Millennial-scale atmospheric CO<sub<2</sub< variations during the Marine Isotope Stage 6 period (190–135 ka)

<p<Using new and previously published <span class="inline-formula"<CO<sub<2</sub<</span< data from the EPICA Dome C ice core (EDC), we reconstruct a new high-resolution record of atmospheric <span class="inline-formula"<CO<sub<2</sub<</span< during Marine Isotope Stage (MIS) 6 (190 to 135 ka) the penultimate glacial period. Similar to the last glacial cycle, where high-resolution data already exists, our record shows that during longer North Atlantic (NA) stadials, millennial <span class="inline-formula"<CO<sub<2</sub<</span< variations during MIS 6 are clearly coincident with the bipolar seesaw signal in the Antarctic temperature record. However, during one short stadial in the NA, atmospheric <span class="inline-formula"<CO<sub<2</sub<</span< variation is small (<span class="inline-formula"<∼5</span< ppm) and the relationship between temperature variations in EDC and atmospheric <span class="inline-formula"<CO<sub<2</sub<</span< is unclear. The magnitude of <span class="inline-formula"<CO<sub<2</sub<</span< increase during Carbon Dioxide Maxima (CDM) is closely related to the NA stadial duration in both MIS 6 and MIS 3 (60–27 ka). This observation implies that during the last two glacials the overall bipolar seesaw coupling of climate and atmospheric <span class="inline-formula"<CO<sub<2</sub<</span< operated similarly. In addition, similar to the last glacial period, CDM during the earliest MIS 6 show different lags with respect to the corresponding abrupt <span class="inline-formula"<CH<sub<4</sub<</span< rises, the latter reflecting rapid warming in the Northern Hemisphere (NH). During MIS 6i at around <span class="inline-formula"<181.5±</span<0.3 ka, CDM 6i lags the abrupt warming in the NH by only <span class="inline-formula"<240±</span<320 years. However, during CDM 6iv (<span class="inline-formula"<171.1±</span<0.2 ka) and CDM 6iii (<span class="inline-formula"<175.4±</span<0.4 ka) the lag is much longer: <span class="inline-formula"<1290±</span<540 years on average. We speculate that the size of this lag may be related to a larger expansion of carbon-rich, southern-sourced waters into the Northern Hemisphere in MIS 6, providing a larger carbon reservoir that requires more time to be depleted.</p< Ausführliche Beschreibung

Gespeichert in:

Autor*in:	J. Shin [verfasserIn] C. Nehrbass-Ahles [verfasserIn] R. Grilli [verfasserIn] J. Chowdhry Beeman [verfasserIn] F. Parrenin [verfasserIn] G. Teste [verfasserIn] A. Landais [verfasserIn] L. Schmidely [verfasserIn] L. Silva [verfasserIn] J. Schmitt [verfasserIn] B. Bereiter [verfasserIn] T. F. Stocker [verfasserIn] H. Fischer [verfasserIn] J. Chappellaz [verfasserIn]

Format:	E-Artikel
Sprache:	Englisch

Erschienen:	2020

Übergeordnetes Werk:	In: Climate of the Past - Copernicus Publications, 2005, 16(2020), Seite 2203-2219
Übergeordnetes Werk:	volume:16 ; year:2020 ; pages:2203-2219

Links:	Link aufrufen Link aufrufen Link aufrufen Journal toc Journal toc

DOI / URN:	10.5194/cp-16-2203-2020

Katalog-ID:	DOAJ002800063

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245	1	0	\|a Millennial-scale atmospheric CO<sub<2</sub< variations during the Marine Isotope Stage 6 period (190–135 ka)
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520			\|a <p<Using new and previously published <span class="inline-formula"<CO<sub<2</sub<</span< data from the EPICA Dome C ice core (EDC), we reconstruct a new high-resolution record of atmospheric <span class="inline-formula"<CO<sub<2</sub<</span< during Marine Isotope Stage (MIS) 6 (190 to 135 ka) the penultimate glacial period. Similar to the last glacial cycle, where high-resolution data already exists, our record shows that during longer North Atlantic (NA) stadials, millennial <span class="inline-formula"<CO<sub<2</sub<</span< variations during MIS 6 are clearly coincident with the bipolar seesaw signal in the Antarctic temperature record. However, during one short stadial in the NA, atmospheric <span class="inline-formula"<CO<sub<2</sub<</span< variation is small (<span class="inline-formula"<∼5</span< ppm) and the relationship between temperature variations in EDC and atmospheric <span class="inline-formula"<CO<sub<2</sub<</span< is unclear. The magnitude of <span class="inline-formula"<CO<sub<2</sub<</span< increase during Carbon Dioxide Maxima (CDM) is closely related to the NA stadial duration in both MIS 6 and MIS 3 (60–27 ka). This observation implies that during the last two glacials the overall bipolar seesaw coupling of climate and atmospheric <span class="inline-formula"<CO<sub<2</sub<</span< operated similarly. In addition, similar to the last glacial period, CDM during the earliest MIS 6 show different lags with respect to the corresponding abrupt <span class="inline-formula"<CH<sub<4</sub<</span< rises, the latter reflecting rapid warming in the Northern Hemisphere (NH). During MIS 6i at around <span class="inline-formula"<181.5±</span<0.3 ka, CDM 6i lags the abrupt warming in the NH by only <span class="inline-formula"<240±</span<320 years. However, during CDM 6iv (<span class="inline-formula"<171.1±</span<0.2 ka) and CDM 6iii (<span class="inline-formula"<175.4±</span<0.4 ka) the lag is much longer: <span class="inline-formula"<1290±</span<540 years on average. We speculate that the size of this lag may be related to a larger expansion of carbon-rich, southern-sourced waters into the Northern Hemisphere in MIS 6, providing a larger carbon reservoir that requires more time to be depleted.</p<
