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Research Highlights
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Research Highlights
Research Highlights
GRL:Scaling the Mixing Efficiency of Sediment-stratified Turbulence
Junbiao Tu1, Daidu Fan 1*, Zhiyu Liu2, William Smyth3*1State Key Laboratory of Marine Geology, Tongji University, Shanghai, China2State Key Laboratory of Marine Environmental Science, and Department of Physical Oceanography, College of Ocean and Earth Sciences, Xiamen University, Xiamen, China,3College of Oceanic and Atmospheric Sciences, Oregon State University, Corvallis, Oregon, USAAbstract:The flux Richardson number Rf, also called the mixing efficiency of stratified turbulence, is important
2022-09-29
82
PNAS:Atmospheric forcing dominates winter Barents-Kara sea ice variability on interannual to decadal timescales
Zhongfang Liua,1, Camille Risib, Francis Codronc, Zhimin Jiana, Zhongwang Weid, Xiaogang Hee, Christopher J. Poulsenf, Yue Wanga, Dong Cheng, Wentao Mah, YanyanChengi and Gabriel J. BowenjaState Key Laboratory of Marine Geology, Tongji University, Shanghai 200092, China; bLaboratoire de Météorologie Dynamique, IPSL, CNRS, Sorbonne Université, Paris 75252, France; cLOCEAN, Sorbonne Université, Paris 75252, France; dGuangdong Province Key Laboratory for Climate Change and Natural Disaster Studies,
2022-09-02
116
GRL:In situ observation of a magnetopause indentation that is correspondent to throat aurora and is caused by magnetopause reconnection
HuiXuan Qiu1, De-Sheng Han1*, BoYi Wang2, HuiTing Feng1, Bin Li3, Su Zhou4, Run Shi1, HuiGen Yang3,1, and Y-L. Zhang51State Key Laboratory of Marine Geology, School of Ocean and Earth Science, Tongji University, Shanghai, China2Institute of Space Science and Applied Technology, Harbin Institute of Technology, Shenzhen, China3MNR Key Laboratory for Polar Science, Polar Research Institute of China, Shanghai, China 4School of Electronics and Communication Engineering, Guiyang University, Guiyang, C
2022-08-20
418
Tectonophysics:The role of fault interaction in earthquake migration in Central Sulawesi, Indonesia
Chang Liua,b, Yaolin Shi caState Key Laboratory of Marine Geology, Tongji University, Shanghai, ChinabShanghai Sheshan National Geophysical Observatory, ChinacKey Laboratory of Computational Geodynamics, Chinese Academy of Sciences, Beijing, ChinaAbstractOver the past 50years, a sequence of destructive earthquakes, such as the 1968 (Mw 7.2), 1996 Tonimi (Mw 7.9), and 2018 Palu (Mw 7.5) earthquakes, occurred on the Palu-Koro strike-slip fault and the Minahassa Megathrust, which caused catastrophi
2022-08-19
87
QSR:Origin of the long-term increase in coccolith size and its implication for carbon cycle and climate over the past 2 Myr
Xiaobo Jin a, Wentao Ma b, c, Chuanlian Liu aaState Key Laboratory of Marine Geology, Tongji University, Shanghai, ChinabState Key Laboratory of Satellite Ocean Environment Dynamics, Second Institute of Oceanography, Ministry of Natural Resources, Hangzhou, ChinacSouthern Marine Science and Engineering Guangdong Laboratory (Zhuhai), Zhuhai, ChinaAbstract: A long-term increase in coccolith size over the Pleistocene has long been discovered in global oceans. Such a long-term and evolutionary chang
2022-07-24
205
EPSL:Highly heterogeneous mantle caused by recycling of oceanic lithosphere from the mantle transition zone
Shengping Qiana,Vincent Saltersb,Alex J. McCoy-Westc,Jonny Wud,Estelle F. Rose-Kogae,Alexander R. L. Nicholsf,Le Zhangg,Huaiyang Zhoua,Kaj Hoernlehia State Key Laboratory of Marine Geology, Tongji University, Shanghai, Chinab Depart. of Earth Ocean and Atmospheric Science and NHMFL, Florida State University, Tallahassee, USAc Isotropics Geochemistry Laboratory, School of Earth and Environmental Science, James Cook University, Townsville, Australiad Depart. of Earth Atmospheric Sciences, Univers
2022-07-15
203
Earth-Science Reviews:Opposite thrust systems under the Subei- South Yellow Sea Basin: A synthesis on the closure of the eastern Tethyan Ocean
Panpan Hua,b, Fengli Yanga,b,*, Sanzhong Lic,d, Ruoyu Zhanga,b, Bin Nib, Erkang Qiua,e, Yanhui Suoc,da State Key Laboratory of Marine Geology, Tongji University, 1239 Siping Rd. Shanghai, 200092, Chinab School of Ocean and Earth Science, Tongji University, 1239 Siping Rd. Shanghai 200092, Chinac Frontiers Science Center for Deep Ocean Multispheres and Earth System, Key Lab of Submarine Geosciences and Prospecting Techniques, MOE and College of Marine Geosciences, Ocean University of China, Qingd
