Global and Planetary Change
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#1Min Yang (CAS: Chinese Academy of Sciences)H-Index: 1
#2Zhongqin Li (CAS: Chinese Academy of Sciences)H-Index: 24
Last. Chunhai Xu (CAS: Chinese Academy of Sciences)H-Index: 6
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Abstract null null Glaciers, as massive freshwater reservoirs, support the planet's living systems and have an impact on our daily lives, even for communities living far away. Ongoing and future climate change is predicted to have strong impacts on the mass balance of alpine glacier around the world. To understand the relationship between climate and glacier dynamics, a range of mass balance models are currently used. Most of these models however, ignore subsurface heat fluxes as a component of ...
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#1Xinchun Liu (CDUT: Chengdu University of Technology)H-Index: 2
#2Mingcai HouH-Index: 6
Last. Yu LiuH-Index: 1
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#2Xianguo Lang (CDUT: Chengdu University of Technology)H-Index: 11
Last. Bing ShenH-Index: 13
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#1Ying Liu (CAS: Chinese Academy of Sciences)H-Index: 6
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#1Thomas M. HoyleH-Index: 4
#2Suzanne A.G. Leroy (University of Liverpool)H-Index: 3
Last. V. Aghayeva (University of Leoben)H-Index: 1
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Abstract null null Marine influence on low-salinity environments can trigger aquatic ecosystem shifts, including biodiversity turnovers. High-resolution palaeoenvironmental records of marine connection events are particularly valuable, as they provide natural laboratories to understand analogous oceanographic and biodiversity turnover events in present-day climate- and anthropogenically-induced incursions. One such incursion event occurred across the Plio-Pleistocene transition when water from t...
1 CitationsSource
#1Huan CuiH-Index: 14
#2Kouki Kitajima (UW: University of Wisconsin-Madison)H-Index: 22
Last. John H. Fournelle (UW: University of Wisconsin-Madison)H-Index: 27
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Abstract null null The Ediacaran Period (ca. 635–539 Ma) witnessed the earliest paleontological evidence for macroscopic life (i.e., Ediacara biota) and geochemical observations of the largest carbon cycle anomaly in Earth history (i.e., Shuram Excursion, SE). Numerous hypotheses have been proposed for the origins of the SE, ranging from primary seawater anomaly to syn- or post-depositional diagenesis. Despite intensive geochemical and theoretical work published in the past decade, empirical evi...
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#1Maria Rose Petrizzo (University of Milan)H-Index: 27
#2David K. Watkins (NU: University of Nebraska–Lincoln)H-Index: 21
Last. Tomonori Kato (Kanazawa University)
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Abstract null null Planktonic foraminiferal population dynamics and benthic foraminiferal and radiolaria distributions combined with δ13C and δ18O measurements of both bulk carbonate and foraminifera provide clues concerning the paleoceanographic changes across the Cenomanian-Turonian boundary interval and the Oceanic Anoxic Event 2 (OAE 2) at southern high latitudes. Samples analyzed are from Integrated Ocean Discovery Program (IODP) Expedition 369 Site U1516 in the Mentelle Basin (eastern flan...
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#1Lucas Vimpere (University of Geneva)H-Index: 1
#2Stephen E. Watkins (University of Geneva)H-Index: 4
Last. Sébastien Castelltort (University of Geneva)H-Index: 20
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Abstract null null The global occurrence of parabolic dunes and their reactivation potential make them significant features in the present global landscape. Several studies have assessed the distribution and structure of parabolic dunes and their relationship to local climate factors with the aim to constrain the processes influencing their activation and potential reactivation. However, none of them have addressed the connection between recently active inland parabolic dunes and climatic condit...
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#1D. Ravidà (FAU: University of Erlangen-Nuremberg)
#2Luca Caracciolo (FAU: University of Erlangen-Nuremberg)H-Index: 13
Last. Harald Stollhofen (FAU: University of Erlangen-Nuremberg)H-Index: 28
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Abstract null null Reconstructing sediment load in deep-time is one of the greatest challenges in the reconstruction of ancient sediment routing systems, particularly because solid statistical models are absent and paleo-climatic, paleo-tectonic, and sedimentary constraints are lacking. This study proposes a reliable workflow for the estimation of paleo-sediment fluxes (Qs) applying the BQART model to a case study from the SE Germanic Basin across the Middle Permian – Early Triassic interval. Th...
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