Quantitative reconstruction of the palaeoclimate of the Shahejie Formation in the Chezhen Depression, Bohai Bay Basin, eastern China
Abstract This paper uses pollen climate analysis and coexistence analysis to systematically analyze the climatic evolution of the Shahejie Formation in the Chezhen Depression, Bohai Bay Basin, eastern China and discusses the relationship between palaeoclimatic evolution and lake level rise. The resu...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Chen, Tao [verfasserIn] |
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| Format: |
E-Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2021 |
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| Schlagwörter: |
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| Anmerkung: |
© Higher Education Press 2021 |
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| Übergeordnetes Werk: |
Enthalten in: Frontiers of earth science in China - Beijing : Higher Education Press, 2007, 15(2021), 4 vom: Dez., Seite 909-921 |
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| Übergeordnetes Werk: |
volume:15 ; year:2021 ; number:4 ; month:12 ; pages:909-921 |
| Links: |
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| DOI / URN: |
10.1007/s11707-021-0932-7 |
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SPR050439111 |
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| 520 | |a Abstract This paper uses pollen climate analysis and coexistence analysis to systematically analyze the climatic evolution of the Shahejie Formation in the Chezhen Depression, Bohai Bay Basin, eastern China and discusses the relationship between palaeoclimatic evolution and lake level rise. The results show that the sedimentary period of the Shahejie Formation in the Chezhen Depression had an overall temperature change trend from hot to cold and simultaneously experienced a dry and wet balance-wet-dry and wet balance-wet transition process. The climatic parameters of the Shahejie Formation in the Chezhen Depression include a mean annual temperature of 8.1°C–15.1°C, a mean coldest monthly temperature of −0.1°C–2°C, a mean warmest monthly temperature of 18.6°C–28°C, a mean annual precipitation of 389–1164 mm, a wettest monthly precipitation amount of 215–262 mm, and a driest monthly precipitation amount of 8–48 mm. Climate change is believed to affect the rise and fall of lake levels to some extent. The quantitative reconstruction of these climatic parameters allows researchers to more intuitively understand the geological background of the Chezhen Depression and guide the exploration and development of oil and gas resources. | ||
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10.1007/s11707-021-0932-7 doi (DE-627)SPR050439111 (SPR)s11707-021-0932-7-e DE-627 ger DE-627 rakwb eng Chen, Tao verfasserin aut Quantitative reconstruction of the palaeoclimate of the Shahejie Formation in the Chezhen Depression, Bohai Bay Basin, eastern China 2021 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Higher Education Press 2021 Abstract This paper uses pollen climate analysis and coexistence analysis to systematically analyze the climatic evolution of the Shahejie Formation in the Chezhen Depression, Bohai Bay Basin, eastern China and discusses the relationship between palaeoclimatic evolution and lake level rise. The results show that the sedimentary period of the Shahejie Formation in the Chezhen Depression had an overall temperature change trend from hot to cold and simultaneously experienced a dry and wet balance-wet-dry and wet balance-wet transition process. The climatic parameters of the Shahejie Formation in the Chezhen Depression include a mean annual temperature of 8.1°C–15.1°C, a mean coldest monthly temperature of −0.1°C–2°C, a mean warmest monthly temperature of 18.6°C–28°C, a mean annual precipitation of 389–1164 mm, a wettest monthly precipitation amount of 215–262 mm, and a driest monthly precipitation amount of 8–48 mm. Climate change is believed to affect the rise and fall of lake levels to some extent. The quantitative reconstruction of these climatic parameters allows researchers to more intuitively understand the geological background of the Chezhen Depression and guide the exploration and development of oil and gas resources. Shahejie Formation (dpeaa)DE-He213 Chezhen Depression (dpeaa)DE-He213 pollen (dpeaa)DE-He213 coexistence analysis (dpeaa)DE-He213 palaeoclimate reconstruction (dpeaa)DE-He213 Zhang, Jinliang aut Li, Yang aut Zhao, Yongfu aut Enthalten in Frontiers of earth science in China Beijing : Higher Education Press, 2007 15(2021), 4 vom: Dez., Seite 909-921 (DE-627)546007406 (DE-600)2389435-0 1673-7490 nnns volume:15 year:2021 number:4 month:12 pages:909-921 https://dx.doi.org/10.1007/s11707-021-0932-7 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER 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_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_120 GBV_ILN_152 GBV_ILN_161 GBV_ILN_171 GBV_ILN_187 GBV_ILN_224 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_702 AR 15 2021 4 12 909-921 |
