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Xiao B, Rey-lglesia A, Yuan J, Hu J, Song S, Hou Y, Chen X, Germonpré M, Bao L, Wang S, Taogetongqimuge, Valentinovna LL, Lister AM, Lai X, Sheng G. Relationships of Late Pleistocene giant deer as revealed by Sinomegaceros mitogenomes from East Asia. iScience 2023; 26:108406. [PMID: 38047074 PMCID: PMC10690636 DOI: 10.1016/j.isci.2023.108406] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 07/26/2023] [Revised: 09/26/2023] [Accepted: 11/03/2023] [Indexed: 12/05/2023] Open
Abstract
The giant deer, widespread in northern Eurasia during the Late Pleistocene, have been classified as western Megaloceros and eastern Sinomegaceros through morphological studies. While Megaloceros's evolutionary history has been unveiled through mitogenomes, Sinomegaceros remains molecularly unexplored. Herein, we generated mitogenomes of giant deer from East Asia. We find that, in contrast to the morphological differences between Megaloceros and Sinomegaceros, they are mixed in the mitochondrial phylogeny, and Siberian specimens suggest a range contact or overlap between these two groups. Meanwhile, one deep divergent clade and another surviving until 20.1 thousand years ago (ka) were detected in northeastern China, the latter implying this area as a potential refugium during the Last Glacial Maximum (LGM). Moreover, stable isotope analyses indicate correlations between climate-introduced vegetation changes and giant deer extinction. Our study demonstrates the genetic relationship between eastern and western giant deer and explores the promoters of their extirpation in northern East Asia.
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Affiliation(s)
- Bo Xiao
- State Key Laboratory of Biogeology and Environmental Geology, China University of Geosciences, Wuhan 430078, China
- School of Earth Sciences, China University of Geosciences, Wuhan 430074, China
| | - Alba Rey-lglesia
- Globe Institute, University of Copenhagen, Copenhagen, 1350 Copenhagen K, Denmark
| | - Junxia Yuan
- State Key Laboratory of Biogeology and Environmental Geology, China University of Geosciences, Wuhan 430078, China
- Faculty of Materials Science and Chemistry, China University of Geosciences, Wuhan 430078, China
| | - Jiaming Hu
- State Key Laboratory of Biogeology and Environmental Geology, China University of Geosciences, Wuhan 430078, China
- School of Earth Sciences, China University of Geosciences, Wuhan 430074, China
| | - Shiwen Song
- State Key Laboratory of Biogeology and Environmental Geology, China University of Geosciences, Wuhan 430078, China
- School of Environmental Studies, China University of Geosciences, Wuhan 430078, China
| | - Yamei Hou
- Key Laboratory of Vertebrate Evolution and Human Origins, Institute of Vertebrate Paleontology and Paleoanthropology, Chinese Academy of Sciences, Beijing 100044, China
| | - Xi Chen
- Department of Cultural Heritage and Museology, Nanjing Normal University, Nanjing 210046, China
| | - Mietje Germonpré
- Royal Belgian Institute of Natural Sciences, 1000 Brussels, Belgium
| | - Lei Bao
- Ordos Institute of Cultural Relics and Archaeology, Ordos 017010, China
| | | | | | - Lbova Liudmila Valentinovna
- Graduate School of International Relations, Peter the Great St. Petersburg Polytechnic University, St. Petersburg, Grazhdansky Av., 28, Russia
| | | | - Xulong Lai
- State Key Laboratory of Biogeology and Environmental Geology, China University of Geosciences, Wuhan 430078, China
- School of Earth Sciences, China University of Geosciences, Wuhan 430074, China
| | - Guilian Sheng
- State Key Laboratory of Biogeology and Environmental Geology, China University of Geosciences, Wuhan 430078, China
- School of Environmental Studies, China University of Geosciences, Wuhan 430078, China
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Seeber PA, Palmer Z, Schmidt A, Chagas A, Kitagawa K, Marinova-Wolff E, Tafelmaier Y, Epp LS. The first European woolly rhinoceros mitogenomes, retrieved from cave hyena coprolites, suggest long-term phylogeographic differentiation. Biol Lett 2023; 19:20230343. [PMID: 37909055 PMCID: PMC10618854 DOI: 10.1098/rsbl.2023.0343] [Citation(s) in RCA: 1] [Impact Index Per Article: 1.0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Grants] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 07/27/2023] [Accepted: 10/09/2023] [Indexed: 11/02/2023] Open
Abstract
The woolly rhinoceros (Coelodonta antiquitatis) is an iconic species of the Eurasian Pleistocene megafauna, which was abundant in Eurasia in the Pleistocene until its demise beginning approximately 10 000 years ago. Despite the early recovery of several specimens from well-known European archaeological sites, including its type specimen (Blumenbach 1799), no genomes of European populations were available so far, and all available genomic data originated exclusively from Siberian populations. Using coprolites of cave hyenas (Crocuta crocuta spelea) recovered from Middle Palaeolithic layers of two caves in Germany (Bockstein-Loch and Hohlenstein-Stadel), we isolated and enriched predator and prey DNA to assemble the first European woolly rhinoceros mitogenomes, in addition to cave hyena mitogenomes. Both coprolite samples produced copious sequences assigned to C. crocuta (27% and 59% mitogenome coverage, respectively) and woolly rhinoceros (Coelodonta antiquitatis; 27% and 81% coverage, respectively). The sequences suggested considerable DNA degradation, which may limit the conclusions to be drawn; however, the mitogenomes of European woolly rhinoceros are genetically distinct from the Siberian woolly rhinoceros, and analyses of the more complete mitogenome suggest a split of the populations potentially coinciding with the earliest fossil records of woolly rhinoceros in Europe.