653		0	\|a Environmental pollution
653		0	\|a Environmental protection
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700	0		\|a J. Shin \|e verfasserin \|4 aut
700	0		\|a C. Nehrbass-Ahles \|e verfasserin \|4 aut
700	0		\|a C. Nehrbass-Ahles \|e verfasserin \|4 aut
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700	0		\|a J. Chowdhry Beeman \|e verfasserin \|4 aut
700	0		\|a F. Parrenin \|e verfasserin \|4 aut
700	0		\|a G. Teste \|e verfasserin \|4 aut
700	0		\|a A. Landais \|e verfasserin \|4 aut
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700	0		\|a H. Fischer \|e verfasserin \|4 aut
700	0		\|a J. Chappellaz \|e verfasserin \|4 aut
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allfields	10.5194/cp-16-2203-2020 doi (DE-627)DOAJ002800063 (DE-599)DOAJ379f5fb57a4a421d924853aa240c4af9 DE-627 ger DE-627 rakwb eng TD172-193.5 TD169-171.8 GE1-350 J. Shin verfasserin aut Millennial-scale atmospheric CO<sub<2</sub< variations during the Marine Isotope Stage 6 period (190–135 ka) 2020 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier <p<Using new and previously published <span class="inline-formula"<CO<sub<2</sub<</span< data from the EPICA Dome C ice core (EDC), we reconstruct a new high-resolution record of atmospheric <span class="inline-formula"<CO<sub<2</sub<</span< during Marine Isotope Stage (MIS) 6 (190 to 135 ka) the penultimate glacial period. Similar to the last glacial cycle, where high-resolution data already exists, our record shows that during longer North Atlantic (NA) stadials, millennial <span class="inline-formula"<CO<sub<2</sub<</span< variations during MIS 6 are clearly coincident with the bipolar seesaw signal in the Antarctic temperature record. However, during one short stadial in the NA, atmospheric <span class="inline-formula"<CO<sub<2</sub<</span< variation is small (<span class="inline-formula"<∼5</span< ppm) and the relationship between temperature variations in EDC and atmospheric <span class="inline-formula"<CO<sub<2</sub<</span< is unclear. The magnitude of <span class="inline-formula"<CO<sub<2</sub<</span< increase during Carbon Dioxide Maxima (CDM) is closely related to the NA stadial duration in both MIS 6 and MIS 3 (60–27 ka). This observation implies that during the last two glacials the overall bipolar seesaw coupling of climate and atmospheric <span class="inline-formula"<CO<sub<2</sub<</span< operated similarly. In addition, similar to the last glacial period, CDM during the earliest MIS 6 show different lags with respect to the corresponding abrupt <span class="inline-formula"<CH<sub<4</sub<</span< rises, the latter reflecting rapid warming in the Northern Hemisphere (NH). During MIS 6i at around <span class="inline-formula"<181.5±</span<0.3 ka, CDM 6i lags the abrupt warming in the NH by only <span class="inline-formula"<240±</span<320 years. However, during CDM 6iv (<span class="inline-formula"<171.1±</span<0.2 ka) and CDM 6iii (<span class="inline-formula"<175.4±</span<0.4 ka) the lag is much longer: <span class="inline-formula"<1290±</span<540 years on average. We speculate that the size of this lag may be related to a larger expansion of carbon-rich, southern-sourced waters into the Northern Hemisphere in MIS 6, providing a larger carbon reservoir that requires more time to be depleted.</p< Environmental pollution Environmental protection Environmental sciences J. Shin verfasserin aut C. Nehrbass-Ahles verfasserin aut C. Nehrbass-Ahles verfasserin aut R. Grilli verfasserin aut J. Chowdhry Beeman verfasserin aut F. Parrenin verfasserin aut G. Teste verfasserin aut A. Landais verfasserin aut L. Schmidely verfasserin aut L. Silva verfasserin aut J. Schmitt verfasserin aut B. Bereiter verfasserin aut B. Bereiter verfasserin aut B. Bereiter verfasserin aut T. F. Stocker verfasserin aut H. Fischer verfasserin aut J. Chappellaz verfasserin aut In Climate of the Past Copernicus Publications, 2005 16(2020), Seite 2203-2219 (DE-627)505943697 (DE-600)2217985-9 18149332 nnns volume:16 year:2020 pages:2203-2219 https://doi.org/10.5194/cp-16-2203-2020 kostenfrei https://doaj.org/article/379f5fb57a4a421d924853aa240c4af9 kostenfrei https://cp.copernicus.org/articles/16/2203/2020/cp-16-2203-2020.pdf kostenfrei https://doaj.org/toc/1814-9324 Journal toc kostenfrei https://doaj.org/toc/1814-9332 Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_95 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_213 GBV_ILN_230 GBV_ILN_267 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_2014 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_4012 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4249 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4338 GBV_ILN_4367 GBV_ILN_4700 AR 16 2020 2203-2219
