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Datasets of project "Neogene Climate Evolution in Eurasia"

Mostrando recursos 1 - 20 de 549

  1. (Appendix) Oligocene to Pliocene palaeoclimate from Russia and Siberia based on carpofloras

    Popova, Svetlana; Utescher, Torsten; Gromyko, Dmitriy; Bruch, Angela A; Mosbrugger, Volker

  2. (Appendix) Oligocene to Pliocene palaeoclimate from Russia and Siberia based on carpofloras

    Popova, Svetlana; Utescher, Torsten; Gromyko, Dmitriy; Bruch, Angela A; Mosbrugger, Volker

  3. Miocene microflora and palaeoclimatic estimates of the Stetten section (Austria)

    Kern, Andrea; Harzhauser, Mathias; Mandic, Oleg; Roetzel, Reinhard; Coric, Stjepan; Bruch, Angela A; Zuschin, Martin
    Pollen analyses have been proven to possess the possibility to decipher rapid vegetational and climate shifts in Neogene sedimentary records. Herein, a c. 21-kyr-long transgression-regression cycle from the Lower Austrian locality Stetten is analysed in detail to evaluate climatic benchmarks for the early phase of the Middle Miocene Climate Optimum and to estimate the pace of environmental change. Based on the Coexistence Approach, a very clear signal of seasonality can be reconstructed. A warm and wet summer season with c. 204-236 mm precipitation during the wettest month was opposed by a rather dry winter season with precipitation of c. 9-24...

  4. Miocene microflora and palaeoclimatic estimates of the Stetten section (Austria)

    Kern, Andrea; Harzhauser, Mathias; Mandic, Oleg; Roetzel, Reinhard; Coric, Stjepan; Bruch, Angela A; Zuschin, Martin
    Pollen analyses have been proven to possess the possibility to decipher rapid vegetational and climate shifts in Neogene sedimentary records. Herein, a c. 21-kyr-long transgression-regression cycle from the Lower Austrian locality Stetten is analysed in detail to evaluate climatic benchmarks for the early phase of the Middle Miocene Climate Optimum and to estimate the pace of environmental change. Based on the Coexistence Approach, a very clear signal of seasonality can be reconstructed. A warm and wet summer season with c. 204-236 mm precipitation during the wettest month was opposed by a rather dry winter season with precipitation of c. 9-24...

  5. (Table 1) Spores and pollen abundances of the Miocene Stetten section (Austria)

    Kern, Andrea; Harzhauser, Mathias; Mandic, Oleg; Roetzel, Reinhard; Coric, Stjepan; Bruch, Angela A; Zuschin, Martin

  6. (Table 1) Spores and pollen abundances of the Miocene Stetten section (Austria)

    Kern, Andrea; Harzhauser, Mathias; Mandic, Oleg; Roetzel, Reinhard; Coric, Stjepan; Bruch, Angela A; Zuschin, Martin

  7. (Appendix A) Miocene palaeoclimatic estimates based on palynomorphs from Stetten section (Austria)

    Kern, Andrea; Harzhauser, Mathias; Mandic, Oleg; Roetzel, Reinhard; Coric, Stjepan; Bruch, Angela A; Zuschin, Martin

  8. (Appendix A) Miocene palaeoclimatic estimates based on palynomorphs from Stetten section (Austria)

    Kern, Andrea; Harzhauser, Mathias; Mandic, Oleg; Roetzel, Reinhard; Coric, Stjepan; Bruch, Angela A; Zuschin, Martin

  9. Neogene floras and palaeoclimatic estimates from various sites of South-West China

    Sun, Bai-Nian; Wu, Jing-Yu; Liu, Yu-Sheng Christopher; Ding, Su-Ting; Li, Xiang-Chuan; Xie, San-Ping; Yan, De-Fei; Lin, Zhi-Cheng
    Neogene climates and vegetation history of western Yunnan are reconstructed on the basis of known fossil plants using the Coexistence Approach (CA) and Leaf Margin Analysis (LMA). Four Neogene leaf floras from Tengchong, Jianchuan and Eryuan in southwestern China are analyzed by the CA, and the paleoclimatic data of one Miocene carpoflora from Longling and three Pliocene palynofloras from Longling, Yangyi and Eryuan are used for comparison. The Miocene vegetation of the whole of West Yunnan is subtropical evergreen broad-leaved forest, and a similar mean annual precipitation is inferred for Tengchong, Longling and Jianchuan. However, by the Late Pliocene a...

