Triple oxygen isotopes of cherts : implications for the δ18O and temperatures of early oceans

The temperature of Earth’s earliest oceans, in which life may have first originated, remains a controversial issue in Earth science. Over the last 50 years, many studies have attempted to apply the temperature dependent fractionation of oxygen isotopes 18O/16O to ancient marine chemical sediments in...
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Autor*in:	Sengupta, Sukanya [verfasserIn] Pack, Andreas [akademischer betreuerIn] Pack, Andreas [gutachterIn] Hoefs, Jochen [gutachterIn]
Hochschulschrift:	Dissertation ; Georg-August-Universität Göttingen ; 2016

Format:	E-Book
Sprache:	Englisch

Erschienen:	Göttingen: 2016

Formangabe:	Hochschulschrift

Umfang:	1 Online-Ressource ; Illustrationen, Diagramme

Weitere Ausgabe:	Erscheint auch als Druck-Ausgabe Sengupta, Sukanya: Triple oxygen isotopes of cherts : implications for the δ18O and temperatures of early oceans - Göttingen, 2016

Links:	Link aufrufen Volltext Volltext Volltext Volltext

DOI / URN:	urn:nbn:de:gbv:7-11858/00-1735-0000-0023-3E7F-6-8

Katalog-ID:	890545316

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Indexfelder

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matchkey_str	senguptasukanyapackandreaspackandreashoe:2016----:rpexgnstpsfhrsmlctosote8adep
hierarchy_sort_str	2016
publishDate	2016
allfields	17,O07 dnb 1135778345 DE-101 urn:nbn:de:gbv:7-11858/00-1735-0000-0023-3E7F-6-8 urn (DE-627)890545316 (DE-576)9890545314 (DE-599)GBV890545316 DE-627 ger DE-627 rda eng XA-DE-NI 910 550 SEPA 22 550 DE-101 Sengupta, Sukanya verfasserin aut Triple oxygen isotopes of cherts : implications for the δ18O and temperatures of early oceans vorgelegt von Sukanya Sengupta Göttingen 2016 1 Online-Ressource Illustrationen, Diagramme Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Dissertation Georg-August-Universität Göttingen 2016 The temperature of Earth’s earliest oceans, in which life may have first originated, remains a controversial issue in Earth science. Over the last 50 years, many studies have attempted to apply the temperature dependent fractionation of oxygen isotopes 18O/16O to ancient marine chemical sediments in order to infer the temperatures of the ancient oceans. The δ18O composition of marine chemical sediments progressively decrease with increasing age leading to the suggestions that either the Precambrian oceans were also strongly depleted in 18O (~-13‰) but had the same temperature as modern day,... Langzeitarchivierung gewährleistet pdager Hochschulschrift (DE-588)4113937-9 (DE-627)105825778 (DE-576)209480580 gnd-content Pack, Andreas akademischer betreuerin dgs Pack, Andreas gutachterin oth Hoefs, Jochen gutachterin oth Erscheint auch als Druck-Ausgabe Sengupta, Sukanya Triple oxygen isotopes of cherts : implications for the δ18O and temperatures of early oceans Göttingen, 2016 218, vi Seiten (DE-627)890545324 