spelling	10.5194/cp-16-2203-2020 doi (DE-627)DOAJ002800063 (DE-599)DOAJ379f5fb57a4a421d924853aa240c4af9 DE-627 ger DE-627 rakwb eng TD172-193.5 TD169-171.8 GE1-350 J. Shin verfasserin aut Millennial-scale atmospheric CO<sub<2</sub< variations during the Marine Isotope Stage 6 period (190–135 ka) 2020 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier <p<Using new and previously published <span class="inline-formula"<CO<sub<2</sub<</span< data from the EPICA Dome C ice core (EDC), we reconstruct a new high-resolution record of atmospheric <span class="inline-formula"<CO<sub<2</sub<</span< during Marine Isotope Stage (MIS) 6 (190 to 135 ka) the penultimate glacial period. Similar to the last glacial cycle, where high-resolution data already exists, our record shows that during longer North Atlantic (NA) stadials, millennial <span class="inline-formula"<CO<sub<2</sub<</span< variations during MIS 6 are clearly coincident with the bipolar seesaw signal in the Antarctic temperature record. However, during one short stadial in the NA, atmospheric <span class="inline-formula"<CO<sub<2</sub<</span< variation is small (<span class="inline-formula"<∼5</span< ppm) and the relationship between temperature variations in EDC and atmospheric <span class="inline-formula"<CO<sub<2</sub<</span< is unclear. The magnitude of <span class="inline-formula"<CO<sub<2</sub<</span< increase during Carbon Dioxide Maxima (CDM) is closely related to the NA stadial duration in both MIS 6 and MIS 3 (60–27 ka). This observation implies that during the last two glacials the overall bipolar seesaw coupling of climate and atmospheric <span class="inline-formula"<CO<sub<2</sub<</span< operated similarly. In addition, similar to the last glacial period, CDM during the earliest MIS 6 show different lags with respect to the corresponding abrupt <span class="inline-formula"<CH<sub<4</sub<</span< rises, the latter reflecting rapid warming in the Northern Hemisphere (NH). During MIS 6i at around <span class="inline-formula"<181.5±</span<0.3 ka, CDM 6i lags the abrupt warming in the NH by only <span class="inline-formula"<240±</span<320 years. However, during CDM 6iv (<span class="inline-formula"<171.1±</span<0.2 ka) and CDM 6iii (<span class="inline-formula"<175.4±</span<0.4 ka) the lag is much longer: <span class="inline-formula"<1290±</span<540 years on average. We speculate that the size of this lag may be related to a larger expansion of carbon-rich, southern-sourced waters into the Northern Hemisphere in MIS 6, providing a larger carbon reservoir that requires more time to be depleted.</p< Environmental pollution Environmental protection Environmental sciences J. Shin verfasserin aut C. Nehrbass-Ahles verfasserin aut C. Nehrbass-Ahles verfasserin aut R. Grilli verfasserin aut J. Chowdhry Beeman verfasserin aut F. Parrenin verfasserin aut G. Teste verfasserin aut A. Landais verfasserin aut L. Schmidely verfasserin aut L. Silva verfasserin aut J. Schmitt verfasserin aut B. Bereiter verfasserin aut B. Bereiter verfasserin aut B. Bereiter verfasserin aut T. F. Stocker verfasserin aut H. Fischer verfasserin aut J. Chappellaz verfasserin aut In Climate of the Past Copernicus Publications, 2005 16(2020), Seite 2203-2219 (DE-627)505943697 (DE-600)2217985-9 18149332 nnns volume:16 year:2020 pages:2203-2219 https://doi.org/10.5194/cp-16-2203-2020 kostenfrei https://doaj.org/article/379f5fb57a4a421d924853aa240c4af9 kostenfrei https://cp.copernicus.org/articles/16/2203/2020/cp-16-2203-2020.pdf kostenfrei https://doaj.org/toc/1814-9324 Journal toc kostenfrei https://doaj.org/toc/1814-9332 Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_95 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_213 GBV_ILN_230 GBV_ILN_267 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_2014 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_4012 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4249 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4338 GBV_ILN_4367 GBV_ILN_4700 AR 16 2020 2203-2219
allfields_unstemmed	10.5194/cp-16-2203-2020 doi (DE-627)DOAJ002800063 (DE-599)DOAJ379f5fb57a4a421d924853aa240c4af9 DE-627 ger DE-627 rakwb eng TD172-193.5 TD169-171.8 GE1-350 J. Shin verfasserin aut Millennial-scale atmospheric CO<sub<2</sub< variations during the Marine Isotope Stage 6 period (190–135 ka) 2020 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier <p<Using new and previously published <span class="inline-formula"<CO<sub<2</sub<</span< data from the EPICA Dome C ice core (EDC), we reconstruct a new high-resolution record of atmospheric <span class="inline-formula"<CO<sub<2</sub<</span< during Marine Isotope Stage (MIS) 6 (190 to 135 ka) the penultimate glacial period. Similar to the last glacial cycle, where high-resolution data already exists, our record shows that during longer North Atlantic (NA) stadials, millennial <span class="inline-formula"<CO<sub<2</sub<</span< variations during MIS 6 are clearly coincident with the bipolar seesaw signal in the Antarctic temperature record. However, during one short stadial in the NA, atmospheric <span class="inline-formula"<CO<sub<2</sub<</span< variation is small (<span class="inline-formula"<∼5</span< ppm) and the relationship between temperature variations in EDC and atmospheric <span class="inline-formula"<CO<sub<2</sub<</span< is unclear. The magnitude of <span class="inline-formula"<CO<sub<2</sub<</span< increase during Carbon Dioxide Maxima (CDM) is closely related to the NA stadial duration in both MIS 6 and MIS 3 (60–27 ka). This observation implies that during the last two glacials the overall bipolar seesaw coupling of climate and atmospheric <span class="inline-formula"<CO<sub<2</sub<</span< operated similarly. In addition, similar to the last glacial period, CDM during the earliest MIS 6 show different lags with respect to the corresponding abrupt <span class="inline-formula"<CH<sub<4</sub<</span< rises, the latter reflecting rapid warming in the Northern Hemisphere (NH). During MIS 6i at around <span class="inline-formula"<181.5±</span<0.3 ka, CDM 6i lags the abrupt warming in the NH by only <span class="inline-formula"<240±</span<320 years. However, during CDM 6iv (<span class="inline-formula"<171.1±</span<0.2 ka) and CDM 6iii (<span class="inline-formula"<175.4±</span<0.4 ka) the lag is much longer: <span class="inline-formula"<1290±</span<540 years on average. We speculate that the size of this lag may be related to a larger expansion of carbon-rich, southern-sourced waters into the Northern Hemisphere in MIS 6, providing a larger carbon reservoir that requires more time to be depleted.