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Affiliation(s)
- P. A. Seeber
- Limnological Institute, University of Konstanz, Konstanz, Germany
| | - Z. Palmer
- Limnological Institute, University of Konstanz, Konstanz, Germany
| | - A. Schmidt
- Limnological Institute, University of Konstanz, Konstanz, Germany
| | - A. Chagas
- Limnological Institute, University of Konstanz, Konstanz, Germany
| | - K. Kitagawa
- Senckenberg Centre for Human Evolution and Palaeoenvironment, University of Tübingen, Tubingen, Germany
- Institute of Archaeological Sciences, Department of Geosciences, University of Tübingen, Tubingen, Germany
| | - E. Marinova-Wolff
- Laboratory for Archaeobotany Baden-Württemberg, State Office for Cultural Heritage, Gaienhofen-Hemmenhofen, Germany
| | - Y. Tafelmaier
- State Office for Cultural Heritage Baden-Württemberg, Palaeolithic & Mesolithic Research Unit, Gaienhofen-Hemmenhofen, Germany
| | - L. S. Epp
- Limnological Institute, University of Konstanz, Konstanz, Germany
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Teng SN, Svenning JC, Xu C. Large mammals and trees in eastern monsoonal China: anthropogenic losses since the Late Pleistocene and restoration prospects in the Anthropocene. Biol Rev Camb Philos Soc 2023; 98:1607-1632. [PMID: 37102332 DOI: 10.1111/brv.12968] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 09/11/2022] [Revised: 04/16/2023] [Accepted: 04/18/2023] [Indexed: 04/28/2023]
Abstract
Massive human-induced declines of large-sized animals and trees (megabiota) from the Late Pleistocene to the Anthropocene have resulted in downsized ecosystems across the globe, in which components and functions have been greatly simplified. In response, active restoration projects of extant large-sized species or functional substitutes are needed at large scales to promote ecological processes that are important for ecosystem self-regulation and biodiversity maintenance. Despite the desired global scope of such projects, they have received little attention in East Asia. Here, we synthesise the biogeographical and ecological knowledge of megabiota in ancient and modern China, with relevant data mostly located in eastern monsoonal China (EMC), aiming to assess its potential for restoring functionally intact ecosystems modulated by megabiota. We found that during the Late Pleistocene, 12 mammalian megafaunal (carnivores ≥15 kg and herbivores ≥500 kg) species disappeared from EMC: one carnivore Crocuta ultima (East Asian spotted hyena) and 11 herbivores including six megaherbivores (≥1000 kg). The relative importance of climate change and humans in driving these losses remains debated, despite accumulating evidence in favour of the latter. Later massive depletion of megafauna and large-sized (45-500 kg) herbivores has been closely associated with agricultural expansion and societal development, especially during the late Holocene. While forests rich in large timber trees (33 taxa in written records) were common in the region 2000-3000 years ago, millennial-long logging has resulted in considerable range contractions and at least 39 threatened species. The wide distribution of C. ultima, which likely favoured open or semi-open habitats (like extant spotted hyenas), suggests the existence of mosaic open and closed vegetation in the Late Pleistocene across EMC, in line with a few pollen-based vegetation reconstructions and potentially, or at least partially, reflecting herbivory by herbivorous megafauna. The widespread loss of megaherbivores may have strongly compromised seed dispersal for both megafruit (fleshy fruits with widths ≥40 mm) and non-megafruit plant species in EMC, especially in terms of extra-long-distance (>10 km) dispersal, which is critical for plant species that rely on effective biotic agents to track rapid climate change. The former occurrence of large mammals and trees have translated into rich material and non-material heritages passed down across generations. Several reintroduction projects have been implemented or are under consideration, with the case of Elaphurus davidianus a notable success in recovering wild populations in the middle reaches of the Yangtze River, although trophic interactions with native carnivorous megafauna have not yet been restored. Lessons of dealing with human-wildlife conflicts are key to public support for maintaining landscapes shared with megafauna and large herbivores in the human-dominated Anthropocene. Meanwhile, potential human-wildlife conflicts, e.g. public health risks, need to be scientifically informed and effectively reduced. The Chinese government's strong commitment to improved policies of ecological protection and restoration (e.g. ecological redlines and national parks) provides a solid foundation for a scaling-up contribution to the global scope needed for solving the crisis of biotic downsizing and ecosystem degradation.
