Through a comprehensive study of magnetostratigraphy and sedimentology of several basins in the northeastern Tibetan Plateau,we reveal that the study area mainly experienced six tectonic uplift stages at approximately...Through a comprehensive study of magnetostratigraphy and sedimentology of several basins in the northeastern Tibetan Plateau,we reveal that the study area mainly experienced six tectonic uplift stages at approximately 52 Ma,34-30 Ma,24-20 Ma,16-12 Ma,8-6 Ma,and 3.6-2.6 Ma.Comprehensive analyses of pollen assemblages from the Qaidam,Linxia,Xining,and West Jiuquan Basins show that the northeastern Tibetan Plateau has undergone six major changes in vegetation types and climate：50-40 Ma for the warm-humid forest vegetation,40-23 Ma for the warm-arid and temperate-arid forest steppe vegetation,23-18.6 Ma for the warm-humid and temperate-humid forest vegetation,18.6-8.5 Ma for the warm-humid and cool-humid forest steppe vegetation,8.6-5 Ma for the temperate sub-humid savanna steppe vegetation,and 5-1.8 Ma for the cold-arid steppe vegetation.Comprehensive comparisons of tectonic uplift events inferred from sedimentary records,climatic changes inferred from pollen,and global climate changes show that in the northeastern Tibetan Plateau the climate in the Paleogene at low altitude was mainly controlled by the global climate change,while that in the Neogene interval with high altitude landscapes of mountains and basins is more controlled by altitude and morphology.展开更多
Objective Located at the interface of terrestrial and marine ecosystems, mangroves are particularly sensitive to environmental changes. They provide a sedimentary sink for organic carbon, whereby core samples could p...Objective Located at the interface of terrestrial and marine ecosystems, mangroves are particularly sensitive to environmental changes. They provide a sedimentary sink for organic carbon, whereby core samples could provide detailed records of mangrove evolution. Human induced, rapid environmental changes in recent years require a better understanding of the mangrove ecosystems evolution in the past, by reconstructing the past mangrove dynamics using triterpenols recorded in sediments. The aim of our work is to improve the application of triterpenols as biomarkers for mangrove development in long term in China.展开更多
基金supported by Foundation of Geological Survey of China (no. 1212011121261)the State Key Laboratory of Biogeology and Environmental Geology, China University of Geosciences (no. GBL11307)
文摘Through a comprehensive study of magnetostratigraphy and sedimentology of several basins in the northeastern Tibetan Plateau,we reveal that the study area mainly experienced six tectonic uplift stages at approximately 52 Ma,34-30 Ma,24-20 Ma,16-12 Ma,8-6 Ma,and 3.6-2.6 Ma.Comprehensive analyses of pollen assemblages from the Qaidam,Linxia,Xining,and West Jiuquan Basins show that the northeastern Tibetan Plateau has undergone six major changes in vegetation types and climate：50-40 Ma for the warm-humid forest vegetation,40-23 Ma for the warm-arid and temperate-arid forest steppe vegetation,23-18.6 Ma for the warm-humid and temperate-humid forest vegetation,18.6-8.5 Ma for the warm-humid and cool-humid forest steppe vegetation,8.6-5 Ma for the temperate sub-humid savanna steppe vegetation,and 5-1.8 Ma for the cold-arid steppe vegetation.Comprehensive comparisons of tectonic uplift events inferred from sedimentary records,climatic changes inferred from pollen,and global climate changes show that in the northeastern Tibetan Plateau the climate in the Paleogene at low altitude was mainly controlled by the global climate change,while that in the Neogene interval with high altitude landscapes of mountains and basins is more controlled by altitude and morphology.
基金granted by the National Natural Science Foundation of China(grants No.41306064 and 41376075)
文摘Objective Located at the interface of terrestrial and marine ecosystems, mangroves are particularly sensitive to environmental changes. They provide a sedimentary sink for organic carbon, whereby core samples could provide detailed records of mangrove evolution. Human induced, rapid environmental changes in recent years require a better understanding of the mangrove ecosystems evolution in the past, by reconstructing the past mangrove dynamics using triterpenols recorded in sediments. The aim of our work is to improve the application of triterpenols as biomarkers for mangrove development in long term in China.
