Micropaleontology and palaeoclimate during the early Cretaceous in the Lishu depression, Songliao basin, Northeast China
Diverse and abundant microfossils, such as palynomorphs, algae and Ostracoda, were collected from lower Cretaceous strata of Lishu depression, located in southeastern Songliao basin, and were identified and classified in order to provide relevant, detailed records for paleoclimate research. The earl...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Wei Yan [verfasserIn] Tailiang Fan [verfasserIn] Hongyu Wang [verfasserIn] Chen Zhu [verfasserIn] Zhiqian Gao [verfasserIn] Xiangjie Meng [verfasserIn] Yangzi Sun [verfasserIn] Fan Yang [verfasserIn] |
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| Format: |
E-Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2017 |
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| Schlagwörter: |
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| Übergeordnetes Werk: |
In: Geoscience Frontiers - Elsevier, 2016, 8(2017), 1, Seite 93-106 |
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| Übergeordnetes Werk: |
volume:8 ; year:2017 ; number:1 ; pages:93-106 |
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| DOI / URN: |
10.1016/j.gsf.2015.12.005 |
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| 520 | |a Diverse and abundant microfossils, such as palynomorphs, algae and Ostracoda, were collected from lower Cretaceous strata of Lishu depression, located in southeastern Songliao basin, and were identified and classified in order to provide relevant, detailed records for paleoclimate research. The early Cretaceous vegetation and climate of southeastern Songliao basin have been inferred from the analysis of palynomorph genera, algae and Ostracoda of the LS1 and SW110 wells. The lower Cretaceous strata include, in ascending stratigraphic order, the Shahezi, Yingcheng and Denglouku formations. Palynological assemblages for each formation, based on biostratigraphic and statistical analyses, provide an assessment of their longitudinal variations. During deposition of the Shahezi Formation, the climate was mid-subtropical. Vegetation consisted of coniferous forest and herbage. During deposition of the Yingcheng Formation, the climate was south Asian tropical. Vegetation consisted mainly of coniferous forest and herbal shrub. In addition, fresh and saline non-marine water dominated the lacustrine setting during deposition of these formations. Deposition of the Denglouku Formation, however, occurred under a hot and dry tropical climate. The vegetation was mostly coniferous forest and lake waters became saline. Palaeoclimate variation is correlated by the lake level change and the development of sedimentary facies. Palaeoclimate contribute to the formation of hydrocarbon source rocks and reservoir. | ||
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10.1016/j.gsf.2015.12.005 doi (DE-627)DOAJ078335728 (DE-599)DOAJ0cfde92f1c6d48c6a967cdaf687d44af DE-627 ger DE-627 rakwb eng QE1-996.5 Wei Yan verfasserin aut Micropaleontology and palaeoclimate during the early Cretaceous in the Lishu depression, Songliao basin, Northeast China 2017 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Diverse and abundant microfossils, such as palynomorphs, algae and Ostracoda, were collected from lower Cretaceous strata of Lishu depression, located in southeastern Songliao basin, and were identified and classified in order to provide relevant, detailed records for paleoclimate research. The early Cretaceous vegetation and climate of southeastern Songliao basin have been inferred from the analysis of palynomorph genera, algae and Ostracoda of the LS1 and SW110 wells. The lower Cretaceous strata include, in ascending stratigraphic order, the Shahezi, Yingcheng and Denglouku formations. Palynological assemblages for each formation, based on biostratigraphic and statistical analyses, provide an assessment of their longitudinal variations. During deposition of the Shahezi Formation, the climate was mid-subtropical. Vegetation consisted of coniferous forest and herbage. During deposition of the Yingcheng Formation, the climate was south Asian tropical. Vegetation consisted mainly of coniferous forest and herbal shrub. In addition, fresh