</p< Environmental pollution Environmental protection Environmental sciences J. Shin verfasserin aut C. Nehrbass-Ahles verfasserin aut C. Nehrbass-Ahles verfasserin aut R. Grilli verfasserin aut J. Chowdhry Beeman verfasserin aut F. Parrenin verfasserin aut G. Teste verfasserin aut A. Landais verfasserin aut L. Schmidely verfasserin aut L. Silva verfasserin aut J. Schmitt verfasserin aut B. Bereiter verfasserin aut B. Bereiter verfasserin aut B. Bereiter verfasserin aut T. F. Stocker verfasserin aut H. Fischer verfasserin aut J. Chappellaz verfasserin aut In Climate of the Past Copernicus Publications, 2005 16(2020), Seite 2203-2219 (DE-627)505943697 (DE-600)2217985-9 18149332 nnns volume:16 year:2020 pages:2203-2219 https://doi.org/10.5194/cp-16-2203-2020 kostenfrei https://doaj.org/article/379f5fb57a4a421d924853aa240c4af9 kostenfrei https://cp.copernicus.org/articles/16/2203/2020/cp-16-2203-2020.pdf kostenfrei https://doaj.org/toc/1814-9324 Journal toc kostenfrei https://doaj.org/toc/1814-9332 Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_95 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_213 GBV_ILN_230 GBV_ILN_267 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_2014 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_4012 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4249 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4338 GBV_ILN_4367 GBV_ILN_4700 AR 16 2020 2203-2219
allfieldsGer	10.5194/cp-16-2203-2020 doi (DE-627)DOAJ002800063 (DE-599)DOAJ379f5fb57a4a421d924853aa240c4af9 DE-627 ger DE-627 rakwb eng TD172-193.5 TD169-171.8 GE1-350 J. Shin verfasserin aut Millennial-scale atmospheric CO<sub<2</sub< variations during the Marine Isotope Stage 6 period (190–135 ka) 2020 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier <p<Using new and previously published <span class="inline-formula"<CO<sub<2</sub<</span< data from the EPICA Dome C ice core (EDC), we reconstruct a new high-resolution record of atmospheric <span class="inline-formula"<CO<sub<2</sub<</span< during Marine Isotope Stage (MIS) 6 (190 to 135 ka) the penultimate glacial period. Similar to the last glacial cycle, where high-resolution data already exists, our record shows that during longer North Atlantic (NA) stadials, millennial <span class="inline-formula"<CO<sub<2</sub<</span< variations during MIS 6 are clearly coincident with the bipolar seesaw signal in the Antarctic temperature record. However, during one short stadial in the NA, atmospheric <span class="inline-formula"<CO<sub<2</sub<</span< variation is small (<span class="inline-formula"<∼5</span< ppm) and the relationship between temperature variations in EDC and atmospheric <span class="inline-formula"<CO<sub<2</sub<</span< is unclear. The magnitude of <span class="inline-formula"<CO<sub<2</sub<</span< increase during Carbon Dioxide Maxima (CDM) is closely related to the NA stadial duration in both MIS 6 and MIS 3 (60–27 ka). This observation implies that during the last two glacials the overall bipolar seesaw coupling of climate and atmospheric <span class="inline-formula"<CO<sub<2</sub<</span< operated similarly. In addition, similar to the last glacial period, CDM during the earliest MIS 6 show different lags with respect to the corresponding abrupt <span class="inline-formula"<CH<sub<4</sub<</span< rises, the latter reflecting rapid warming in the Northern Hemisphere (NH). During MIS 6i at around <span class="inline-formula"<181.5±</span<0.3 ka, CDM 6i lags the abrupt warming in the NH by only <span class="inline-formula"<240±</span<320 years. However, during CDM 6iv (<span class="inline-formula"<171.1±</span<0.2 ka) and CDM 6iii (<span class="inline-formula"<175.4±</span<0.4 ka) the lag is much longer: <span class="inline-formula"<1290±</span<540 years on average. We speculate that the size of this lag may be related to a larger expansion of carbon-rich, southern-sourced waters into the Northern Hemisphere in MIS 6, providing a larger carbon reservoir that requires more time to be depleted.</p< Environmental pollution Environmental protection Environmental sciences J. Shin verfasserin aut C. Nehrbass-Ahles verfasserin aut C. Nehrbass-Ahles verfasserin aut R. Grilli verfasserin aut J. Chowdhry Beeman verfasserin aut F. Parrenin verfasserin aut G. Teste verfasserin aut A. Landais verfasserin aut L. Schmidely verfasserin aut L. Silva verfasserin aut J. Schmitt verfasserin aut B. Bereiter verfasserin aut B. Bereiter verfasserin aut B. Bereiter verfasserin aut T. F. Stocker verfasserin aut H. Fischer verfasserin aut J. Chappellaz verfasserin aut In Climate of the Past Copernicus Publications, 2005 16(2020), Seite 2203-2219 (DE-627)505943697 (DE-600)2217985-9 18149332 nnns volume:16 year:2020 pages:2203-2219 https://doi.org/10.5194/cp-16-2203-2020 kostenfrei https://doaj.org/article/379f5fb57a4a421d924853aa240c4af9 kostenfrei https://cp.copernicus.org/articles/16/2203/2020/cp-16-2203-2020.pdf kostenfrei https://doaj.org/toc/1814-9324 Journal toc kostenfrei https://doaj.org/toc/1814-9332 Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_95 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_213 GBV_ILN_230 GBV_ILN_267 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_2014 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_4012 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4249 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4338 GBV_ILN_4367 GBV_ILN_4700 AR 16 2020 2203-2219
