagmites and stalactites from the okshola cave, fauske, northern norway, supplement to: linge, henriette; lauritzen, stein-erik; andersson, carin; hansen, j k; skoglund, rannveig o; sundqvist, h s (2009): stable isotope records for the last 10000 years from okshola cave (fauske, northern norway) and regional comparisons. climate of the past, 5(4), 667-682 |
publisher |
PANGAEA - Data Publisher for Earth & Environmental Science |
publishDate |
2009 |
url |
https://dx.doi.org/10.1594/pangaea.728964 https://doi.pangaea.de/10.1594/PANGAEA.728964 |
long_lat |
ENVELOPE(15.392,15.392,67.259,67.259) ENVELOPE(12.753,12.753,65.913,65.913) |
geographic |
Fauske Norway Skoglund |
geographic_facet |
Fauske Norway Skoglund |
genre |
Northern Norway |
genre_facet |
Northern Norway |
op_relation |
https://dx.doi.org/10.5194/cp-5-667-2009 |
op_rights |
Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 |
op_rightsnorm |
CC-BY |
op_doi |
https://doi.org/10.1594/pangaea.728964 https://doi.org/10.5194/cp-5-667-2009 |
_version_ |
1766145428892418048 |