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Affiliation(s)
- Shuqing N Teng
- School of Life Sciences, Nanjing University, Nanjing, 210023, China
| | - Jens-Christian Svenning
- Center for Ecological Dynamics in a Novel Biosphere (ECONOVO) & Center for Biodiversity Dynamics in a Changing World (BIOCHANGE), Department of Biology, Aarhus University, Aarhus, 8000, Denmark
| | - Chi Xu
- School of Life Sciences, Nanjing University, Nanjing, 210023, China
- Key Laboratory of Restoration and Reconstruction of Degraded Ecosystems in northwestern China of Ministry of Education, Ningxia University, Yinchuan, 750021, China
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Yuan J, Sun G, Xiao B, Hu J, Wang L, Taogetongqimuge, Bao L, Hou Y, Song S, Jiang S, Wu Y, Pan D, Liu Y, Westbury MV, Lai X, Sheng G. Ancient mitogenomes reveal a high maternal genetic diversity of Pleistocene woolly rhinoceros in Northern China. BMC Ecol Evol 2023; 23:56. [PMID: 37752413 PMCID: PMC10521388 DOI: 10.1186/s12862-023-02168-0] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Grants] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 07/23/2023] [Accepted: 09/18/2023] [Indexed: 09/28/2023] Open
Abstract
BACKGROUND Woolly rhinoceros (Coelodonta antiquitatis) is a typical indicator of cold-stage climate that was widely distributed in Northern Hemisphere during the Middle-Late Pleistocene. Although a plethora of fossils have been excavated from Northern China, their phylogenetic status, intraspecific diversity and phylogeographical structure are still vague. RESULTS In the present study, we generated four mitogenomes from Late Pleistocene woolly rhinoceros in Northern China and compared them with published data. Bayesian and network analyses indicate that the analyzed individuals contain at least four maternal haplogroups, and Chinese samples fall in three of them. One of our samples belongs to a previously unidentified early diverging clade (haplogroup D), which separated from other woolly rhinoceros around 0.57 Ma (95% CI: 0.76-0.41 Ma). The timing of this clade's origin coincides with the first occurrence of woolly rhinoceros, which are thought to have evolved in Europe. Our other three samples cluster in haplogroup C, previously only identified from one specimen from Wrangel Island (ND030) and initially considered to be an isolated clade. Herein, our findings suggest that ND030 is likely descended from a northward dispersal of the individuals carrying haplogroup C from Northern China. Additionally, Chinese woolly rhinoceros specimens exhibit higher nucleotide diversity than those from Siberia. CONCLUSION Our findings highlight Northern China as a possible refugium and a key evolution center of the Pleistocene woolly rhinoceros.
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Affiliation(s)
- Junxia Yuan
- State Key Laboratory of Biogeology and Environmental Geology, China University of Geosciences, Wuhan, 430078, China.
- Bioarchaeology Laboratory, Jilin University, Changchun, 130012, China.