http://hdl.handle.net/11858/00-1735-0000-0023-3E7F-6 Resolving-System Volltext kostenfrei Volltext http://nbn-resolving.org/urn:nbn:de:gbv:7-11858/00-1735-0000-0023-3E7F-6-8 Resolving-System Volltext kostenfrei Volltext http://nbn-resolving.de/urn:nbn:de:gbv:7-11858/00-1735-0000-0023-3E7F-6-8 2017-07-05 Resolving-System Volltext http://d-nb.info/1135778345/34 2017-07-05 Langzeitarchivierung Nationalbibliothek Volltext GBV-ODiss GBV_ILN_20 ISIL_DE-84 SYSFLAG_1 GBV_KXP SSG-OPC-GEO SSG-OPC-GGO GBV_ILN_21 ISIL_DE-46 GBV_ILN_22 ISIL_DE-18 GBV_ILN_23 ISIL_DE-830 GBV_ILN_30 ISIL_DE-104 GBV_ILN_40 ISIL_DE-7 GBV_ILN_60 ISIL_DE-705 GBV_ILN_63 ISIL_DE-Wim2 GBV_ILN_70 ISIL_DE-89 GBV_ILN_105 ISIL_DE-841 GBV_ILN_110 ISIL_DE-Luen4 GBV_ILN_132 ISIL_DE-959 GBV_ILN_151 ISIL_DE-546 GBV_ILN_161 ISIL_DE-960 GBV_ILN_293 ISIL_DE-960-3 GBV_ILN_370 ISIL_DE-1373 GBV_ILN_2403 ISIL_DE-LFER BO 045F 910 20 01 0084 169971617X x 06-07-17 21 01 0046 1699729204 z 06-07-17 22 01 0018 1699742170 SUBolrd xu 06-07-17 23 01 0830 1699754683 olr-d x 06-07-17 30 01 0104 1699762511 z 06-07-17 40 01 0007 169530196X ediss xsn 20-06-17 60 01 0705 1699782547 OLRD z 06-07-17 63 01 3401 1699795169 ORD x 06-07-17 70 01 0089 1699801118 zdo 06-07-17 105 01 0841 1699869553 z 06-07-17 110 01 3110 1699809844 x 06-07-17 132 01 0959 1699818746 OLR-DISS x 06-07-17 151 01 0546 3583672860 OLR-ODISS z 31-01-20 161 01 0960 1699832110 ORD x 06-07-17 293 01 3293 1699859221 ORD xf 06-07-17 370 01 4370 1699866538 x 06-07-17 2403 01 DE-LFER 3475889536 00 --%%-- --%%-- n --%%-- l01 15-05-19 20 01 0084 http://nbn-resolving.de/urn:nbn:de:gbv:7-11858/00-1735-0000-0023-3E7F-6-8 21 01 0046 http://nbn-resolving.de/urn:nbn:de:gbv:7-11858/00-1735-0000-0023-3E7F-6-8 22 01 0018 http://nbn-resolving.de/urn:nbn:de:gbv:7-11858/00-1735-0000-0023-3E7F-6-8 23 01 0830 http://nbn-resolving.de/urn:nbn:de:gbv:7-11858/00-1735-0000-0023-3E7F-6-8 30 01 0104 http://nbn-resolving.de/urn:nbn:de:gbv:7-11858/00-1735-0000-0023-3E7F-6-8 40 01 0007 Volltext http://hdl.handle.net/11858/00-1735-0000-0023-3E7F-6 LF 60 01 0705 http://nbn-resolving.de/urn:nbn:de:gbv:7-11858/00-1735-0000-0023-3E7F-6-8 63 01 3401 E-Book http://nbn-resolving.de/urn:nbn:de:gbv:7-11858/00-1735-0000-0023-3E7F-6-8 LF 70 01 0089 http://nbn-resolving.de/urn:nbn:de:gbv:7-11858/00-1735-0000-0023-3E7F-6-8 105 01 0841 http://nbn-resolving.de/urn:nbn:de:gbv:7-11858/00-1735-0000-0023-3E7F-6-8 110 01 3110 http://nbn-resolving.de/urn:nbn:de:gbv:7-11858/00-1735-0000-0023-3E7F-6-8 132 01 0959 http://nbn-resolving.de/urn:nbn:de:gbv:7-11858/00-1735-0000-0023-3E7F-6-8 151 01 0546 Volltext http://nbn-resolving.de/urn:nbn:de:gbv:7-11858/00-1735-0000-0023-3E7F-6-8 161 01 0960 http://nbn-resolving.de/urn:nbn:de:gbv:7-11858/00-1735-0000-0023-3E7F-6-8 293 01 3293 http://nbn-resolving.de/urn:nbn:de:gbv:7-11858/00-1735-0000-0023-3E7F-6-8 370 01 4370 http://nbn-resolving.de/urn:nbn:de:gbv:7-11858/00-1735-0000-0023-3E7F-6-8 2403 01 DE-LFER http://nbn-resolving.org/urn:nbn:de:gbv:7-11858/00-1735-0000-0023-3E7F-6-8 40 00 DE-7 00 (DE-627)625047842 VBO 000 Isotopengeologie 60 01 0705 10 ho 20 01 0084 OLRD 110 01 3110 OLRD 370 01 4370 OLRD 22 01 0018 SUBolrd 23 01 0830 olr-d 40 01 0007 ediss 60 01 0705 OLRD 63 01 3401 ORD 132 01 0959 OLR-DISS 151 01 0546 OLR-ODISS 161 01 0960 ORD 293 01 3293 ORD 23 01 0830 2017-07-06:08:49:20