allfieldsSound	10.5194/cp-16-2203-2020 doi (DE-627)DOAJ002800063 (DE-599)DOAJ379f5fb57a4a421d924853aa240c4af9 DE-627 ger DE-627 rakwb eng TD172-193.5 TD169-171.8 GE1-350 J. Shin verfasserin aut Millennial-scale atmospheric CO<sub<2</sub< variations during the Marine Isotope Stage 6 period (190–135 ka) 2020 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier <p<Using new and previously published <span class="inline-formula"<CO<sub<2</sub<</span< data from the EPICA Dome C ice core (EDC), we reconstruct a new high-resolution record of atmospheric <span class="inline-formula"<CO<sub<2</sub<</span< during Marine Isotope Stage (MIS) 6 (190 to 135 ka) the penultimate glacial period. Similar to the last glacial cycle, where high-resolution data already exists, our record shows that during longer North Atlantic (NA) stadials, millennial <span class="inline-formula"<CO<sub<2</sub<</span< variations during MIS 6 are clearly coincident with the bipolar seesaw signal in the Antarctic temperature record. However, during one short stadial in the NA, atmospheric <span class="inline-formula"<CO<sub<2</sub<</span< variation is small (<span class="inline-formula"<∼5</span< ppm) and the relationship between temperature variations in EDC and atmospheric <span class="inline-formula"<CO<sub<2</sub<</span< is unclear. The magnitude of <span class="inline-formula"<CO<sub<2</sub<</span< increase during Carbon Dioxide Maxima (CDM) is closely related to the NA stadial duration in both MIS 6 and MIS 3 (60–27 ka). This observation implies that during the last two glacials the overall bipolar seesaw coupling of climate and atmospheric <span class="inline-formula"<CO<sub<2</sub<</span< operated similarly. In addition, similar to the last glacial period, CDM during the earliest MIS 6 show different lags with respect to the corresponding abrupt <span class="inline-formula"<CH<sub<4</sub<</span< rises, the latter reflecting rapid warming in the Northern Hemisphere (NH). During MIS 6i at around <span class="inline-formula"<181.5±</span<0.3 ka, CDM 6i lags the abrupt warming in the NH by only <span class="inline-formula"<240±</span<320 years. However, during CDM 6iv (<span class="inline-formula"<171.1±</span<0.2 ka) and CDM 6iii (<span class="inline-formula"<175.4±</span<0.4 ka) the lag is much longer: <span class="inline-formula"<1290±</span<540 years on average. We speculate that the size of this lag may be related to a larger expansion of carbon-rich, southern-sourced waters into the Northern Hemisphere in MIS 6, providing a larger carbon reservoir that requires more time to be depleted.</p< Environmental pollution Environmental protection Environmental sciences J. Shin verfasserin aut C. Nehrbass-Ahles verfasserin aut C. Nehrbass-Ahles verfasserin aut R. Grilli verfasserin aut J. Chowdhry Beeman verfasserin aut F. Parrenin verfasserin aut G. Teste verfasserin aut A. Landais verfasserin aut L. Schmidely verfasserin aut L. Silva verfasserin aut J. Schmitt verfasserin aut B. Bereiter verfasserin aut B. Bereiter verfasserin aut B. Bereiter verfasserin aut T. F. Stocker verfasserin aut H. Fischer verfasserin aut J. Chappellaz verfasserin aut In Climate of the Past Copernicus Publications, 2005 16(2020), Seite 2203-2219 (DE-627)505943697 (DE-600)2217985-9 18149332 nnns volume:16 year:2020 pages:2203-2219 https://doi.org/10.5194/cp-16-2203-2020 kostenfrei https://doaj.org/article/379f5fb57a4a421d924853aa240c4af9 kostenfrei https://cp.copernicus.org/articles/16/2203/2020/cp-16-2203-2020.pdf kostenfrei https://doaj.org/toc/1814-9324 Journal toc kostenfrei https://doaj.org/toc/1814-9332 Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_95 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_213 GBV_ILN_230 GBV_ILN_267 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_2014 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_4012 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4249 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4338 GBV_ILN_4367 GBV_ILN_4700 AR 16 2020 2203-2219
language	English
source	In Climate of the Past 16(2020), Seite 2203-2219 volume:16 year:2020 pages:2203-2219
sourceStr	In Climate of the Past 16(2020), Seite 2203-2219 volume:16 year:2020 pages:2203-2219
format_phy_str_mv	Article
institution	findex.gbv.de
topic_facet	Environmental pollution Environmental protection Environmental sciences
isfreeaccess_bool	true
container_title	Climate of the Past
authorswithroles_txt_mv	J. Shin @@aut@@ C. Nehrbass-Ahles @@aut@@ R. Grilli @@aut@@ J. Chowdhry Beeman @@aut@@ F. Parrenin @@aut@@ G. Teste @@aut@@ A. Landais @@aut@@ L. Schmidely @@aut@@ L. Silva @@aut@@ J. Schmitt @@aut@@ B. Bereiter @@aut@@ T. F. Stocker @@aut@@ H. Fischer @@aut@@ J. Chappellaz @@aut@@
publishDateDaySort_date	2020-01-01T00:00:00Z
hierarchy_top_id	505943697