and saline non-marine water dominated the lacustrine setting during deposition of these formations. Deposition of the Denglouku Formation, however, occurred under a hot and dry tropical climate. The vegetation was mostly coniferous forest and lake waters became saline. Palaeoclimate variation is correlated by the lake level change and the development of sedimentary facies. Palaeoclimate contribute to the formation of hydrocarbon source rocks and reservoir. Palynomorph Palaeoclimate Early Cretaceous Lishu depression Songliao Basin Geology Tailiang Fan verfasserin aut Hongyu Wang verfasserin aut Chen Zhu verfasserin aut Zhiqian Gao verfasserin aut Xiangjie Meng verfasserin aut Yangzi Sun verfasserin aut Fan Yang verfasserin aut In Geoscience Frontiers Elsevier, 2016 8(2017), 1, Seite 93-106 (DE-627)DOAJ000091189 25889192 nnns volume:8 year:2017 number:1 pages:93-106 https://doi.org/10.1016/j.gsf.2015.12.005 kostenfrei https://doaj.org/article/0cfde92f1c6d48c6a967cdaf687d44af kostenfrei http://www.sciencedirect.com/science/article/pii/S1674987116000025 kostenfrei https://doaj.org/toc/1674-9871 Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ AR 8 2017 1 93-106 |
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10.1016/j.gsf.2015.12.005 doi (DE-627)DOAJ078335728 (DE-599)DOAJ0cfde92f1c6d48c6a967cdaf687d44af DE-627 ger DE-627 rakwb eng QE1-996.5 Wei Yan verfasserin aut Micropaleontology and palaeoclimate during the early Cretaceous in the Lishu depression, Songliao basin, Northeast China 2017 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Diverse and abundant microfossils, such as palynomorphs, algae and Ostracoda, were collected from lower Cretaceous strata of Lishu depression, located in southeastern Songliao basin, and were identified and classified in order to provide relevant, detailed records for paleoclimate research. The early Cretaceous vegetation and climate of southeastern Songliao basin have been inferred from the analysis of palynomorph genera, algae and Ostracoda of the LS1 and SW110 wells. The lower Cretaceous strata include, in ascending stratigraphic order, the Shahezi, Yingcheng and Denglouku formations. Palynological assemblages for each formation, based on biostratigraphic and statistical analyses, provide an assessment of their longitudinal variations. During deposition of the Shahezi Formation, the climate was mid-subtropical. Vegetation consisted of coniferous forest and herbage. During deposition of the Yingcheng Formation, the climate was south Asian tropical. Vegetation consisted mainly of coniferous forest and herbal shrub. In addition, fresh and saline non-marine water dominated the lacustrine setting during deposition of these formations. Deposition of the Denglouku Formation, however, occurred under a hot and dry tropical climate. The vegetation was mostly coniferous forest and lake waters became saline. Palaeoclimate variation is correlated by the lake level change and the development of sedimentary facies. Palaeoclimate contribute to the formation of hydrocarbon source rocks and reservoir. Palynomorph Palaeoclimate Early Cretaceous Lishu depression Songliao Basin Geology Tailiang Fan verfasserin aut Hongyu Wang verfasserin aut Chen Zhu verfasserin aut Zhiqian Gao verfasserin aut Xiangjie Meng verfasserin aut Yangzi Sun verfasserin aut Fan Yang verfasserin aut In Geoscience Frontiers Elsevier, 2016 8(2017), 1, Seite 93-106 (DE-627)DOAJ000091189 25889192 nnns volume:8 year:2017 number:1 pages:93-106 https://doi.org/10.1016/j.gsf.2015.12.005 kostenfrei https://doaj.org/article/0cfde92f1c6d48c6a967cdaf687d44af kostenfrei http://www.sciencedirect.com/science/article/pii/S1674987116000025 kostenfrei https://doaj.org/toc/1674-9871 Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ AR 8 2017 1 93-106 |