spelling	17,O07 dnb 1135778345 DE-101 urn:nbn:de:gbv:7-11858/00-1735-0000-0023-3E7F-6-8 urn (DE-627)890545316 (DE-576)9890545314 (DE-599)GBV890545316 DE-627 ger DE-627 rda eng XA-DE-NI 910 550 SEPA 22 550 DE-101 Sengupta, Sukanya verfasserin aut Triple oxygen isotopes of cherts : implications for the δ18O and temperatures of early oceans vorgelegt von Sukanya Sengupta Göttingen 2016 1 Online-Ressource Illustrationen, Diagramme Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Dissertation Georg-August-Universität Göttingen 2016 The temperature of Earth’s earliest oceans, in which life may have first originated, remains a controversial issue in Earth science. Over the last 50 years, many studies have attempted to apply the temperature dependent fractionation of oxygen isotopes 18O/16O to ancient marine chemical sediments in order to infer the temperatures of the ancient oceans. The δ18O composition of marine chemical sediments progressively decrease with increasing age leading to the suggestions that either the Precambrian oceans were also strongly depleted in 18O (~-13‰) but had the same temperature as modern day,... Langzeitarchivierung gewährleistet pdager Hochschulschrift (DE-588)4113937-9 (DE-627)105825778 (DE-576)209480580 gnd-content Pack, Andreas akademischer betreuerin dgs Pack, Andreas gutachterin oth Hoefs, Jochen gutachterin oth Erscheint auch als Druck-Ausgabe Sengupta, Sukanya Triple oxygen isotopes of cherts : implications for the δ18O and temperatures of early oceans Göttingen, 2016 218, vi Seiten (DE-627)890545324 http://hdl.handle.net/11858/00-1735-0000-0023-3E7F-6 Resolving-System Volltext kostenfrei Volltext http://nbn-resolving.org/urn:nbn:de:gbv:7-11858/00-1735-0000-0023-3E7F-6-8 Resolving-System Volltext kostenfrei Volltext http://nbn-resolving.de/urn:nbn:de:gbv:7-11858/00-1735-0000-0023-3E7F-6-8 2017-07-05 Resolving-System Volltext http://d-nb.info/1135778345/34 2017-07-05 Langzeitarchivierung Nationalbibliothek Volltext GBV-ODiss GBV_ILN_20 ISIL_DE-84 SYSFLAG_1 GBV_KXP SSG-OPC-GEO SSG-OPC-GGO GBV_ILN_21 ISIL_DE-46 GBV_ILN_22 ISIL_DE-18 GBV_ILN_23 ISIL_DE-830 GBV_ILN_30 ISIL_DE-104 GBV_ILN_40 ISIL_DE-7 GBV_ILN_60 ISIL_DE-705 GBV_ILN_63 ISIL_DE-Wim2 GBV_ILN_70 ISIL_DE-89 GBV_ILN_105 ISIL_DE-841 GBV_ILN_110 ISIL_DE-Luen4 GBV_ILN_132 ISIL_DE-959 GBV_ILN_151 ISIL_DE-546 GBV_ILN_161 ISIL_DE-960 GBV_ILN_293 ISIL_DE-960-3 GBV_ILN_370 ISIL_DE-1373 GBV_ILN_2403 ISIL_DE-LFER BO 045F 910 20 01 0084 169971617X x 06-07-17 21 01 0046 1699729204 z 06-07-17 22 01 0018 1699742170 SUBolrd xu 06-07-17 23 01 0830 1699754683 olr-d x 06-07-17 30 