id	DOAJ002800063
language_de	englisch
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Shin</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">Millennial-scale atmospheric CO<sub<2</sub< variations during the Marine Isotope Stage 6 period (190–135 ka)</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">2020</subfield></datafield><datafield tag="336" ind1=" " ind2=" "><subfield code="a">Text</subfield><subfield code="b">txt</subfield><subfield code="2">rdacontent</subfield></datafield><datafield tag="337" ind1=" " ind2=" "><subfield code="a">Computermedien</subfield><subfield code="b">c</subfield><subfield code="2">rdamedia</subfield></datafield><datafield tag="338" ind1=" " ind2=" "><subfield code="a">Online-Ressource</subfield><subfield code="b">cr</subfield><subfield code="2">rdacarrier</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a"><p<Using new and previously published <span class="inline-formula"<CO<sub<2</sub<</span< data from the EPICA Dome C ice core (EDC), we reconstruct a new high-resolution record of atmospheric <span class="inline-formula"<CO<sub<2</sub<</span< during Marine Isotope Stage (MIS) 6 (190 to 135 ka) the penultimate glacial period. Similar to the last glacial cycle, where high-resolution data already exists, our record shows that during longer North Atlantic (NA) stadials, millennial <span class="inline-formula"<CO<sub<2</sub<</span< variations during MIS 6 are clearly coincident with the bipolar seesaw signal in the Antarctic temperature record. However, during one short stadial in the NA, atmospheric <span class="inline-formula"<CO<sub<2</sub<</span< variation is small (<span class="inline-formula"<∼5</span< ppm) and the relationship between temperature variations in EDC and atmospheric <span class="inline-formula"<CO<sub<2</sub<</span< is unclear. The magnitude of <span class="inline-formula"<CO<sub<2</sub<</span< increase during Carbon Dioxide Maxima (CDM) is closely related to the NA stadial duration in both MIS 6 and MIS 3 (60–27 ka). This observation implies that during the last two glacials the overall bipolar seesaw coupling of climate and atmospheric <span class="inline-formula"<CO<sub<2</sub<</span< operated similarly. In addition, similar to the last glacial period, CDM during the earliest MIS 6 show different lags with respect to the corresponding abrupt <span class="inline-formula"<CH<sub<4</sub<</span< rises, the latter reflecting rapid warming in the Northern Hemisphere (NH). During MIS 6i at around <span class="inline-formula"<181.5±</span<0.3 ka, CDM 6i lags the abrupt warming in the NH by only <span class="inline-formula"<240±</span<320 years. However, during CDM 6iv (<span class="inline-formula"<171.1±</span<0.2 ka) and CDM 6iii (<span class="inline-formula"<175.4±</span<0.4 ka) the lag is much longer: <span class="inline-formula"<1290±</span<540 years on average. 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callnumber-first	T - Technology
author	J. Shin
spellingShingle	J. Shin misc TD172-193.5 misc TD169-171.8 misc GE1-350 misc Environmental pollution misc Environmental protection misc Environmental sciences Millennial-scale atmospheric CO<sub<2</sub< variations during the Marine Isotope Stage 6 period (190–135 ka)
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topic_title	TD172-193.5 TD169-171.8 GE1-350 Millennial-scale atmospheric CO<sub<2</sub< variations during the Marine Isotope Stage 6 period (190–135 ka)
topic	misc TD172-193.5 misc TD169-171.8 misc GE1-350 misc Environmental pollution misc Environmental protection misc Environmental sciences
topic_unstemmed	misc TD172-193.5 misc TD169-171.8 misc GE1-350 misc Environmental pollution misc Environmental protection misc Environmental sciences
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title	Millennial-scale atmospheric CO<sub<2</sub< variations during the Marine Isotope Stage 6 period (190–135 ka)
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title_full	Millennial-scale atmospheric CO<sub<2</sub< variations during the Marine Isotope Stage 6 period (190–135 ka)
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author_browse	J. Shin C. Nehrbass-Ahles R. Grilli J. Chowdhry Beeman F. Parrenin G. Teste A. Landais L. Schmidely L. Silva J. Schmitt B. Bereiter T. F. Stocker H. Fischer J. Chappellaz
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title_sort	millennial-scale atmospheric co<sub<2</sub< variations during the marine isotope stage 6 period (190–135 ka)
callnumber	TD172-193.5
title_auth	Millennial-scale atmospheric CO<sub<2</sub< variations during the Marine Isotope Stage 6 period (190–135 ka)
abstract	<p<Using new and previously published <span class="inline-formula"<CO<sub<2</sub<</span< data from the EPICA Dome C ice core (EDC), we reconstruct a new high-resolution record of atmospheric <span class="inline-formula"<CO<sub<2</sub<</span< during Marine Isotope Stage (MIS) 6 (190 to 135 ka) the penultimate glacial period. Similar to the last glacial cycle, where high-resolution data already exists, our record shows that during longer North Atlantic (NA) stadials, millennial <span class="inline-formula"<CO<sub<2</sub<</span< variations during MIS 6 are clearly coincident with the bipolar seesaw signal in the Antarctic temperature record. However, during one short stadial in the NA, atmospheric <span class="inline-formula"<CO<sub<2</sub<</span< variation is small (<span class="inline-formula"<∼5</span< ppm) and