2022-07-06
194
QSR: Sea level change and Kuroshio intrusion dominated Taiwan sediment source-to-sink processes in the northeastern South China Sea over the past 244 kyrs
Chi Zhang a, Shouye Yang a, *, Xiangtong Huang a, *, Yanguang Dou b, Fangliang Li a, Xinning Xu a, Qiang Hao a, Jianhua Gao caState Key Laboratory of Marine Geology, Tongji University, Shanghai 200092, ChinabKey Laboratory of Marine Hydrocarbon Resources and Environmental Geology, Qingdao Institute of Marine Geology, Ministry of Natural Resources, Qingdao 266071, ChinacSchool of Geography and Ocean Science, Nanjing University, Nanjing 210023, ChinaAbstractThe terrigenous sediment source-to-sink
2022-06-29
220
GCA: Archaeal tetraether lipids and their biphytane carbon isotope composition in sediments along an estuarine biogeochemical gradient
Juan He a, Jiayuan Jia a, Wei Guo b, Guodong Jia a,c,*aState Key Laboratory of Marine Geology, Tongji University, Shanghai, ChinabCollage of Water Resources and Environmental Engineering, East China University of Technology, Nanchang, ChinacSouthern Marine Science and Engineering Guangdong Laboratory (Zhuhai), ChinaAbstractThe stable carbon isotopic composition of Thaumarchaeota-produced crenarchaeol (δ13Ccren) is thought to reflect the δ13C of dissolved inorganic carbon (DIC) and is valuable in
2022-06-23
163
GRL:Exploring the deep ocean single-frequency microseisms southwest of Japan in northern Philippine Sea
Bin Huang 1, Mei Xue 1,2, Zhen Guo 3,4, and Wenkai Song 1,51State Key Laboratory of Marine Geology, School of Ocean and Earth Science, Tongji University, Shanghai, China.2Shanghai Sheshan National Geophysical Observatory, Shanghai, China. 3College of Civil Engineering, Tongji University, Shanghai, China.4Key Laboratory of Geotechnical and Underground Engineering of the Ministry of Education, Tongji University, Shanghai, China.5Now at Department of Earth and Planetary Sciences, The University of
2022-06-17
175
Nature Communications: A global temperature control of silicate weathering intensity
Kai Deng1,2*, Shouye Yang1*, Yulong Guo11 State Key Laboratory of Marine Geology, Tongji University, 200092 Shanghai, China2 Institute of Geochemistry and Petrology, Department of Earth Sciences, ETH Zürich, Clausiusstrasse 25, 8092 Zürich, SwitzerlandAbstractSilicate weathering as an important negative feedback can regulate the Earth’s climate over time, but much debate concerns its response strength to each climatic factor and its evolution with land surface reorganisation. Such discrepancy ar
2022-04-06
230
Sedimentology: The role of mass-transport complexes (MTCs) in the initiation and evolution of submarine canyons
近日,国际沉积学家协会(IAS)期刊Sedimentology《沉积学》以“The role of mass‐transport complexes in the initiation and evolution of submarine canyons”为题发表了海洋地质国家重点实验室吴南研究员与合作者的研究成果。海底滑坡广泛分布在陆架—陆坡—深海体系中,其搬运过程对海底地层侵蚀能力非常强,因此海底滑坡不仅可以改变陆架形态,还可以携带大量沉积物从陆架地区搬运并沉积至深海盆地。因此,海底滑坡在海洋沉积源汇系统中扮演着重要角色,是深海沉积系统中重要的沉积物之一。然而,以往针对海底滑坡与其他沉积体系相互作用的研究多局限于单一讨论海底滑坡与深海浊流水道、海底滑坡与深海峡谷体系、或海底滑坡与底流之间相互作用关系,缺乏对海底滑坡与浊流—底流—深海峡谷系统之间相互作用机理的整合研究。针对以上问题,该研究在澳大利亚板块东南缘深海Otway Basin中(如图1所示)探讨现代海底滑坡与深海底流、浊流、和峡谷沉积体系之间相互作用机制。图1.研究区地理位置图。研究区陆架—陆坡地区发育众多大型海底滑坡,海底
2022-04-06
197
GRL:Seismic anisotropy within the subducting northern Philippine Sea plate, SW Japan, using DONET seafloor observation network
Y. Liul, M. Xuel3, Z. Guo2, Ailan Zhu31State Key Laboratory of Marine Geology, Tongji University, Shanghai, China,200092.2College of Civil Engineering, Tongii University, Shanghai, China,200092.3Shanghai Sheshan National Geophysical Observatory, Shanghai, China.AbstractAnisotropy within subducted slabs carries important information about the deformation history of the slabs. Seismic waves propagating a long distance within a subducted slab can be utilized to invert for the slab anisotropy. The D
2022-04-06
204
EPSL:Responses of silicate weathering intensity to the Pliocene-Quaternary cooling in East and Southeast Asia
FangliangLiabShouyeYangaDaniel O.BreeckerbEvan J.Ramosb XiangtongHuangaZongqiDuancdYulongGuoaChaoLiaXiMeieaState Key Laboratory of Marine Geology, Tongji University, Shanghai, ChinabDepartment of Geological Sciences, University of Texas at Austin, Austin, TX, USAcInstitute of Geographic Sciences and Natural Resources Research, Beijing, ChinadGeographical Society of China, Beijing, ChinaeQingdao Institute of Marine Geology, Qingdao, ChinaAbstractSilicate weathering plays a key role in maintaining
2022-04-02
177
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