01 0104 1699762511 z 06-07-17 40 01 0007 169530196X ediss xsn 20-06-17 60 01 0705 1699782547 OLRD z 06-07-17 63 01 3401 1699795169 ORD x 06-07-17 70 01 0089 1699801118 zdo 06-07-17 105 01 0841 1699869553 z 06-07-17 110 01 3110 1699809844 x 06-07-17 132 01 0959 1699818746 OLR-DISS x 06-07-17 151 01 0546 3583672860 OLR-ODISS z 31-01-20 161 01 0960 1699832110 ORD x 06-07-17 293 01 3293 1699859221 ORD xf 06-07-17 370 01 4370 1699866538 x 06-07-17 2403 01 DE-LFER 3475889536 00 --%%-- --%%-- n --%%-- l01 15-05-19 20 01 0084 http://nbn-resolving.de/urn:nbn:de:gbv:7-11858/00-1735-0000-0023-3E7F-6-8 21 01 0046 http://nbn-resolving.de/urn:nbn:de:gbv:7-11858/00-1735-0000-0023-3E7F-6-8 22 01 0018 http://nbn-resolving.de/urn:nbn:de:gbv:7-11858/00-1735-0000-0023-3E7F-6-8 23 01 0830 http://nbn-resolving.de/urn:nbn:de:gbv:7-11858/00-1735-0000-0023-3E7F-6-8 30 01 0104 http://nbn-resolving.de/urn:nbn:de:gbv:7-11858/00-1735-0000-0023-3E7F-6-8 40 01 0007 Volltext http://hdl.handle.net/11858/00-1735-0000-0023-3E7F-6 LF 60 01 0705 http://nbn-resolving.de/urn:nbn:de:gbv:7-11858/00-1735-0000-0023-3E7F-6-8 63 01 3401 E-Book http://nbn-resolving.de/urn:nbn:de:gbv:7-11858/00-1735-0000-0023-3E7F-6-8 LF 70 01 0089 http://nbn-resolving.de/urn:nbn:de:gbv:7-11858/00-1735-0000-0023-3E7F-6-8 105 01 0841 http://nbn-resolving.de/urn:nbn:de:gbv:7-11858/00-1735-0000-0023-3E7F-6-8 110 01 3110 http://nbn-resolving.de/urn:nbn:de:gbv:7-11858/00-1735-0000-0023-3E7F-6-8 132 01 0959 http://nbn-resolving.de/urn:nbn:de:gbv:7-11858/00-1735-0000-0023-3E7F-6-8 151 01 0546 Volltext http://nbn-resolving.de/urn:nbn:de:gbv:7-11858/00-1735-0000-0023-3E7F-6-8 161 01 0960 http://nbn-resolving.de/urn:nbn:de:gbv:7-11858/00-1735-0000-0023-3E7F-6-8 293 01 3293 http://nbn-resolving.de/urn:nbn:de:gbv:7-11858/00-1735-0000-0023-3E7F-6-8 370 01 4370 http://nbn-resolving.de/urn:nbn:de:gbv:7-11858/00-1735-0000-0023-3E7F-6-8 2403 01 DE-LFER http://nbn-resolving.org/urn:nbn:de:gbv:7-11858/00-1735-0000-0023-3E7F-6-8 40 00 DE-7 00 (DE-627)625047842 VBO 000 Isotopengeologie 60 01 0705 10 ho 20 01 0084 OLRD 110 01 3110 OLRD 370 01 4370 OLRD 22 01 0018 SUBolrd 23 01 0830 olr-d 40 01 0007 ediss 60 01 0705 OLRD 63 01 3401 ORD 132 01 0959 OLR-DISS 151 01 0546 OLR-ODISS 161 01 0960 ORD 293 01 3293 ORD 23 01 0830 2017-07-06:08:49:20
allfields_unstemmed	17,O07 dnb 1135778345 DE-101 urn:nbn:de:gbv:7-11858/00-1735-0000-0023-3E7F-6-8 urn (DE-627)890545316 (DE-576)9890545314 (DE-599)GBV890545316 DE-627 ger DE-627 rda eng XA-DE-NI 910 550 SEPA 22 550 DE-101 Sengupta, Sukanya verfasserin aut Triple oxygen isotopes of cherts : implications for the δ18O and temperatures of early oceans vorgelegt von Sukanya Sengupta Göttingen 2016 1 Online-Ressource Illustrationen, Diagramme Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Dissertation Georg-August-Universität Göttingen 2016 The temperature of Earth’s earliest oceans, in which life may have first originated, remains a controversial issue