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Daoliang Chu
China University of Geosciences
18Publications
9H-index
237Citations
Publications 18
Newest
Ting Song2
Estimated H-index: 2
(China University of Geosciences),
Jinnan Tong10
Estimated H-index: 10
(China University of Geosciences),
Li Tian7
Estimated H-index: 7
(China University of Geosciences)
... more
Abstract Immediately after the latest Permian mass extinction, bivalve faunas colonized the Permian-Triassic Transitional Beds (PTTB), especially in littoral clastic facies of South China. The Permian-Triassic (P-Tr) transitional bivalve fauna is composed of holdovers, long-term survivors and newly evolved taxa, and characterized by moderate diversity and high dominance. However, the taxonomy and ecology of this bivalve fauna of littoral clastic facies have not been well understood, especially i...
Ref 53 Source Cite this paper
Li Tian7
Estimated H-index: 7
,
Jinnan Tong10
Estimated H-index: 10
,
Yifan Xiao1
Estimated H-index: 1
... more
Abstract Shallow carbonate platforms exhibit major changes in faunal composition and facies types during the latest Permian and earliest Triassic. Although the microbialites that developed following the latest Permian mass extinction (LPME) have attracted wide attention, temporal variations in shallow-platform facies and faunas prior to the LPME have been less thoroughly studied. Here, we analyze diversity patterns and variation in skeletal composition in three Upper Permian sections from isolat...
Ref 102Cited 1 Source Cite this paper
Ying Cao (China University of Geosciences), Huyue Song7
Estimated H-index: 7
(China University of Geosciences),
Thomas J. Algeo8
Estimated H-index: 8
(University of Cincinnati)
... more
Abstract Global warming is inferred to have been one of the main causes of the Permian-Triassic (P-Tr) boundary mass extinction. Although a strong temperature rise in tropical sea-surface temperatures during the latest Permian has been documented, coeval climate changes in terrestrial sections are less well-known. Here, we analyzed multiple weathering indexes (including CIA, CIW, and PIA) for two terrestrial sections in North China (Shichuanhe and Yima), all of which show a major excursion towar...
Ref 113 Source Cite this paper
Wenchao Shu (China University of Geosciences), Jinnan Tong10
Estimated H-index: 10
(China University of Geosciences),
Li Tian7
Estimated H-index: 7
(University of Bristol)
... more
Abstract Forty-four well-preserved specimens of Kouphichnium , a typical limuloid (horseshoe crab) trackway, are reported and systematically studied for the first time from continental Upper Permian to Lower Triassic successions in North China. A new ichnotaxonomic system of Kouphichnium is proposed according to the ichnotaxobase of limuloid trackways, including simple foot imprints (T), pusher imprints (P), median impressions (M) and genal spine impressions (GS). In total, one ichnogenus and si...
Ref 69 Source Cite this paper
2017 in geology [IF: 4.63]
Huyue Song7
Estimated H-index: 7
(China University of Geosciences),
Haijun Song8
Estimated H-index: 8
(China University of Geosciences),
Thomas J. Algeo8
Estimated H-index: 8
(University of Cincinnati)
... more
Ref 29Cited 11 Source Cite this paper
Haijun Song8
Estimated H-index: 8
(China University of Geosciences),
Ganqing Jiang9
Estimated H-index: 9
(University of Nevada, Las Vegas),
Simon W. Poulton10
Estimated H-index: 10
(University of Leeds)
... more
Banded iron formations were a prevalent feature of marine sedimentation ~3.8–1.8 billion years ago and they provide key evidence for ferruginous oceans. The disappearance of banded iron formations at ~1.8 billion years ago was traditionally taken as evidence for the demise of ferruginous oceans, but recent geochemical studies show that ferruginous conditions persisted throughout the later Precambrian, and were even a feature of Phanerozoic ocean anoxic events. Here, to reconcile these observatio...
Ref 58Cited 6 Download Pdf Cite this paper
Daoliang Chu9
Estimated H-index: 9
(China University of Geosciences),
Jinnan Tong10
Estimated H-index: 10
(China University of Geosciences),
Michael J. Benton9
Estimated H-index: 9
(University of Bristol)
... more
Abstract Correlation between marine and continental Permian-Triassic (P-Tr) strata is crucial for full understanding of the nature of this global extinction event, but it has proved difficult to achieve. Here, we show that two sections in South China and North China record similar mixed continental-marine biota in the post-extinction stratigraphic interval, including conchostracans, plants, insects, marine bivalves and lingulid brachiopods. In addition, the continental P-Tr mass extinction was r...
Ref 86Cited 4 Source Cite this paper
Daoliang Chu9
Estimated H-index: 9
(China University of Geosciences),
Jinnan Tong10
Estimated H-index: 10
(China University of Geosciences),
David J. Bottjer10
Estimated H-index: 10
(University of Southern California)
... more
Abstract Evidence for microbial mats has been reported repeatedly from marine Lower Triassic rocks, but scarcely mentioned in post-mass extinction terrestrial facies. Here, we report from the terrestrial Lower Triassic Liujiagou Formation in North China the presence of five kinds of microbially induced sedimentary structures (MISS) or sedimentary surface textures, including “old elephant skin” textures, wrinkle structures, palimpsest ripples, “ Manchuriophycus ” structures and sand cracks. Terre...
Ref 122Cited 6 Download Pdf Cite this paper
2016 in geological magazine [IF: 1.97]
Haijun Song8
Estimated H-index: 8
(China University of Geosciences),
Jinnan Tong10
Estimated H-index: 10
(China University of Geosciences),
Paul B. Wignall9
Estimated H-index: 9
(University of Leeds)
... more
Survival and recovery are important dynamic processes of biotic evolution during major geological transitions. Disaster and opportunistic taxa are two significant groups that dominate the ecosystem in the aftermath of mass extinction events. Disaster taxa appear immediately after such crises whilst opportunists pre-date the crisis but also bloom in the aftermath. This paper documents three disaster foraminiferal species and seven opportunistic foraminiferal species from Lower Triassic succession...
Ref 78Cited 7 Source Cite this paper
Daoliang Chu9
Estimated H-index: 9
(China University of Geosciences),
Jianxin Yu8
Estimated H-index: 8
(China University of Geosciences),
Jinnan Tong10
Estimated H-index: 10
(China University of Geosciences)
... more
Abstract The Permian-Triassic boundary marks the greatest mass extinction during the Phanerozoic, which was coupled with major global environmental changes, and is known especially from well-preserved marine fossil records and continuous carbonate deposits. However, the placement of the Permian-Triassic boundary in terrestrial sections and accurate correlation with the marine strata are difficult due to the absence of the key marine index fossils in terrestrial-marine siliciclastic settings. Her...
Ref 110Cited 10 Download Pdf Cite this paper
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