  10. Neogene floras and palaeoclimatic estimates from various sites of South-West China

    Sun, Bai-Nian; Wu, Jing-Yu; Liu, Yu-Sheng Christopher; Ding, Su-Ting; Li, Xiang-Chuan; Xie, San-Ping; Yan, De-Fei; Lin, Zhi-Cheng
    Neogene climates and vegetation history of western Yunnan are reconstructed on the basis of known fossil plants using the Coexistence Approach (CA) and Leaf Margin Analysis (LMA). Four Neogene leaf floras from Tengchong, Jianchuan and Eryuan in southwestern China are analyzed by the CA, and the paleoclimatic data of one Miocene carpoflora from Longling and three Pliocene palynofloras from Longling, Yangyi and Eryuan are used for comparison. The Miocene vegetation of the whole of West Yunnan is subtropical evergreen broad-leaved forest, and a similar mean annual precipitation is inferred for Tengchong, Longling and Jianchuan. However, by the Late Pliocene a...

  11. (Appendix 1) Neogene fossil macrofloras from four sites of South-West China

    Sun, Bai-Nian; Wu, Jing-Yu; Liu, Yu-Sheng Christopher; Ding, Su-Ting; Li, Xiang-Chuan; Xie, San-Ping; Yan, De-Fei; Lin, Zhi-Cheng

  12. (Appendix 1) Neogene fossil macrofloras from four sites of South-West China

    Sun, Bai-Nian; Wu, Jing-Yu; Liu, Yu-Sheng Christopher; Ding, Su-Ting; Li, Xiang-Chuan; Xie, San-Ping; Yan, De-Fei; Lin, Zhi-Cheng

  13. (Table 1) Neogene palaeoclimatic estimates based on eight fossil samples from South-West China

    Sun, Bai-Nian; Wu, Jing-Yu; Liu, Yu-Sheng Christopher; Ding, Su-Ting; Li, Xiang-Chuan; Xie, San-Ping; Yan, De-Fei; Lin, Zhi-Cheng

  14. (Table 1) Neogene palaeoclimatic estimates based on eight fossil samples from South-West China

    Sun, Bai-Nian; Wu, Jing-Yu; Liu, Yu-Sheng Christopher; Ding, Su-Ting; Li, Xiang-Chuan; Xie, San-Ping; Yan, De-Fei; Lin, Zhi-Cheng

  15. (Table 2) Miocene palaeoclimatic estimates based on 35 fossil floras from Northern China

    Liu, Yu-Sheng Christopher; Utescher, Torsten; Zhou, Zhekun; Sun, Bainian

  16. (Table 2) Miocene palaeoclimatic estimates based on 35 fossil floras from Northern China

    Liu, Yu-Sheng Christopher; Utescher, Torsten; Zhou, Zhekun; Sun, Bainian

  17. Early - Late Miocene palaeoclimate data and palaefloras of 48 samples from Southern China

    Yao, Yi-Feng; Bruch, Angela A; Mosbrugger, Volker; Li, Cheng-Sen
    Southern China, especially Yunnan, has undergone high tectonic activity caused by the uplift of Himalayan Mountains during the Neogene, which led to a fast changing palaeogeography. Previous study shows that Southern China has been influenced by the Asian Monsoon since at least the Early Miocene. However, it is yet not well understood how intense the Miocene monsoon system was. In the present study, 63 fossil floras of 16 localities from Southern China are compiled and evaluated for obtaining available information concerning floristic composition, stratigraphic age, sedimentology, etc. Based on such reliable information, selected mega- and micro-floras have been analysed with...

  18. Early - Late Miocene palaeoclimate data and palaefloras of 48 samples from Southern China

    Yao, Yi-Feng; Bruch, Angela A; Mosbrugger, Volker; Li, Cheng-Sen
    Southern China, especially Yunnan, has undergone high tectonic activity caused by the uplift of Himalayan Mountains during the Neogene, which led to a fast changing palaeogeography. Previous study shows that Southern China has been influenced by the Asian Monsoon since at least the Early Miocene. However, it is yet not well understood how intense the Miocene monsoon system was. In the present study, 63 fossil floras of 16 localities from Southern China are compiled and evaluated for obtaining available information concerning floristic composition, stratigraphic age, sedimentology, etc. Based on such reliable information, selected mega- and micro-floras have been analysed with...

  19. Miocene micro and macro floras from 48 samples of Southern China

    Yao, Yi-Feng; Bruch, Angela A; Mosbrugger, Volker; Li, Cheng-Sen

  20. Miocene micro and macro floras from 48 samples of Southern China

    Yao, Yi-Feng; Bruch, Angela A; Mosbrugger, Volker; Li, Cheng-Sen

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