in Earth science. Over the last 50 years, many studies have attempted to apply the temperature dependent fractionation of oxygen isotopes 18O/16O to ancient marine chemical sediments in order to infer the temperatures of the ancient oceans. The δ18O composition of marine chemical sediments progressively decrease with increasing age leading to the suggestions that either the Precambrian oceans were also strongly depleted in 18O (~-13‰) but had the same temperature as modern day,... Langzeitarchivierung gewährleistet pdager Hochschulschrift (DE-588)4113937-9 (DE-627)105825778 (DE-576)209480580 gnd-content Pack, Andreas akademischer betreuerin dgs Pack, Andreas gutachterin oth Hoefs, Jochen gutachterin oth Erscheint auch als Druck-Ausgabe Sengupta, Sukanya Triple oxygen isotopes of cherts : implications for the δ18O and temperatures of early oceans Göttingen, 2016 218, vi Seiten (DE-627)890545324 http://hdl.handle.net/11858/00-1735-0000-0023-3E7F-6 Resolving-System Volltext kostenfrei Volltext http://nbn-resolving.org/urn:nbn:de:gbv:7-11858/00-1735-0000-0023-3E7F-6-8 Resolving-System Volltext kostenfrei Volltext http://nbn-resolving.de/urn:nbn:de:gbv:7-11858/00-1735-0000-0023-3E7F-6-8 2017-07-05 Resolving-System Volltext http://d-nb.info/1135778345/34 2017-07-05 Langzeitarchivierung Nationalbibliothek Volltext GBV-ODiss GBV_ILN_20 ISIL_DE-84 SYSFLAG_1 GBV_KXP SSG-OPC-GEO SSG-OPC-GGO GBV_ILN_21 ISIL_DE-46 GBV_ILN_22 ISIL_DE-18 GBV_ILN_23 ISIL_DE-830 GBV_ILN_30 ISIL_DE-104 GBV_ILN_40 ISIL_DE-7 GBV_ILN_60 ISIL_DE-705 GBV_ILN_63 ISIL_DE-Wim2 GBV_ILN_70 ISIL_DE-89 GBV_ILN_105 ISIL_DE-841 GBV_ILN_110 ISIL_DE-Luen4 GBV_ILN_132 ISIL_DE-959 GBV_ILN_151 ISIL_DE-546 GBV_ILN_161 ISIL_DE-960 GBV_ILN_293 ISIL_DE-960-3 GBV_ILN_370 ISIL_DE-1373 GBV_ILN_2403 ISIL_DE-LFER BO 045F 910 20 01 0084 169971617X x 06-07-17 21 01 0046 1699729204 z 06-07-17 22 01 0018 1699742170 SUBolrd xu 06-07-17 23 01 0830 1699754683 olr-d x 06-07-17 30 01 0104 1699762511 z 06-07-17 40 01 0007 169530196X ediss xsn 20-06-17 60 01 0705 1699782547 OLRD z 06-07-17 63 01 3401 1699795169 ORD x 06-07-17 70 01 0089 1699801118 zdo 06-07-17 105 01 0841 1699869553 z 06-07-17 110 01 3110 1699809844 x 06-07-17 132 01 0959 1699818746 OLR-DISS x 06-07-17 151 01 0546 3583672860 OLR-ODISS z 31-01-20 161 01 0960 1699832110 ORD x 06-07-17 293 01 3293 1699859221 ORD xf 06-07-17 370 01 4370 1699866538 x 06-07-17 2403 01 DE-LFER 3475889536 00 --%%-- --%%-- n --%%-- l01 15-05-19 20 01 0084 http://nbn-resolving.de/urn:nbn:de:gbv:7-11858/00-1735-0000-0023-3E7F-6-8 21 01 0046 http://nbn-resolving.de/urn:nbn:de:gbv:7-11858/00-1735-0000-0023-3E7F-6-8 22 01 0018 http://nbn-resolving.de/urn:nbn:de:gbv:7-11858/00-1735-0000-0023-3E7F-6-8 23 01 0830 http://nbn-resolving.de/urn:nbn:de:gbv:7-11858/00-1735-0000-0023-3E7F-6-8 30 01 0104 http://nbn-resolving.de/urn:nbn:de:gbv:7-11858/00-1735-0000-0023-3E7F-6-8 40 01 0007 Volltext http://hdl.handle.net/11858/00-1735-0000-0023-3E7F-6 LF 