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10.1007/s11707-021-0932-7 doi (DE-627)SPR050439111 (SPR)s11707-021-0932-7-e DE-627 ger DE-627 rakwb eng Chen, Tao verfasserin aut Quantitative reconstruction of the palaeoclimate of the Shahejie Formation in the Chezhen Depression, Bohai Bay Basin, eastern China 2021 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Higher Education Press 2021 Abstract This paper uses pollen climate analysis and coexistence analysis to systematically analyze the climatic evolution of the Shahejie Formation in the Chezhen Depression, Bohai Bay Basin, eastern China and discusses the relationship between palaeoclimatic evolution and lake level rise. The results show that the sedimentary period of the Shahejie Formation in the Chezhen Depression had an overall temperature change trend from hot to cold and simultaneously experienced a dry and wet balance-wet-dry and wet balance-wet transition process. The climatic parameters of the Shahejie Formation in the Chezhen Depression include a mean annual temperature of 8.1°C–15.1°C, a mean coldest monthly temperature of −0.1°C–2°C, a mean warmest monthly temperature of 18.6°C–28°C, a mean annual precipitation of 389–1164 mm, a wettest monthly precipitation amount of 215–262 mm, and a driest monthly precipitation amount of 8–48 mm. Climate change is believed to affect the rise and fall of lake levels to some extent. The quantitative reconstruction of these climatic parameters allows researchers to more intuitively understand the geological background of the Chezhen Depression and guide the exploration and development of oil and gas resources. Shahejie Formation (dpeaa)DE-He213 Chezhen Depression (dpeaa)DE-He213 pollen (dpeaa)DE-He213 coexistence analysis (dpeaa)DE-He213 palaeoclimate reconstruction (dpeaa)DE-He213 Zhang, Jinliang aut Li, Yang aut Zhao, Yongfu aut Enthalten in Frontiers of earth science in China Beijing : Higher Education Press, 2007 15(2021), 4 vom: Dez., Seite 909-921 (DE-627)546007406 (DE-600)2389435-0 1673-7490 nnns volume:15 year:2021 number:4 month:12 pages:909-921 https://dx.doi.org/10.1007/s11707-021-0932-7 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER 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_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_120 GBV_ILN_152 GBV_ILN_161 GBV_ILN_171 GBV_ILN_187 GBV_ILN_224 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_702 AR 15 2021 4 12 909-921 |
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10.1007/s11707-021-0932-7 doi (DE-627)SPR050439111 (SPR)s11707-021-0932-7-e DE-627 ger DE-627 rakwb eng Chen, Tao verfasserin aut Quantitative reconstruction of the palaeoclimate of the Shahejie Formation in the Chezhen Depression, Bohai Bay Basin, eastern China 2021 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Higher Education Press 2021 Abstract This paper uses pollen climate analysis and coexistence analysis to systematically analyze the climatic evolution of the Shahejie Formation in the Chezhen Depression, Bohai Bay Basin, eastern China and discusses the relationship between palaeoclimatic evolution and lake level rise. The results show that the sedimentary period of the Shahejie Formation in the Chezhen Depression had an overall temperature change trend from hot to cold and simultaneously experienced a dry and wet balance-wet-dry and wet balance-wet transition process. The climatic parameters of the Shahejie Formation in the Chezhen Depression include a mean annual temperature of 8.1°C–15.1°C, a mean coldest monthly temperature of −0.1°C–2°C, a mean warmest monthly temperature of 18.6°C–28°C, a mean annual precipitation of 389–1164 mm, a wettest monthly precipitation amount of 215–262 mm, and a driest monthly precipitation amount of 8–48 mm. Climate change is believed to affect the rise and fall of lake levels to some extent. The quantitative reconstruction of these climatic parameters allows researchers to more intuitively understand the geological background of the Chezhen Depression and guide the exploration and development of oil and gas resources. Shahejie Formation (dpeaa)DE-He213 Chezhen Depression (dpeaa)DE-He213 pollen (dpeaa)DE-He213 coexistence analysis (dpeaa)DE-He213 palaeoclimate reconstruction (dpeaa)DE-He213 Zhang, Jinliang aut Li, Yang aut Zhao, Yongfu aut Enthalten in Frontiers of earth science in China Beijing : Higher Education Press, 2007 15(2021), 4 vom: Dez., Seite 909-921 (DE-627)546007406 (DE-600)2389435-0 1673-7490 nnns volume:15 year:2021 number:4 month:12 pages:909-921 https://dx.doi.org/10.1007/s11707-021-0932-7 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER 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_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_120 GBV_ILN_152 GBV_ILN_161 GBV_ILN_171 GBV_ILN_187 GBV_ILN_224 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_702 AR 15 2021 4 12 909-921 |
