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Research Highlights
Research Highlights
Nature Communications: 3D architecture and complex behavior along the simple central San Andreas fault
Yifang Cheng,1,2,3,4* Roland Bürgmann,2,3Richard M. Allen2,31State Key Laboratory of Marine Geology, Tongji University, Shanghai, China2 Department of Earth and Planetary Science, University of California, Berkeley, CA, USA3Berkeley Seismological Laboratory, University of California, Berkeley, Berkeley, California, U.S.A.4School of Ocean and Earth Science, Tongji University, Shanghai, ChinaAbstract:The central San Andreas Fault (CSAF) exhibits a simple linear large-scale fault geometry, yet seis
2024-06-27
15
GPC: Particle size shapes prokaryotic communities and vertical connectivity in the water columns of the slope and central basin of the South China Sea
Zhonglin Maa, Paraskevi Marab, Lei Sua, Long Wangc, Huifang Lid, Rui Zhangc,e,Virginia P. Edgcombb, Jiangtao Lia*aState Key Laboratory of Marine Geology,Tongji University, Shanghai 200092, ChinabDepartment of Geology and Geophysics, Woods Hole Oceanographic Institution, Woods Hole, MA, USAcInstitude for Advanced Study, Shenzhen University, Shenzhen 518060, ChinadSchool of Marine Science and Fisheries, Jiangsu Ocean University, Lianyungang 222005, China ESouthern Marine Science and Engineering Gu
2024-06-27
15
Geology:Turbidity currents regulate the transport and settling of microplastics in a deep-sea submarine canyon
Xiaodong Zhang1; Zhifei Liu1; Daoji Li2; Yulong Zhao1; Yanwei Zhang11State Key Laboratory of Marine Geology, Tongji University, Shanghai 200092, China2State Key Laboratory of Estuarine and Coastal Research, East China Normal University, Shanghai 200062, ChinaAbstract:Microplastics are widely distributed in deep oceans, with some of the highest concentrations reported in submarine canyons, which are thought to be closely related to turbidity currents. However, the turbidity current role in microp
2024-06-08
38
Geology: Late Oligocene−Miocene evolution of deep-water circulation in the abyssal South China Sea: Insights from Nd isotopes of fossil fish teeth
Wei Shu1,2, Christophe Colin1,*, Zhifei Liu2,*, and Arnaud Dapoigny31Géosciences Paris-Saclay (GEOPS), Université Paris-Saclay, CNRS, Orsay 91405, France 2State Key Laboratory of Marine Geology, Tongji University, Shanghai 200092, China3Laboratoire des Sciences du Climat et de L’Environnement, LSCE/IPSL, CEA-CNRS-UVSQ, Université Paris-Saclay, Gif-sur-Yvette 91191, FranceAbstract: A long-term neodymium isotope (εNd) record of fossil fish teeth was investigated to constrain the evolution of deep-
2024-06-07
32
Deep-Sea Research Part I: Oceanographic Research Papers: Radiocarbon-based ages and growth rates of cold-water bamboo corals in the South China Sea
HaozhuangWanga,XiaoliZhoua,HaowenDanga,LesWatlinga,ZhiminJianaaState Key Laboratory of Marine Geology, Tongji University, Shanghai, ChinaAbstract:Growth rates of cold-water bamboo corals are of crucial importance for establishing high-resolution chronology and reconstructing the development of these corals. However, due to the difficulty of sampling, their ages and growth rates as well as ecological indications are still fragmentary. In this study, radiocarbon analysis was performed on live-coll
2024-05-21
54
Scientific Reports: Mesoscale eddy-strengthened deep-sea topographic Rossby waves in the southwestern South China Sea
Wenzhuo Wanga, Zhifei Liua, Yulong Zhaoa, Baozhi Lina, Xiaodong Zhanga, Jingwen Zhanga, Jiaying Lia, Junyuan Caoa, Hongzhe SongaaState Key Laboratory of Marine Geology, Tongji University, Shanghai 200092, ChinaAbstract:Topographic Rossby waves (TRWs) dominate the low-frequency variability of deep ocean currents and play a crucial role in energy exchange and material mixing. On the continental slope of the southwestern South China Sea, a deep-water mooring was deployed to observe TRWs for a perio
2024-05-21
57
EPSL: Precessional forcing of biogeochemical and nutrient cycling in the tropical western Pacific during the late Pleistocene
XiaoboJina,XingxingWanga,XinquanZhoua,XiaoyingJianga,PeijunQiaoa,ChuanlianLiuaaState Key Laboratory of Marine Geology, Tongji University, Shanghai 200092, ChinaAbstract:Unravelling the biogenic material export production and its relationship to surface ocean nutrient conditions, along with their external forcing, will provide insights into the ocean carbon biogeochemical cycle. In this study, we present data on coccolith particulate inorganic carbon (PIC) export production, coccolith carbon isot