- Faculty of Materials Science and Chemistry, China University of Geosciences, Wuhan, 430078, China.
| | - Guojiang Sun
- State Key Laboratory of Biogeology and Environmental Geology, China University of Geosciences, Wuhan, 430078, China
- Faculty of Materials Science and Chemistry, China University of Geosciences, Wuhan, 430078, China
| | - Bo Xiao
- State Key Laboratory of Biogeology and Environmental Geology, China University of Geosciences, Wuhan, 430078, China
- School of Earth Science, China University of Geosciences, Wuhan, 430074, China
| | - Jiaming Hu
- State Key Laboratory of Biogeology and Environmental Geology, China University of Geosciences, Wuhan, 430078, China
- School of Earth Science, China University of Geosciences, Wuhan, 430074, China
| | - Linying Wang
- State Key Laboratory of Biogeology and Environmental Geology, China University of Geosciences, Wuhan, 430078, China
- Faculty of Materials Science and Chemistry, China University of Geosciences, Wuhan, 430078, China
- College of Earth and Environmental Science, Lanzhou University, Lanzhou, 730099, China
| | | | - Lei Bao
- Ordos Institute of Cultural Relics and Archaeology, Ordos, 017010, China
| | - Yamei Hou
- Key Laboratory of Vertebrate Evolution and Human Origins, Institute of Vertebrate Paleontology and Paleoanthropology, Chinese Academy of Sciences, Beijing, 100044, China
| | - Shiwen Song
- State Key Laboratory of Biogeology and Environmental Geology, China University of Geosciences, Wuhan, 430078, China
- School of Environmental Studies, China University of Geosciences, Wuhan, 430078, China
| | - Shan Jiang
- State Key Laboratory of Biogeology and Environmental Geology, China University of Geosciences, Wuhan, 430078, China
- Faculty of Materials Science and Chemistry, China University of Geosciences, Wuhan, 430078, China
| | - Yong Wu
- The Third Geological and Mineral Exploration Institute of Gansu Bureau of Geology and Mineral Resources, Lanzhou, 730050, China
| | - Dong Pan
- Palaeontological Fossil Conservation Center, Qinggang County, Suihua, 151600, China
| | - Yang Liu
- School of Sociology & Anthropology, Sun Yat-sen University, Guangzhou, 510275, China
| | | | - Xulong Lai
- State Key Laboratory of Biogeology and Environmental Geology, China University of Geosciences, Wuhan, 430078, China
- School of Earth Science, China University of Geosciences, Wuhan, 430074, China
| | - Guilian Sheng
- State Key Laboratory of Biogeology and Environmental Geology, China University of Geosciences, Wuhan, 430078, China.
- School of Environmental Studies, China University of Geosciences, Wuhan, 430078, China.
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5
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Utzeri VJ, Cilli E, Fontani F, Zoboli D, Orsini M, Ribani A, Latorre A, Lissovsky AA, Pillola GL, Bovo S, Gruppioni G, Luiselli D, Fontanesi L. Ancient DNA re-opens the question of the phylogenetic position of the Sardinian pika Prolagus sardus (Wagner, 1829), an extinct lagomorph. Sci Rep 2023; 13:13635. [PMID: 37604894 PMCID: PMC10442435 DOI: 10.1038/s41598-023-40746-w] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Grants] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 03/18/2023] [Accepted: 08/16/2023] [Indexed: 08/23/2023] Open
Abstract
Palaeogenomics is contributing to refine our understanding of many major evolutionary events at an unprecedented resolution, with relevant impacts in several fields, including phylogenetics of extinct species. Few extant and extinct animal species from Mediterranean regions have been characterised at the DNA level thus far. The Sardinian pika, Prolagus sardus (Wagner, 1829), was an iconic lagomorph species that populated Sardinia and Corsica and became extinct during the Holocene. There is a certain scientific debate on the phylogenetic assignment of the extinct genus Prolagus to the family Ochotonidae (one of the only two extant families of the order Lagomorpha) or to a separated family Prolagidae, or to the subfamily Prolaginae within the family Ochotonidae. In this study, we successfully reconstructed a portion of the mitogenome of a Sardinian pika dated to the Neolithic period and recovered from the Cabaddaris cave, an archaeological site in Sardinia. Our calibrated phylogeny may support the hypothesis that the genus Prolagus is an independent sister group to the family Ochotonidae that diverged from the Ochotona genus lineage about 30 million years ago. These results may contribute to refine the phylogenetic interpretation of the morphological peculiarities of the Prolagus genus already described by palaeontological studies.