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10.1016/j.gsf.2015.12.005 doi (DE-627)DOAJ078335728 (DE-599)DOAJ0cfde92f1c6d48c6a967cdaf687d44af DE-627 ger DE-627 rakwb eng QE1-996.5 Wei Yan verfasserin aut Micropaleontology and palaeoclimate during the early Cretaceous in the Lishu depression, Songliao basin, Northeast China 2017 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Diverse and abundant microfossils, such as palynomorphs, algae and Ostracoda, were collected from lower Cretaceous strata of Lishu depression, located in southeastern Songliao basin, and were identified and classified in order to provide relevant, detailed records for paleoclimate research. The early Cretaceous vegetation and climate of southeastern Songliao basin have been inferred from the analysis of palynomorph genera, algae and Ostracoda of the LS1 and SW110 wells. The lower Cretaceous strata include, in ascending stratigraphic order, the Shahezi, Yingcheng and Denglouku formations. Palynological assemblages for each formation, based on biostratigraphic and statistical analyses, provide an assessment of their longitudinal variations. During deposition of the Shahezi Formation, the climate was mid-subtropical. Vegetation consisted of coniferous forest and herbage. During deposition of the Yingcheng Formation, the climate was south Asian tropical. Vegetation consisted mainly of coniferous forest and herbal shrub. In addition, fresh and saline non-marine water dominated the lacustrine setting during deposition of these formations. Deposition of the Denglouku Formation, however, occurred under a hot and dry tropical climate. The vegetation was mostly coniferous forest and lake waters became saline. Palaeoclimate variation is correlated by the lake level change and the development of sedimentary facies. Palaeoclimate contribute to the formation of hydrocarbon source rocks and reservoir. Palynomorph Palaeoclimate Early Cretaceous Lishu depression Songliao Basin Geology Tailiang Fan verfasserin aut Hongyu Wang verfasserin aut Chen Zhu verfasserin aut Zhiqian Gao verfasserin aut Xiangjie Meng verfasserin aut Yangzi Sun verfasserin aut Fan Yang verfasserin aut In Geoscience Frontiers Elsevier, 2016 8(2017), 1, Seite 93-106 (DE-627)DOAJ000091189 25889192 nnns volume:8 year:2017 number:1 pages:93-106 https://doi.org/10.1016/j.gsf.2015.12.005 kostenfrei https://doaj.org/article/0cfde92f1c6d48c6a967cdaf687d44af kostenfrei http://www.sciencedirect.com/science/article/pii/S1674987116000025 kostenfrei https://doaj.org/toc/1674-9871 Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ AR 8 2017 1 93-106 |
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Wei Yan |
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Wei Yan misc QE1-996.5 misc Palynomorph misc Palaeoclimate misc Early Cretaceous misc Lishu depression misc Songliao Basin misc Geology Micropaleontology and palaeoclimate during the early Cretaceous in the Lishu depression, Songliao basin, Northeast China |
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QE1-996.5 Micropaleontology and palaeoclimate during the early Cretaceous in the Lishu depression, Songliao basin, Northeast China Palynomorph Palaeoclimate Early Cretaceous Lishu depression Songliao Basin |
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Micropaleontology and palaeoclimate during the early Cretaceous in the Lishu depression, Songliao basin, Northeast China |
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Micropaleontology and palaeoclimate during the early Cretaceous in the Lishu depression, Songliao basin, Northeast China |
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Wei Yan |
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Wei Yan Tailiang Fan Hongyu Wang Chen Zhu Zhiqian Gao Xiangjie Meng Yangzi Sun Fan Yang |
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micropaleontology and palaeoclimate during the early cretaceous in the lishu depression, songliao basin, northeast china |
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Micropaleontology and palaeoclimate during the early Cretaceous in the Lishu depression, Songliao basin, Northeast China |
| abstract |