the relationship between temperature variations in EDC and atmospheric <span class="inline-formula"<CO<sub<2</sub<</span< is unclear. The magnitude of <span class="inline-formula"<CO<sub<2</sub<</span< increase during Carbon Dioxide Maxima (CDM) is closely related to the NA stadial duration in both MIS 6 and MIS 3 (60–27 ka). This observation implies that during the last two glacials the overall bipolar seesaw coupling of climate and atmospheric <span class="inline-formula"<CO<sub<2</sub<</span< operated similarly. In addition, similar to the last glacial period, CDM during the earliest MIS 6 show different lags with respect to the corresponding abrupt <span class="inline-formula"<CH<sub<4</sub<</span< rises, the latter reflecting rapid warming in the Northern Hemisphere (NH). During MIS 6i at around <span class="inline-formula"<181.5±</span<0.3 ka, CDM 6i lags the abrupt warming in the NH by only <span class="inline-formula"<240±</span<320 years. However, during CDM 6iv (<span class="inline-formula"<171.1±</span<0.2 ka) and CDM 6iii (<span class="inline-formula"<175.4±</span<0.4 ka) the lag is much longer: <span class="inline-formula"<1290±</span<540 years on average. We speculate that the size of this lag may be related to a larger expansion of carbon-rich, southern-sourced waters into the Northern Hemisphere in MIS 6, providing a larger carbon reservoir that requires more time to be depleted.</p<
abstractGer	<p<Using new and previously published <span class="inline-formula"<CO<sub<2</sub<</span< data from the EPICA Dome C ice core (EDC), we reconstruct a new high-resolution record of atmospheric <span class="inline-formula"<CO<sub<2</sub<</span< during Marine Isotope Stage (MIS) 6 (190 to 135 ka) the penultimate glacial period. Similar to the last glacial cycle, where high-resolution data already exists, our record shows that during longer North Atlantic (NA) stadials, millennial <span class="inline-formula"<CO<sub<2</sub<</span< variations during MIS 6 are clearly coincident with the bipolar seesaw signal in the Antarctic temperature record. However, during one short stadial in the NA, atmospheric <span class="inline-formula"<CO<sub<2</sub<</span< variation is small (<span class="inline-formula"<∼5</span< ppm) and the relationship between temperature variations in EDC and atmospheric <span class="inline-formula"<CO<sub<2</sub<</span< is unclear. The magnitude of <span class="inline-formula"<CO<sub<2</sub<</span< increase during Carbon Dioxide Maxima (CDM) is closely related to the NA stadial duration in both MIS 6 and MIS 3 (60–27 ka). This observation implies that during the last two glacials the overall bipolar seesaw coupling of climate and atmospheric <span class="inline-formula"<CO<sub<2</sub<</span< operated similarly. In addition, similar to the last glacial period, CDM during the earliest MIS 6 show different lags with respect to the corresponding abrupt <span class="inline-formula"<CH<sub<4</sub<</span< rises, the latter reflecting rapid warming in the Northern Hemisphere (NH). During MIS 6i at around <span class="inline-formula"<181.5±</span<0.3 ka, CDM 6i lags the abrupt warming in the NH by only <span class="inline-formula"<240±</span<320 years. However, during CDM 6iv (<span class="inline-formula"<171.1±</span<0.2 ka) and CDM 6iii (<span class="inline-formula"<175.4±</span<0.4 ka) the lag is much longer: <span class="inline-formula"<1290±</span<540 years on average. We speculate that the size of this lag may be related to a larger expansion of carbon-rich, southern-sourced waters into the Northern Hemisphere in MIS 6, providing a larger carbon reservoir that requires more time to be depleted.</p<
abstract_unstemmed	<p<Using new and previously published <span class="inline-formula"<CO<sub<2</sub<</span< data from the EPICA Dome C ice core (EDC), we reconstruct a new high-resolution record of atmospheric <span class="inline-formula"<CO<sub<2</sub<</span< during Marine Isotope Stage (MIS) 6 (190 to 135 ka) the penultimate glacial period. Similar to the last glacial cycle, where high-resolution data already exists, our record shows that during longer North Atlantic (NA) stadials, millennial <span class="inline-formula"<CO<sub<2</sub<</span< variations during MIS 6 are clearly coincident with the bipolar seesaw signal in the Antarctic temperature record. However, during one short stadial in the NA, atmospheric <span class="inline-formula"<CO<sub<2</sub<</span< variation is small (<span class="inline-formula"<∼5</span< ppm) and the relationship between temperature variations in EDC and atmospheric <span class="inline-formula"<CO<sub<2</sub<</span< is unclear. The magnitude of <span class="inline-formula"<CO<sub<2</sub<</span< increase during Carbon Dioxide Maxima (CDM) is closely related to the NA stadial duration in both MIS 6 and MIS 3 (60–27 ka). This observation implies that during the last two glacials the overall bipolar seesaw coupling of climate and atmospheric <span class="inline-formula"<CO<sub<2</sub<</span< operated similarly. In addition, similar to the last glacial period, CDM during the earliest MIS 6 show different lags with respect to the corresponding abrupt <span class="inline-formula"<CH<sub<4</sub<</span< rises, the latter reflecting rapid warming in the Northern Hemisphere (NH). During MIS 6i at around <span class="inline-formula"<181.5±</span<0.3 ka, CDM 6i lags the abrupt warming in the NH by only <span class="inline-formula"<240±</span<320 years. However, during CDM 6iv (<span class="inline-formula"<171.1±</span<0.2 ka) and CDM 6iii (<span class="inline-formula"<175.4±</span<0.4 ka) the lag is much longer: <span class="inline-formula"<1290±</span<540 years on average. We speculate that the size of this lag may be related to a larger expansion of carbon-rich, southern-sourced waters into the Northern Hemisphere in MIS 6, providing a larger carbon reservoir that requires more time to be depleted.</p<