60 01 0705 http://nbn-resolving.de/urn:nbn:de:gbv:7-11858/00-1735-0000-0023-3E7F-6-8 63 01 3401 E-Book http://nbn-resolving.de/urn:nbn:de:gbv:7-11858/00-1735-0000-0023-3E7F-6-8 LF 70 01 0089 http://nbn-resolving.de/urn:nbn:de:gbv:7-11858/00-1735-0000-0023-3E7F-6-8 105 01 0841 http://nbn-resolving.de/urn:nbn:de:gbv:7-11858/00-1735-0000-0023-3E7F-6-8 110 01 3110 http://nbn-resolving.de/urn:nbn:de:gbv:7-11858/00-1735-0000-0023-3E7F-6-8 132 01 0959 http://nbn-resolving.de/urn:nbn:de:gbv:7-11858/00-1735-0000-0023-3E7F-6-8 151 01 0546 Volltext http://nbn-resolving.de/urn:nbn:de:gbv:7-11858/00-1735-0000-0023-3E7F-6-8 161 01 0960 http://nbn-resolving.de/urn:nbn:de:gbv:7-11858/00-1735-0000-0023-3E7F-6-8 293 01 3293 http://nbn-resolving.de/urn:nbn:de:gbv:7-11858/00-1735-0000-0023-3E7F-6-8 370 01 4370 http://nbn-resolving.de/urn:nbn:de:gbv:7-11858/00-1735-0000-0023-3E7F-6-8 2403 01 DE-LFER http://nbn-resolving.org/urn:nbn:de:gbv:7-11858/00-1735-0000-0023-3E7F-6-8 40 00 DE-7 00 (DE-627)625047842 VBO 000 Isotopengeologie 60 01 0705 10 ho 20 01 0084 OLRD 110 01 3110 OLRD 370 01 4370 OLRD 22 01 0018 SUBolrd 23 01 0830 olr-d 40 01 0007 ediss 60 01 0705 OLRD 63 01 3401 ORD 132 01 0959 OLR-DISS 151 01 0546 OLR-ODISS 161 01 0960 ORD 293 01 3293 ORD 23 01 0830 2017-07-06:08:49:20
allfieldsGer	17,O07 dnb 1135778345 DE-101 urn:nbn:de:gbv:7-11858/00-1735-0000-0023-3E7F-6-8 urn (DE-627)890545316 (DE-576)9890545314 (DE-599)GBV890545316 DE-627 ger DE-627 rda eng XA-DE-NI 910 550 SEPA 22 550 DE-101 Sengupta, Sukanya verfasserin aut Triple oxygen isotopes of cherts : implications for the δ18O and temperatures of early oceans vorgelegt von Sukanya Sengupta Göttingen 2016 1 Online-Ressource Illustrationen, Diagramme Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Dissertation Georg-August-Universität Göttingen 2016 The temperature of Earth’s earliest oceans, in which life may have first originated, remains a controversial issue in Earth science. Over the last 50 years, many studies have attempted to apply the temperature dependent fractionation of oxygen isotopes 18O/16O to ancient marine chemical sediments in order to infer the temperatures of the ancient oceans. The δ18O composition of marine chemical sediments progressively decrease with increasing age leading to the suggestions that either the Precambrian oceans were also strongly depleted in 18O (~-13‰) but had the same temperature as modern day,... Langzeitarchivierung gewährleistet pdager Hochschulschrift (DE-588)4113937-9 (DE-627)105825778 (DE-576)209480580 gnd-content Pack, Andreas akademischer betreuerin dgs Pack, Andreas gutachterin oth Hoefs, Jochen gutachterin oth Erscheint auch als Druck-Ausgabe Sengupta, Sukanya Triple oxygen isotopes of cherts : implications for the δ18O and temperatures of early oceans Göttingen, 2016 218, vi Seiten (DE-627)890545324 http://hdl.handle.net/11858/00-1735-0000-0023-3E7F-6 Resolving-System Volltext kostenfrei Volltext