Diverse and abundant microfossils, such as palynomorphs, algae and Ostracoda, were collected from lower Cretaceous strata of Lishu depression, located in southeastern Songliao basin, and were identified and classified in order to provide relevant, detailed records for paleoclimate research. The early Cretaceous vegetation and climate of southeastern Songliao basin have been inferred from the analysis of palynomorph genera, algae and Ostracoda of the LS1 and SW110 wells. The lower Cretaceous strata include, in ascending stratigraphic order, the Shahezi, Yingcheng and Denglouku formations. Palynological assemblages for each formation, based on biostratigraphic and statistical analyses, provide an assessment of their longitudinal variations. During deposition of the Shahezi Formation, the climate was mid-subtropical. Vegetation consisted of coniferous forest and herbage. During deposition of the Yingcheng Formation, the climate was south Asian tropical. Vegetation consisted mainly of coniferous forest and herbal shrub. In addition, fresh and saline non-marine water dominated the lacustrine setting during deposition of these formations. Deposition of the Denglouku Formation, however, occurred under a hot and dry tropical climate. The vegetation was mostly coniferous forest and lake waters became saline. Palaeoclimate variation is correlated by the lake level change and the development of sedimentary facies. Palaeoclimate contribute to the formation of hydrocarbon source rocks and reservoir. |
| abstractGer |
Diverse and abundant microfossils, such as palynomorphs, algae and Ostracoda, were collected from lower Cretaceous strata of Lishu depression, located in southeastern Songliao basin, and were identified and classified in order to provide relevant, detailed records for paleoclimate research. The early Cretaceous vegetation and climate of southeastern Songliao basin have been inferred from the analysis of palynomorph genera, algae and Ostracoda of the LS1 and SW110 wells. The lower Cretaceous strata include, in ascending stratigraphic order, the Shahezi, Yingcheng and Denglouku formations. Palynological assemblages for each formation, based on biostratigraphic and statistical analyses, provide an assessment of their longitudinal variations. During deposition of the Shahezi Formation, the climate was mid-subtropical. Vegetation consisted of coniferous forest and herbage. During deposition of the Yingcheng Formation, the climate was south Asian tropical. Vegetation consisted mainly of coniferous forest and herbal shrub. In addition, fresh and saline non-marine water dominated the lacustrine setting during deposition of these formations. Deposition of the Denglouku Formation, however, occurred under a hot and dry tropical climate. The vegetation was mostly coniferous forest and lake waters became saline. Palaeoclimate variation is correlated by the lake level change and the development of sedimentary facies. Palaeoclimate contribute to the formation of hydrocarbon source rocks and reservoir. |
| abstract_unstemmed |
Diverse and abundant microfossils, such as palynomorphs, algae and Ostracoda, were collected from lower Cretaceous strata of Lishu depression, located in southeastern Songliao basin, and were identified and classified in order to provide relevant, detailed records for paleoclimate research. The early Cretaceous vegetation and climate of southeastern Songliao basin have been inferred from the analysis of palynomorph genera, algae and Ostracoda of the LS1 and SW110 wells. The lower Cretaceous strata include, in ascending stratigraphic order, the Shahezi, Yingcheng and Denglouku formations. Palynological assemblages for each formation, based on biostratigraphic and statistical analyses, provide an assessment of their longitudinal variations. During deposition of the Shahezi Formation, the climate was mid-subtropical. Vegetation consisted of coniferous forest and herbage. During deposition of the Yingcheng Formation, the climate was south Asian tropical. Vegetation consisted mainly of coniferous forest and herbal shrub. In addition, fresh and saline non-marine water dominated the lacustrine setting during deposition of these formations. Deposition of the Denglouku Formation, however, occurred under a hot and dry tropical climate. The vegetation was mostly coniferous forest and lake waters became saline. Palaeoclimate variation is correlated by the lake level change and the development of sedimentary facies. Palaeoclimate contribute to the formation of hydrocarbon source rocks and reservoir. |
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Micropaleontology and palaeoclimate during the early Cretaceous in the Lishu depression, Songliao basin, Northeast China |
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