Zobrazeno 1 - 10
of 208
pro vyhledávání: '"Gangjian Wei"'
Autor:
Kaiqiang Xu, Asfandyar Shahab, Jörg Rinklebe, He Xiao, Jieyue Li, Feng Ye, Yanhong Li, Dunqiu Wang, Michael S. Bank, Gangjian Wei
Publikováno v:
Emerging Contaminants, Vol 10, Iss 3, Pp 100383- (2024)
Microplastics (MPs) (64.12 %) of detected MPs were
Externí odkaz:
https://doaj.org/article/0c7ba7ab9b0e42c0b2472ec55534a501
Publikováno v:
Geophysical Research Letters, Vol 51, Iss 7, Pp n/a-n/a (2024)
Abstract Whether Mn carbonates can be used as a proxy for the oxygenation event is debated. Here we examined the Early Cretaceous lacustrine Mn carbonates from North China, which contain abundant microbial fossils. The extremely positive δ13C (up to
Externí odkaz:
https://doaj.org/article/67129f279aef4c309485343dfa87249f
Publikováno v:
Geochemistry, Geophysics, Geosystems, Vol 25, Iss 4, Pp n/a-n/a (2024)
Abstract The fluxes of metal cations and isotopes released by weathering of silicate rocks are crucial and a prerequisite for constraining geochemical fluxes to rivers and oceans. This study presents mineral and elemental compositions along with 87Sr
Externí odkaz:
https://doaj.org/article/3b811f67ae2d457988fe39d04a693e20
Publikováno v:
Geochemistry, Geophysics, Geosystems, Vol 25, Iss 4, Pp n/a-n/a (2024)
Abstract Understanding the stable strontium isotope fractionation between seawater and ferromanganese crusts/nodules is crucial for reconstructing seawater Sr isotopic history. This study explores stable Sr isotope fractionation during adsorption to
Externí odkaz:
https://doaj.org/article/ca074ad13ee345d8baad2b66ceba3769
Autor:
Zhibing Wang, Feng Ye, Jie Li, Jinlong Ma, Yiwei Chen, Xi Liu, Chao Huang, Ti Zeng, Gangjian Wei, Qingquan Hong
Publikováno v:
Geochemistry, Geophysics, Geosystems, Vol 25, Iss 2, Pp n/a-n/a (2024)
Abstract Understanding the geochemical behavior of the Mo isotopes in estuarine systems is essential for determining the isotopic composition of riverine inputs to the ocean and for assessing the historical oxidation state of Earth’s ancient oceans
Externí odkaz:
https://doaj.org/article/a26304bf337f42389ba537923b61b755
Publikováno v:
Geochemistry, Geophysics, Geosystems, Vol 24, Iss 12, Pp n/a-n/a (2023)
Abstract River sediments are valuable archives of the environmental conditions within their catchments. The Yangtze and Yellow Rivers are the most active fluvial systems for sediment transport in East Asia, and they are regarded as potential sediment
Externí odkaz:
https://doaj.org/article/e5e8edb92a2c4e5f8e62562b3451e12b
Autor:
Xiaoxiao Yu, Xi Mei, Jianxing Liu, Jiarui Lin, Gangjian Wei, Xuefa Shi, Jianghao Bai, Mang Lin
Publikováno v:
Geophysical Research Letters, Vol 50, Iss 16, Pp n/a-n/a (2023)
Abstract Magnetic greigite may be a valuable indicator for methane emissions in the geological past, if its formation pathway and diagenetic environment can be unambiguously defined. Here, we investigate sulfur isotopic compositions of iron sulfides
Externí odkaz:
https://doaj.org/article/c8c73cfc9a7e4c9ebc58665473375f65
Publikováno v:
Geophysical Research Letters, Vol 50, Iss 13, Pp n/a-n/a (2023)
Abstract The 4.2 ka BP Event is an abrupt climate change that might have contributed to the collapse of ancient civilizations and marks the transition between the mid‐ and late‐Holocene. Despite considerable research on this event, our understand
Externí odkaz:
https://doaj.org/article/4704b19e6312402d8f54376e3eeb3c3a
Publikováno v:
Frontiers in Earth Science, Vol 10 (2022)
Well-preserved paleo-shoreline systems suggest lake shrinkage occurred in a vast region of the Tibetan Plateau, indicating dramatic paleo-environmental changes that linked closely to variations in Asian monsoon precipitation, glacial meltwater, and e
Externí odkaz:
https://doaj.org/article/23b87eb3d18a4a95ab137c15dfd53a3d
Autor:
Jieqiong Zou, Wenfeng Deng, Xuefei Chen, Xi Liu, Yangrui Guo, Guanqiang Cai, Xiaoping Xia, Qing Yang, Yanqiang Zhang, Ti Zeng, Gangjian Wei
Publikováno v:
Solid Earth Sciences, Vol 6, Iss 2, Pp 129-141 (2021)
Oxygen isotope composition (δ18O) in Porites coral skeletons at the micrometer scale has been proposed to be uninfluenced by temperature in previous studies. Considering that temperature is the main controlling factor of coral δ18O at the macro sca
Externí odkaz:
https://doaj.org/article/2ddf4172a84549bb8e31c795cdac8e07