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Speleothem fluid inclusion water isotopes and inferred temperatures from Milandre Cave, Switzerland
appsOther research productkeyboard_double_arrow_right Collection 2019 English PANGAEA SNSF | STALCLIM II - Multi-proxy...
SNSF| STALCLIM II - Multi-proxy climatic and environmental reconstructions from stalagmites from Switzerland, Turkey, Arabia and India
Authors: Affolter, Stéphane; Häuselmann, Anamaria Diana; Fleitmann, Dominik; Edwards, R Lawrence; +2 Authors
Affolter, Stéphane; Häuselmann, Anamaria Diana; Fleitmann, Dominik; Edwards, R Lawrence; Cheng, Hai; Leuenberger, Markus Christian;
The reasons for the early Holocene temperature discrepancy between northern hemispheric model simulations and paleoclimate reconstructions—known as the Holocene temperature conundrum—remain unclear. Using hydrogen isotopes of fluid inclusion water extracted from stalagmites from the Milandre Cave in Switzerland, we established a mid-latitude European mean annual temperature reconstruction for the past 14,000 years. Our Milandre Cave fluid inclusion temperature record (MC-FIT) resembles Greenland and Mediterranean sea surface temperature trends but differs from recent reconstructions obtained from biogenic proxies and climate models. The water isotopes are further synchronized with tropical precipitation records, stressing the Northern Hemisphere signature. Our results support the existence of a European Holocene Thermal Maximum and data model temperature discrepancies. Moreover, data-data comparison reveals a significant latitudinal temperature gradient within Europe. Last, the MC-FIT record suggests that seasonal biases in the proxies are not the primary cause of the Holocene temperature conundrum.
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PANGAEA - Data Publisher for Earth and Environmental Science
Collection . 2019
License: http://creativecommons.org/licenses/by-nc/4.0/
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Collection . 2019
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Black carbon (rBC), bismuth, lead and others from 1741 to 2015 AD from Colle Gnifetti ice core (Swiss/Italian Alps)
appsOther research productkeyboard_double_arrow_right Collection 2018 English PANGAEA SNSF | Paleo fires from high-alp...
SNSF| Paleo fires from high-alpine ice cores
Authors: Sigl, Michael; Abram, Nerilie J; Gabrieli, Jacopo; Jenk, Theo M; +2 Authors
Sigl, Michael; Abram, Nerilie J; Gabrieli, Jacopo; Jenk, Theo M; Osmont, Dimitri; Schwikowski, Margit;
We present sub-annually resolved concentration records of refractory black carbon (rBC; using soot photometry) as well as distinctive tracers for mineral dust (calcium, sulfate, sodium), biomass burning (ammonium) and industrial pollution (lead, bismuth, ammonium, nitrate) from the Colle Gnifetti (4450 m asl; 45.932°N, 7.876°E) ice core in the Alps from 1741-2015 AD. The data is a composite of two ice cores: CG03B drilled in 2003; CG15 drilled in 2015 at the same site.
PANGAEA - Data Publi...arrow_drop_down
PANGAEA - Data Publisher for Earth and Environmental Science
Collection . 2018
License: http://creativecommons.org/licenses/by/4.0/
Data sources: PANGAEA - Data Publisher for Earth and Environmental Science
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Collection . 2018
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The following results are related to European Marine Science. Are you interested to view more results? Visit OpenAIRE - Explore.