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10.1007/s11707-021-0932-7 doi (DE-627)SPR050439111 (SPR)s11707-021-0932-7-e DE-627 ger DE-627 rakwb eng Chen, Tao verfasserin aut Quantitative reconstruction of the palaeoclimate of the Shahejie Formation in the Chezhen Depression, Bohai Bay Basin, eastern China 2021 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Higher Education Press 2021 Abstract This paper uses pollen climate analysis and coexistence analysis to systematically analyze the climatic evolution of the Shahejie Formation in the Chezhen Depression, Bohai Bay Basin, eastern China and discusses the relationship between palaeoclimatic evolution and lake level rise. The results show that the sedimentary period of the Shahejie Formation in the Chezhen Depression had an overall temperature change trend from hot to cold and simultaneously experienced a dry and wet balance-wet-dry and wet balance-wet transition process. The climatic parameters of the Shahejie Formation in the Chezhen Depression include a mean annual temperature of 8.1°C–15.1°C, a mean coldest monthly temperature of −0.1°C–2°C, a mean warmest monthly temperature of 18.6°C–28°C, a mean annual precipitation of 389–1164 mm, a wettest monthly precipitation amount of 215–262 mm, and a driest monthly precipitation amount of 8–48 mm. Climate change is believed to affect the rise and fall of lake levels to some extent. The quantitative reconstruction of these climatic parameters allows researchers to more intuitively understand the geological background of the Chezhen Depression and guide the exploration and development of oil and gas resources. Shahejie Formation (dpeaa)DE-He213 Chezhen Depression (dpeaa)DE-He213 pollen (dpeaa)DE-He213 coexistence analysis (dpeaa)DE-He213 palaeoclimate reconstruction (dpeaa)DE-He213 Zhang, Jinliang aut Li, Yang aut Zhao, Yongfu aut Enthalten in Frontiers of earth science in China Beijing : Higher Education Press, 2007 15(2021), 4 vom: Dez., Seite 909-921 (DE-627)546007406 (DE-600)2389435-0 1673-7490 nnns volume:15 year:2021 number:4 month:12 pages:909-921 https://dx.doi.org/10.1007/s11707-021-0932-7 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER 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_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_120 GBV_ILN_152 GBV_ILN_161 GBV_ILN_171 GBV_ILN_187 GBV_ILN_224 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_702 AR 15 2021 4 12 909-921 |
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10.1007/s11707-021-0932-7 doi (DE-627)SPR050439111 (SPR)s11707-021-0932-7-e DE-627 ger DE-627 rakwb eng Chen, Tao verfasserin aut Quantitative reconstruction of the palaeoclimate of the Shahejie Formation in the Chezhen Depression, Bohai Bay Basin, eastern China 2021 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Higher Education Press 2021 Abstract This paper uses pollen climate analysis and coexistence analysis to systematically analyze the climatic evolution of the Shahejie Formation in the Chezhen Depression, Bohai Bay Basin, eastern China and discusses the relationship between palaeoclimatic evolution and lake level rise. The results show that the sedimentary period of the Shahejie Formation in the Chezhen Depression had an overall temperature change trend from hot to cold and simultaneously experienced a dry and wet balance-wet-dry and wet balance-wet transition process. The climatic parameters of the Shahejie Formation in the Chezhen Depression include a mean annual temperature of 8.1°C–15.1°C, a mean coldest monthly temperature of −0.1°C–2°C, a mean warmest monthly temperature of 18.6°C–28°C, a mean annual precipitation of 389–1164 mm, a wettest monthly precipitation amount of 215–262 mm, and a driest monthly precipitation amount of 8–48 mm. Climate change is believed to affect the rise and fall of lake levels to some extent. The quantitative reconstruction of these climatic parameters allows researchers to more intuitively understand the geological background of the Chezhen Depression and guide the exploration and development of oil and gas resources. Shahejie Formation (dpeaa)DE-He213 Chezhen Depression (dpeaa)DE-He213 pollen (dpeaa)DE-He213 coexistence analysis (dpeaa)DE-He213 palaeoclimate reconstruction (dpeaa)DE-He213 Zhang, Jinliang aut Li, Yang aut Zhao, Yongfu aut Enthalten in Frontiers of earth science in China Beijing : Higher Education Press, 2007 15(2021), 4 vom: Dez., Seite 909-921 (DE-627)546007406 (DE-600)2389435-0 1673-7490 nnns volume:15 year:2021 number:4 month:12 pages:909-921 https://dx.doi.org/10.1007/s11707-021-0932-7 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER 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_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_120 GBV_ILN_152 GBV_ILN_161 GBV_ILN_171 GBV_ILN_187 GBV_ILN_224 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_702 AR 15 2021 4 12 909-921 |
