Article
Geography, Physical
Xin Wei, Jianbo Liu, Renbin Zhan, Zhiqiang Zhou, Guanzhou Yan
Summary: This study reviewed the available data on the distribution of Middle-early Late Ordovician trilobites in South China and analyzed their diversity dynamics. The results revealed three macroevolutionary phases and three faunal turnovers. Changes in sea level and substrate conditions played a significant role in the faunal replacements. The radiation of trilobites was primarily influenced by the development and expansion of the Whiterock Fauna, with a shift towards outer platform environments over time. Climate cooling, substrate conditions, and increased oxygen levels and nutrients likely provided favorable conditions for trilobite radiation during the Middle Ordovician.
PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY
(2024)
Article
Geosciences, Multidisciplinary
Taniel Danelian, Claude Monnet
Summary: Based on a comprehensive dataset of middle Cambrian to Silurian radiolarian occurrences, this study investigates the diversity patterns and taxonomic evolution of radiolarian species. The research highlights significant changes in radiolarian diversity during the Darriwilian, possibly related to global changes and Earth's climate. Despite robust long-term trends in radiolarian biodiversity, the documented patterns are partly influenced by uneven sampling through space and time.
EARTH-SCIENCE REVIEWS
(2021)
Article
Ecology
Facheng Ye, Maria Aleksandra Bitner, Guang Rong Shi
Summary: Based on the latest global database of living brachiopods, this study found that about 59% of brachiopod species have smooth shells and there is no statistically significant linear trend between shell ornamentation index, latitudes, and water depths. These findings contrast with the patterns observed in fossil brachiopods and can be attributed to various factors including habitat selection and adaptation strategies rather than predation pressure.
ECOLOGY AND EVOLUTION
(2023)
Article
Geosciences, Multidisciplinary
Yiying Deng, Junxuan Fan, Shuhan Zhang, Xiang Fang, Zhongyang Chen, Yukun Shi, Haiwen Wang, Xinbing Wang, Jiao Yang, Xudong Hou, Yue Wang, Yuandong Zhang, Qing Chen, Aihua Yang, Ru Fan, Shaochun Dong, Huiqing Xu, Shuzhong Shen
Summary: The study utilized high-resolution chronostratigraphy to reveal two major biological events in the early Paleozoic era: GOBE and LOME. GOBE started in the early Ordovician and ended at the Darriwilian boundary, consisting of two major radiation phases; while the Late Ordovician witnessed two extinction events resulting in a regional species loss of approximately 67%.
EARTH-SCIENCE REVIEWS
(2021)
Article
Geosciences, Multidisciplinary
Linna Zhang, Junxuan Fan, Bo Wang, Yuandong Zhang, Jianbo Liu, Hao Huang, Qing Chen
Summary: High-resolution, quantitative paleogeographical reconstruction based on geological big data and GIS is crucial for visualizing regional and global paleogeographical features and their evolution, as well as understanding the interaction of lithosphere, hydrosphere, and biosphere. This study collected and standardized a comprehensive dataset of 807 Ordovician sections in South China, and reconstructed lithofacies paleogeographical maps and stratigraphical thickness isopach maps for ten consecutive time intervals. Precise timing and processes of land-sea distribution and basin basement transformation were revealed, showing distinct paleogeographical processes among different terranes. The study recognized a new evolutionary process of the paleogeographical pattern in South China and provided insights into depositional centers, provenance regions, and the effects of tectonic movement and sea-level changes.
EARTH-SCIENCE REVIEWS
(2023)
Article
Geography, Physical
Chengsheng Jin, Zhiwei Liao, Gary G. Lash
Summary: The study suggests that fluctuations in redox conditions, in addition to commonly cited thresholds of bimetal ratios, may have influenced the redox trends during the Ordovician-Silurian transitional interval. The strong correlation between changing redox conditions and fossil distributions implies that dynamic and ferruginous conditions contributed to biotic crises. The coupling of total organic carbon (TOC) and redox proxies highlights the importance of prolonged anoxia or euxinia in the accumulation and preservation of organic matter.
PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY
(2021)
Article
Geography, Physical
Yangbo Lu, Jun Shen, Yuxuan Wang, Yongchao Lu, Thomas J. Algeo, Shu Jiang, Detian Yan, Qiyang Gou
Summary: The Late Ordovician mass extinction (LOME) occurred in two discrete pulses, linked to environmental stresses caused by the onset and termination of the Hirnantian Glaciation. Recent studies have suggested a potential connection between LOME and massive volcanism during the Ordovician-Silurian transition (OST), based on significant mercury anomalies in the South China region. However, the study finds that volcanic activity in South China during the OST was a regional phenomenon, and there is a discrepancy between the distribution of bentonite beds and the overall redox evolution in the region. Mercury isotope analysis suggests that seawater was the source of mercury enrichment during the OST. Therefore, the LOME may not have been caused by massive volcanism, but rather by long-term cooling, weathering, anoxia, and marine eutrophication.
PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY
(2022)
Article
Biology
Xiang Fang, Yingyan Mao, Qi Liu, Wenwei Yuan, Zhongyang Chen, Rongchang Wu, Lixia Li, Yuchen Zhang, Junye Ma, Wenhui Wang, Renbin Zhan, Shanchi Peng, Yuandong Zhang, Diying Huang
Summary: This article reports on a new tropical Lagerstatte, Liexi fauna, which has been recently discovered in the Lower Ordovician carbonate succession in western Hunan, South China. The fauna contains a variety of soft tissues and shelly fossils, including Cambrian relics and Ordovician taxa, revealing a complex marine ecosystem and providing new evidence for understanding the macroevolution and onset of the GOBE in the Ordovician.
PROCEEDINGS OF THE ROYAL SOCIETY B-BIOLOGICAL SCIENCES
(2022)
Article
Geography, Physical
Min Li, Qingyong Luo, Jianfa Chen, Shengbao Shi, Jiajia Yang, Xuemin Xu, Jing Qin, Yangyang Wang, Qingwei Dong
Summary: The study revealed a significant shift in nitrogen isotopes from the Wufeng Formation to the Longmaxi Formation in the Yangtze Sea region, indicating changes in oceanic redox conditions. This suggests that the nitrogen cycle perturbation during the pre- and post-Hirnantian intervals was directly related to environmental changes, with anaerobic processes dominating the nitrogen cycle in the Wufeng Formation and denitrification and anaerobic processes playing a more important role in the Longmaxi Formation. Nitrogen isotopes serve as a reliable indicator of paleoenvironmental changes and are valuable for understanding paleodepositional conditions and global geological events during the Ordovician-Silurian period.
PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY
(2021)
Article
Geosciences, Multidisciplinary
Xueying Ma, James Ogg, Yuanzheng Lu, Ru Fan, Chunju Huang, Zhong Luo, Shenghui Deng
Summary: This study surveyed and sampled the Upper Ordovician sections on the Upper Yangtze Platform, and identified a positive 813C excursion, the Pagoda Positive 813C Excursion (PPCE), through geochemo-bio-cyclostratigraphy evidences. Spectral analysis of high-resolution magnetic susceptibility logs showed consistent wavelengths, and the duration of the PPCE event was determined to be 3.7 to 4.4 million years. This is the first documentation of the PPCE event on the Upper Yangtze Platform, revising the previous description.
JOURNAL OF ASIAN EARTH SCIENCES
(2022)
Article
Geosciences, Multidisciplinary
Jixin Jia, Xuebin Du, Ke Zhao, Yongchao Lu, Chao Tan
Summary: During the Ordovician-Silurian transition, large-scale explosive volcanism occurred globally, including in South China. The tectonic activities leading to this volcanism in the South China Block, particularly on the northern and southern margins, are still debated. Through the analysis of the sources of K-bentonite layers in South China during this transition, it is revealed that there were two different sources of volcanic activity, suggesting different geodynamic settings, including within-plate extension and subduction-collision processes.
MARINE AND PETROLEUM GEOLOGY
(2022)
Article
Geography, Physical
Juwan Jeon, Yue Li, Stephen Kershaw, Zhongyang Chen, Junye Ma, Jeong-Hyun Lee, Kun Liang, Shenyang Yu, Bing Huang, Yuandong Zhang
Summary: Microfacies analysis of upper Hirnantian carbonates in northeastern Guizhou province, China reveals the composition and biodiversity during this period, suggesting the presence of diverse warm-water biota. The development of these organisms may be attributed to localized favorable environmental conditions.
PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY
(2022)
Article
Geography, Physical
Yangbo Lu, Fang Hao, Detian Yan, Yongchao Lu
Summary: The study conducted on bentonite beds-bearing intervals from the Upper Ordovician Wufeng Formation in South China reveals the short-term and long-term impacts of volcanic activity on the paleoenvironment. Short-term effects include environmental disruptions such as ocean fertilization and warmer climate, while the long-term effects show a correlation between distribution of bentonite beds and global sea-level fluctuations, suggesting a cumulative heating effect from intense volcanic activities in South China.
PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY
(2021)
Article
Multidisciplinary Sciences
Xin Men, Chuanlong Mou, Xiangying Ge
Summary: The Ordovician-Silurian transition was a critical period in geological history, characterized by significant changes in climate, biota, and oceanic conditions. Through a detailed analysis of formations in the Sichuan Basin, this study provides insights into the provenance, paleoclimate, and paleoredox conditions during the Late Ordovician-early Silurian. The results highlight the influence of collisional settings on the provenance, fluctuations in climate, and shifts in oceanic redox conditions, offering valuable information about the timing of the Late Ordovician mass extinction and its relationship with climatic and oceanic changes.
SCIENTIFIC REPORTS
(2022)
Article
Geochemistry & Geophysics
Jun Shen, Thomas J. Algeo, Qinglai Feng
Summary: High mercury concentrations in the Ordovician-Silurian transition sections of South China come from the uptake of mercury from seawater. Mercury isotope studies support a marine source, ruling out a volcanic source. Local environmental conditions play a dominant role in mercury enrichment in the South China strata.
EARTH AND PLANETARY SCIENCE LETTERS
(2022)
Article
Paleontology
Colin D. Sproat, Jisuo Jin, Ren-Bin Zhan, David M. Rudkin
Article
Geography, Physical
Colin D. Sproat, Jisuo Jin
PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY
(2017)
Article
Geography, Physical
Cale A. C. Gushulak, Jisuo Jin
PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY
(2017)
Article
Geology
Jisuo Jin, Akbar Sohrabi, Colin Sproat
Article
Geology
David Alexander Taylor Harper, Jisuo Jin, Christian Mac Orum Rasmussen
Article
Zoology
Renbin Zhan, Jisuo Jin
INTEGRATIVE ZOOLOGY
(2014)
Article
Paleontology
Yan Liang, Renbin Zhan, Jisuo Jin
Article
Geology
Paul Copper, Jisuo Jin
NEWSLETTERS ON STRATIGRAPHY
(2014)
Article
Paleontology
Renbin Zhan, David A. T. Harper, Jisuo Jin, Yan Liang, Jianbo Liu, Lars Stemmerik, Svend Stouge
Article
Paleontology
Guang-Xu Wang, Zheng-Fu Guo, Ren-Bin Zhan, Ji-Suo Jin
Article
Paleontology
Ren Bin Zhan, Jia Yu Rong, Ji Suo Jin, Yan Liang, Wen Wei Yuan, Yuan Dong Zhang, Yi Wang
Article
Paleontology
Jisuo Jin, Robert B. Blodgett
JOURNAL OF PALEONTOLOGY
(2020)
Article
Paleontology
Jisuo Jin, Robert B. Blodgett, David A. T. Harper, Christian M. O. Rasmussen
Summary: The Late Ordovician Tcherskidium fauna, characterized by large and ribbed shells, was mainly distributed in the paleoequatorial and northern paleotropical zones, while the Southern Hemisphere was influenced by cold-water invasions.
JOURNAL OF PALEONTOLOGY
(2022)
Article
Paleontology
Joshua B. Zimmt, Jisuo Jin
Summary: This study reports a new species, Hirnantia notiskuani, from the lower Ellis Bay Formation in Anticosti Island. It is similar to the type species, H. sagittifera, but has distinct differences. The findings indicate that the entire Ellis Bay Formation is of Hirnantian age.
JOURNAL OF PALEONTOLOGY
(2023)
Article
Paleontology
Jisuo Jin, Jose Santamaria, Donald Mikulic, Timothy Chowns
Summary: A study found that fossils from Georgia, Tennessee, Illinois, and New York provide evidence of the distribution of a brachiopod species called Platymerella in a subtropical and tropical cool-water environment during the early Silurian period. Compared to other regions, these fossils have flatter shape and thicker shells.
JOURNAL OF PALEONTOLOGY
(2023)