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title_short	Millennial-scale atmospheric CO<sub<2</sub< variations during the Marine Isotope Stage 6 period (190–135 ka)
url	https://doi.org/10.5194/cp-16-2203-2020 https://doaj.org/article/379f5fb57a4a421d924853aa240c4af9 https://cp.copernicus.org/articles/16/2203/2020/cp-16-2203-2020.pdf https://doaj.org/toc/1814-9324 https://doaj.org/toc/1814-9332
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Shin</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">Millennial-scale atmospheric CO<sub<2</sub< variations during the Marine Isotope Stage 6 period (190–135 ka)</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">2020</subfield></datafield><datafield tag="336" ind1=" " ind2=" "><subfield code="a">Text</subfield><subfield code="b">txt</subfield><subfield code="2">rdacontent</subfield></datafield><datafield tag="337" ind1=" " ind2=" "><subfield code="a">Computermedien</subfield><subfield code="b">c</subfield><subfield code="2">rdamedia</subfield></datafield><datafield tag="338" ind1=" " ind2=" "><subfield code="a">Online-Ressource</subfield><subfield code="b">cr</subfield><subfield code="2">rdacarrier</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a"><p<Using new and previously published <span class="inline-formula"<CO<sub<2</sub<</span< data from the EPICA Dome C ice core (EDC), we reconstruct a new high-resolution record of atmospheric <span class="inline-formula"<CO<sub<2</sub<</span< during Marine Isotope Stage (MIS) 6 (190 to 135 ka) the penultimate glacial period. Similar to the last glacial cycle, where high-resolution data already exists, our record shows that during longer North Atlantic (NA) stadials, millennial <span class="inline-formula"<CO<sub<2</sub<</span< variations during MIS 6 are clearly coincident with the bipolar seesaw signal in the Antarctic temperature record. However, during one short stadial in the NA, atmospheric <span class="inline-formula"<CO<sub<2</sub<</span< variation is small (<span class="inline-formula"<∼5</span< ppm) and the relationship between temperature variations in EDC and atmospheric <span class="inline-formula"<CO<sub<2</sub<</span< is unclear. The magnitude of <span class="inline-formula"<CO<sub<2</sub<</span< increase during Carbon Dioxide Maxima (CDM) is closely related to the NA stadial duration in both MIS 6 and MIS 3 (60–27 ka). This observation implies that during the last two glacials the overall bipolar seesaw coupling of climate and atmospheric <span class="inline-formula"<CO<sub<2</sub<</span< operated similarly. In addition, similar to the last glacial period, CDM during the earliest MIS 6 show different lags with respect to the corresponding abrupt <span class="inline-formula"<CH<sub<4</sub<</span< rises, the latter reflecting rapid warming in the Northern Hemisphere (NH). During MIS 6i at around <span class="inline-formula"<181.5±</span<0.3 ka, CDM 6i lags the abrupt warming in the NH by only <span class="inline-formula"<240±</span<320 years. However, during CDM 6iv (<span class="inline-formula"<171.1±</span<0.2 ka) and CDM 6iii (<span class="inline-formula"<175.4±</span<0.4 ka) the lag is much longer: <span class="inline-formula"<1290±</span<540 years on average. We speculate that the size of this lag may be related to a larger expansion of carbon-rich, southern-sourced waters into the Northern Hemisphere in MIS 6, providing a larger carbon reservoir that requires more time to be depleted.</p<</subfield></datafield><datafield tag="653" ind1=" " ind2="0"><subfield code="a">Environmental pollution</subfield></datafield><datafield tag="653" ind1=" " ind2="0"><subfield code="a">Environmental protection</subfield></datafield><datafield tag="653" ind1=" " ind2="0"><subfield code="a">Environmental sciences</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">J. Shin</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">C. Nehrbass-Ahles</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">C. Nehrbass-Ahles</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">R. Grilli</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">J. Chowdhry Beeman</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">F. Parrenin</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">G. Teste</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">A. Landais</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">L. Schmidely</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">L. Silva</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">J. Schmitt</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">B. Bereiter</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">B. Bereiter</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">B. 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Millennial-scale atmospheric CO<sub<2</sub< variations during the Marine Isotope Stage 6 period (190–135 ka)

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