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Quantitative reconstruction of the palaeoclimate of the Shahejie Formation in the Chezhen Depression, Bohai Bay Basin, eastern China Shahejie Formation (dpeaa)DE-He213 Chezhen Depression (dpeaa)DE-He213 pollen (dpeaa)DE-He213 coexistence analysis (dpeaa)DE-He213 palaeoclimate reconstruction (dpeaa)DE-He213 |
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quantitative reconstruction of the palaeoclimate of the shahejie formation in the chezhen depression, bohai bay basin, eastern china |
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Quantitative reconstruction of the palaeoclimate of the Shahejie Formation in the Chezhen Depression, Bohai Bay Basin, eastern China |
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Abstract This paper uses pollen climate analysis and coexistence analysis to systematically analyze the climatic evolution of the Shahejie Formation in the Chezhen Depression, Bohai Bay Basin, eastern China and discusses the relationship between palaeoclimatic evolution and lake level rise. The results show that the sedimentary period of the Shahejie Formation in the Chezhen Depression had an overall temperature change trend from hot to cold and simultaneously experienced a dry and wet balance-wet-dry and wet balance-wet transition process. The climatic parameters of the Shahejie Formation in the Chezhen Depression include a mean annual temperature of 8.1°C–15.1°C, a mean coldest monthly temperature of −0.1°C–2°C, a mean warmest monthly temperature of 18.6°C–28°C, a mean annual precipitation of 389–1164 mm, a wettest monthly precipitation amount of 215–262 mm, and a driest monthly precipitation amount of 8–48 mm. Climate change is believed to affect the rise and fall of lake levels to some extent. The quantitative reconstruction of these climatic parameters allows researchers to more intuitively understand the geological background of the Chezhen Depression and guide the exploration and development of oil and gas resources. © Higher Education Press 2021 |
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Abstract This paper uses pollen climate analysis and coexistence analysis to systematically analyze the climatic evolution of the Shahejie Formation in the Chezhen Depression, Bohai Bay Basin, eastern China and discusses the relationship between palaeoclimatic evolution and lake level rise. The results show that the sedimentary period of the Shahejie Formation in the Chezhen Depression had an overall temperature change trend from hot to cold and simultaneously experienced a dry and wet balance-wet-dry and wet balance-wet transition process. The climatic parameters of the Shahejie Formation in the Chezhen Depression include a mean annual temperature of 8.1°C–15.1°C, a mean coldest monthly temperature of −0.1°C–2°C, a mean warmest monthly temperature of 18.6°C–28°C, a mean annual precipitation of 389–1164 mm, a wettest monthly precipitation amount of 215–262 mm, and a driest monthly precipitation amount of 8–48 mm. Climate change is believed to affect the rise and fall of lake levels to some extent. The quantitative reconstruction of these climatic parameters allows researchers to more intuitively understand the geological background of the Chezhen Depression and guide the exploration and development of oil and gas resources. © Higher Education Press 2021 |
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Abstract This paper uses pollen climate analysis and coexistence analysis to systematically analyze the climatic evolution of the Shahejie Formation in the Chezhen Depression, Bohai Bay Basin, eastern China and discusses the relationship between palaeoclimatic evolution and lake level rise. The results show that the sedimentary period of the Shahejie Formation in the Chezhen Depression had an overall temperature change trend from hot to cold and simultaneously experienced a dry and wet balance-wet-dry and wet balance-wet transition process. The climatic parameters of the Shahejie Formation in the Chezhen Depression include a mean annual temperature of 8.1°C–15.1°C, a mean coldest monthly temperature of −0.1°C–2°C, a mean warmest monthly temperature of 18.6°C–28°C, a mean annual precipitation of 389–1164 mm, a wettest monthly precipitation amount of 215–262 mm, and a driest monthly precipitation amount of 8–48 mm. Climate change is believed to affect the rise and fall of lake levels to some extent. The quantitative reconstruction of these climatic parameters allows researchers to more intuitively understand the geological background of the Chezhen Depression and guide the exploration and development of oil and gas resources. © Higher Education Press 2021 |
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