http://nbn-resolving.org/urn:nbn:de:gbv:7-11858/00-1735-0000-0023-3E7F-6-8 Resolving-System Volltext kostenfrei Volltext http://nbn-resolving.de/urn:nbn:de:gbv:7-11858/00-1735-0000-0023-3E7F-6-8 2017-07-05 Resolving-System Volltext http://d-nb.info/1135778345/34 2017-07-05 Langzeitarchivierung Nationalbibliothek Volltext GBV-ODiss GBV_ILN_20 ISIL_DE-84 SYSFLAG_1 GBV_KXP SSG-OPC-GEO SSG-OPC-GGO GBV_ILN_21 ISIL_DE-46 GBV_ILN_22 ISIL_DE-18 GBV_ILN_23 ISIL_DE-830 GBV_ILN_30 ISIL_DE-104 GBV_ILN_40 ISIL_DE-7 GBV_ILN_60 ISIL_DE-705 GBV_ILN_63 ISIL_DE-Wim2 GBV_ILN_70 ISIL_DE-89 GBV_ILN_105 ISIL_DE-841 GBV_ILN_110 ISIL_DE-Luen4 GBV_ILN_132 ISIL_DE-959 GBV_ILN_151 ISIL_DE-546 GBV_ILN_161 ISIL_DE-960 GBV_ILN_293 ISIL_DE-960-3 GBV_ILN_370 ISIL_DE-1373 GBV_ILN_2403 ISIL_DE-LFER BO 045F 910 20 01 0084 169971617X x 06-07-17 21 01 0046 1699729204 z 06-07-17 22 01 0018 1699742170 SUBolrd xu 06-07-17 23 01 0830 1699754683 olr-d x 06-07-17 30 01 0104 1699762511 z 06-07-17 40 01 0007 169530196X ediss xsn 20-06-17 60 01 0705 1699782547 OLRD z 06-07-17 63 01 3401 1699795169 ORD x 06-07-17 70 01 0089 1699801118 zdo 06-07-17 105 01 0841 1699869553 z 06-07-17 110 01 3110 1699809844 x 06-07-17 132 01 0959 1699818746 OLR-DISS x 06-07-17 151 01 0546 3583672860 OLR-ODISS z 31-01-20 161 01 0960 1699832110 ORD x 06-07-17 293 01 3293 1699859221 ORD xf 06-07-17 370 01 4370 1699866538 x 06-07-17 2403 01 DE-LFER 3475889536 00 --%%-- --%%-- n --%%-- l01 15-05-19 20 01 0084 http://nbn-resolving.de/urn:nbn:de:gbv:7-11858/00-1735-0000-0023-3E7F-6-8 21 01 0046 http://nbn-resolving.de/urn:nbn:de:gbv:7-11858/00-1735-0000-0023-3E7F-6-8 22 01 0018 http://nbn-resolving.de/urn:nbn:de:gbv:7-11858/00-1735-0000-0023-3E7F-6-8 23 01 0830 http://nbn-resolving.de/urn:nbn:de:gbv:7-11858/00-1735-0000-0023-3E7F-6-8 30 01 0104 http://nbn-resolving.de/urn:nbn:de:gbv:7-11858/00-1735-0000-0023-3E7F-6-8 40 01 0007 Volltext http://hdl.handle.net/11858/00-1735-0000-0023-3E7F-6 LF 60 01 0705 http://nbn-resolving.de/urn:nbn:de:gbv:7-11858/00-1735-0000-0023-3E7F-6-8 63 01 3401 E-Book http://nbn-resolving.de/urn:nbn:de:gbv:7-11858/00-1735-0000-0023-3E7F-6-8 LF 70 01 0089 http://nbn-resolving.de/urn:nbn:de:gbv:7-11858/00-1735-0000-0023-3E7F-6-8 105 01 0841 http://nbn-resolving.de/urn:nbn:de:gbv:7-11858/00-1735-0000-0023-3E7F-6-8 110 01 3110 http://nbn-resolving.de/urn:nbn:de:gbv:7-11858/00-1735-0000-0023-3E7F-6-8 132 01 0959 http://nbn-resolving.de/urn:nbn:de:gbv:7-11858/00-1735-0000-0023-3E7F-6-8 151 01 0546 Volltext http://nbn-resolving.de/urn:nbn:de:gbv:7-11858/00-1735-0000-0023-3E7F-6-8 161 01 0960 http://nbn-resolving.de/urn:nbn:de:gbv:7-11858/00-1735-0000-0023-3E7F-6-8 293 01 3293 http://nbn-resolving.de/urn:nbn:de:gbv:7-11858/00-1735-0000-0023-3E7F-6-8 370 01 4370 http://nbn-resolving.de/urn:nbn:de:gbv:7-11858/00-1735-0000-0023-3E7F-6-8 2403 01 DE-LFER http://nbn-resolving.org/urn:nbn:de:gbv:7-11858/00-1735-0000-0023-3E7F-6-8 40 00 DE-7 00 (DE-627)625047842 VBO 000 Isotopengeologie 60 01 0705 10 ho 20 01 0084 OLRD 110 01 3110 OLRD 370 01 4370 OLRD 22 01 0018 SUBolrd 23 01 0830 olr-d 40 01 0007 ediss 60 01 0705 OLRD 63 01 3401 ORD 132 01 0959 OLR-DISS 151 01 0546 OLR-ODISS 161 01 0960 ORD 293 01 3293 ORD 23 01 0830 2017-07-06:08:49:20