2 Research products

Speleothem fluid inclusion water isotopes and inferred temperatures from Milandre Cave, Switzerland
appsOther research productkeyboard_double_arrow_right Collection 2019 English PANGAEA SNSF | STALCLIM II - Multi-proxy...
SNSF| STALCLIM II - Multi-proxy climatic and environmental reconstructions from stalagmites from Switzerland, Turkey, Arabia and India
Authors: Affolter, Stéphane; Häuselmann, Anamaria Diana; Fleitmann, Dominik; Edwards, R Lawrence; +2 Authors
Affolter, Stéphane; Häuselmann, Anamaria Diana; Fleitmann, Dominik; Edwards, R Lawrence; Cheng, Hai; Leuenberger, Markus Christian;
The reasons for the early Holocene temperature discrepancy between northern hemispheric model simulations and paleoclimate reconstructions—known as the Holocene temperature conundrum—remain unclear. Using hydrogen isotopes of fluid inclusion water extracted from stalagmites from the Milandre Cave in Switzerland, we established a mid-latitude European mean annual temperature reconstruction for the past 14,000 years. Our Milandre Cave fluid inclusion temperature record (MC-FIT) resembles Greenland and Mediterranean sea surface temperature trends but differs from recent reconstructions obtained from biogenic proxies and climate models. The water isotopes are further synchronized with tropical precipitation records, stressing the Northern Hemisphere signature. Our results support the existence of a European Holocene Thermal Maximum and data model temperature discrepancies. Moreover, data-data comparison reveals a significant latitudinal temperature gradient within Europe. Last, the MC-FIT record suggests that seasonal biases in the proxies are not the primary cause of the Holocene temperature conundrum.
PANGAEA - Data Publi...arrow_drop_down
PANGAEA - Data Publisher for Earth and Environmental Science
Collection . 2019
License: http://creativecommons.org/licenses/by-nc/4.0/
Data sources: PANGAEA - Data Publisher for Earth and Environmental Science
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PANGAEA - Data Publi...arrow_drop_down
PANGAEA - Data Publisher for Earth and Environmental Science
Collection . 2019
License: http://creativecommons.org/licenses/by-nc/4.0/
Data sources: PANGAEA - Data Publisher for Earth and Environmental Science
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Black carbon (rBC), bismuth, lead and others from 1741 to 2015 AD from Colle Gnifetti ice core (Swiss/Italian Alps)
appsOther research productkeyboard_double_arrow_right Collection 2018 English PANGAEA SNSF | Paleo fires from high-alp...
SNSF| Paleo fires from high-alpine ice cores
Authors: Sigl, Michael; Abram, Nerilie J; Gabrieli, Jacopo; Jenk, Theo M; +2 Authors
Sigl, Michael; Abram, Nerilie J; Gabrieli, Jacopo; Jenk, Theo M; Osmont, Dimitri; Schwikowski, Margit;
We present sub-annually resolved concentration records of refractory black carbon (rBC; using soot photometry) as well as distinctive tracers for mineral dust (calcium, sulfate, sodium), biomass burning (ammonium) and industrial pollution (lead, bismuth, ammonium, nitrate) from the Colle Gnifetti (4450 m asl; 45.932°N, 7.876°E) ice core in the Alps from 1741-2015 AD. The data is a composite of two ice cores: CG03B drilled in 2003; CG15 drilled in 2015 at the same site.
PANGAEA - Data Publi...arrow_drop_down
PANGAEA - Data Publisher for Earth and Environmental Science
Collection . 2018
License: http://creativecommons.org/licenses/by/4.0/
Data sources: PANGAEA - Data Publisher for Earth and Environmental Science
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PANGAEA - Data Publi...arrow_drop_down
PANGAEA - Data Publisher for Earth and Environmental Science
Collection . 2018
License: http://creativecommons.org/licenses/by/4.0/
Data sources: PANGAEA - Data Publisher for Earth and Environmental Science
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European Marine Science
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Speleothem fluid inclusion water isotopes and inferred temperatures from Milandre Cave, Switzerland

Black carbon (rBC), bismuth, lead and others from 1741 to 2015 AD from Colle Gnifetti ice core (Swiss/Italian Alps)

Speleothem fluid inclusion water isotopes and inferred temperatures from Milandre Cave, Switzerland

Black carbon (rBC), bismuth, lead and others from 1741 to 2015 AD from Colle Gnifetti ice core (Swiss/Italian Alps)

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Speleothem fluid inclusion water isotopes and inferred temperatures from Milandre Cave, Switzerland

Black carbon (rBC), bismuth, lead and others from 1741 to 2015 AD from Colle Gnifetti ice core (Swiss/Italian Alps)

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Speleothem fluid inclusion water isotopes and inferred temperatures from Milandre Cave, Switzerland

Black carbon (rBC), bismuth, lead and others from 1741 to 2015 AD from Colle Gnifetti ice core (Swiss/Italian Alps)

European Marine Science
Other research products
Swiss National Science Foundation
SNSF|Programmes
CH