2024-05-16
45
GRL:Intermittent lobe reconnection under prolonged northward interplanetary magnetic field condition: Insights from cusp spot event observations
Xiong, Y.-Ta., Han, D.-Sa., Wang, Z.-Wa., Shi, Ra.,Feng, H.-Ta.aState Key Laboratory of Marine Geology, School of Ocean and Earth Science, Tongji University, Shanghai, ChinaAbstract:Previous studies have suggested that lobe reconnection under stable northward interplanetary magnetic field (IMF) conditions should be continuous. However, to what extent it can be considered as continuous is unknown. Auroral cusp spots have been considered a signature of lobe reconnection. Here, we show that during
2024-05-07
50
GRL:Three-Dimensional Teleseismic Elastic Reverse-Time Migration With Deconvolution Imaging Condition and Its Application to Southwest Japan
Peng Zou1,2, Jiubing Cheng1, Tengfei Wang1, Haijiang Zhang11State Key Laboratory of Marine Geology, Tongji University, Shanghai, China2School of Earth and Space Sciences, University of Science and Technology of China, Hefei, ChinaAbstract:We have developed a novel deconvolution-based reverse time migration method to image lithospheric structures using teleseismic data recorded by dense seismic arrays. Unlike traditional approaches that rely on the retrieval of Greens functions (or receiver funct
2024-04-30
22
QSR:A novel method to advance the brGDGTs-based paleoclimate reconstruction applicable to different terrestrial environments
Liping Tian a, b, 1, Mengyuan Wang c, d, 1, Cong Chen b, *, Xiao Zhang b, Zhuo Zheng b, d, Meiling Man e, Kangyou Huang b, d, Li Li a, Guodong Jia a, d, *aState Key Laboratory of Marine Geology, Tongji University, Shanghai, 200092, ChinabSchool of Earth Sciences and Engineering, Sun Yat-sen University, Zhuhai, 519082, ChinacSchool of Marine Sciences, Sun Yat-sen University, Zhuhai, 519082, ChinadSouthern Marine Science and Engineering Guangdong Laboratory (Zhuhai), Zhuhai, 519082, ChinaeDepartme
2024-04-22
28
JGR-Biogeosciences: Organic Carbon Sources in Surface Sediments on the Northern South China Sea
Baozhi Lin1, Zhifei Liu1, Timothy I. Eglinton2, MartinG. Wiesner3,4, Thomas M. Blattmann2, and Negar Haghipou2,51State Key Laboratory of Marine Geology,Tongji University, Shanghai, China,2Geological Institute, ETHZürich, Zürich, Switzerland, 3Institute of Geology, University of Hamburg, Hamburg, Germany, 4Key Laboratory of Marine Ecosystem Dynamics, Second Institute of Oceanography, Ministry of Natural Resources, Hangzhou, China, 5Laboratory of Ion Beam Physics, ETH Zürich, Zürich, SwitzerlandAb
2024-04-10
30
GCA:Lithium isotope fractionation during submarine hydrothermal alteration processes
Di Cai1*, Hebin Shao2, Long-Fei Gou3,4, Zhangdong Jin4,3Shouye Yang11. State Key Laboratory of Marine Geology, Tongji University, 1239 Siping Road, Shanghai 200092, PR China;2. Key Laboratory for Polar Science of the State Oceanic Administration, Polar Research Institute of China, Shanghai 200136, China;3. Department of Geography, Changan University, Xian 710054, China4. State Key Laboratory of Loess and Quaternary Geology, Institute of Earth Environment, Chinese Academy of Sciences, Xian 710061
2024-04-09
19
Catena: Holocene wildfire regime shifts induced by the enhancement of human activities in the Changjiang (Yangtze River) Basin
Qiang Haoab, Min Tangc, Xiangtong Huanga, Chi Zhanga, Shaohua Dang a, Shouye YangaaState Key Laboratory of Marine Geology, Tongji University, Shanghai, 200092, ChinabThe Engineering Technical College of Chengdu University of Technology, Leshan, 614000, China.cSchool of Earth Science, Yunnan University, Kunming, 650500, China.Abstract:Deforestation and technical innovation have changed the natural fire regimes, topography and carbon reservoirs during the history of human evolution. Recognition o
2024-03-29
27
Geology:Modification of Archean cratons in southern Africa with foundered segments dropped into the shallow lower mantle
Jiaji Xi1;Youqiang Yu1;Dapeng Zhao2;Jiashun Hu31State Key Laboratory of Marine Geology, Tongji University, Shanghai 200092, China2Department of Geophysics, Graduate School of Science, Tohoku University, Sendai 980-8578, Japan3Department of Earth and Space Sciences, Southern University of Science and Technology, Shenzhen 518055, ChinaAbstract:Subducted slabs have been detected in the lower mantle for almost 30 years, yet the presence of foundered cratonic segments in the lower mantle is still unc
2024-03-21
33
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