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title_sort	triple oxygen isotopes of cherts : implications for the δ18o and temperatures of early oceans
title_auth	Triple oxygen isotopes of cherts : implications for the δ18O and temperatures of early oceans
abstract	The temperature of Earth’s earliest oceans, in which life may have first originated, remains a controversial issue in Earth science. Over the last 50 years, many studies have attempted to apply the temperature dependent fractionation of oxygen isotopes 18O/16O to ancient marine chemical sediments in order to infer the temperatures of the ancient oceans. The δ18O composition of marine chemical sediments progressively decrease with increasing age leading to the suggestions that either the Precambrian oceans were also strongly depleted in 18O (~-13‰) but had the same temperature as modern day,...
abstractGer	The temperature of Earth’s earliest oceans, in which life may have first originated, remains a controversial issue in Earth science. Over the last 50 years, many studies have attempted to apply the temperature dependent fractionation of oxygen isotopes 18O/16O to ancient marine chemical sediments in order to infer the temperatures of the ancient oceans. The δ18O composition of marine chemical sediments progressively decrease with increasing age leading to the suggestions that either the Precambrian oceans were also strongly depleted in 18O (~-13‰) but had the same temperature as modern day,...
abstract_unstemmed	The temperature of Earth’s earliest oceans, in which life may have first originated, remains a controversial issue in Earth science. Over the last 50 years, many studies have attempted to apply the temperature dependent fractionation of oxygen isotopes 18O/16O to ancient marine chemical sediments in order to infer the temperatures of the ancient oceans. The δ18O composition of marine chemical sediments progressively decrease with increasing age leading to the suggestions that either the Precambrian oceans were also strongly depleted in 18O (~-13‰) but had the same temperature as modern day,...
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title_short	Triple oxygen isotopes of cherts : implications for the δ18O and temperatures of early oceans
url	http://hdl.handle.net/11858/00-1735-0000-0023-3E7F-6 http://nbn-resolving.org/urn:nbn:de:gbv:7-11858/00-1735-0000-0023-3E7F-6-8 http://nbn-resolving.de/urn:nbn:de:gbv:7-11858/00-1735-0000-0023-3E7F-6-8 http://d-nb.info/1135778345/34
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Triple oxygen isotopes of cherts : implications for the δ18O and temperatures of early oceans

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