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Affiliation(s)
- Valerio Joe Utzeri
- Department of Agricultural and Food Sciences, Division of Animal Sciences, University of Bologna, Viale Giuseppe Fanin 46, 40127, Bologna, Italy.
| | - Elisabetta Cilli
- Department of Cultural Heritage, University of Bologna, Via degli Ariani 1, 48121, Ravenna, Italy.
| | - Francesco Fontani
- Department of Cultural Heritage, University of Bologna, Via degli Ariani 1, 48121, Ravenna, Italy
| | - Daniel Zoboli
- Department of Chemical and Geological Sciences, University of Cagliari, Cittadella Universitaria SS 554, 09042, Monserrato, Italy
| | - Massimiliano Orsini
- Laboratory of Microbial Ecology, Istituto Zooprofilattico Sperimentale delle Venezie, Viale dell'università 10, 35120, Legnaro, Italy
| | - Anisa Ribani
- Department of Agricultural and Food Sciences, Division of Animal Sciences, University of Bologna, Viale Giuseppe Fanin 46, 40127, Bologna, Italy
| | - Adriana Latorre
- Department of Cultural Heritage, University of Bologna, Via degli Ariani 1, 48121, Ravenna, Italy
| | - Andrey A Lissovsky
- A.N. Severtsov Institute of Ecology and Evolution of the Russian Academy of Sciences, Moscow, Russia
| | - Gian Luigi Pillola
- Department of Chemical and Geological Sciences, University of Cagliari, Cittadella Universitaria SS 554, 09042, Monserrato, Italy
| | - Samuele Bovo
- Department of Agricultural and Food Sciences, Division of Animal Sciences, University of Bologna, Viale Giuseppe Fanin 46, 40127, Bologna, Italy
| | - Giorgio Gruppioni
- Department of Cultural Heritage, University of Bologna, Via degli Ariani 1, 48121, Ravenna, Italy
| | - Donata Luiselli
- Department of Cultural Heritage, University of Bologna, Via degli Ariani 1, 48121, Ravenna, Italy
| | - Luca Fontanesi
- Department of Agricultural and Food Sciences, Division of Animal Sciences, University of Bologna, Viale Giuseppe Fanin 46, 40127, Bologna, Italy.
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Hou X, Zhao J, Zhang H, Preick M, Hu J, Xiao B, Wang L, Deng M, Liu S, Chang F, Sheng G, Lai X, Hofreiter M, Yuan J. Paleogenomes Reveal a Complex Evolutionary History of Late Pleistocene Bison in Northeastern China. Genes (Basel) 2022; 13:genes13101684. [PMID: 36292570 PMCID: PMC9602171 DOI: 10.3390/genes13101684] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [MESH Headings] [Track Full Text] [Download PDF] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 08/17/2022] [Revised: 09/14/2022] [Accepted: 09/16/2022] [Indexed: 11/30/2022] Open
Abstract
Steppe bison are a typical representative of the Mid-Late Pleistocene steppes of the northern hemisphere. Despite the abundance of fossil remains, many questions related to their genetic diversity, population structure and dispersal route are still elusive. Here, we present both near-complete and partial mitochondrial genomes, as well as a partial nuclear genome from fossil bison samples excavated from Late Pleistocene strata in northeastern China. Maximum-likelihood and Bayesian trees both suggest the bison clade are divided into three maternal haplogroups (A, B and C), and Chinese individuals fall in two of them. Bayesian analysis shows that the split between haplogroup C and the ancestor of haplogroups A and B dates at 326 ky BP (95% HPD: 397-264 ky BP). In addition, our nuclear phylogenomic tree also supports a basal position for the individual carrying haplogroup C. Admixture analyses suggest that CADG467 (haplogroup C) has a similar genetic structure to steppe bison from Siberia (haplogroup B). Our new findings indicate that the genetic diversity of Pleistocene bison was probably even higher than previously thought and that northeastern Chinese populations of several mammalian species, including Pleistocene bison, were genetically distinct.
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Affiliation(s)
- Xindong Hou
- State Key Laboratory of Biogeology and Environmental Geology, China University of Geosciences, Wuhan 430078, China
- School of Environmental Studies, China University of Geosciences, Wuhan 430078, China
| | - Jian Zhao
- School of Environmental Studies, China University of Geosciences, Wuhan 430078, China
| | - Hucai Zhang
- Institute for Ecological Research and Pollution Control of Plateau Lakes, School of Ecology and Environmental Science, Yunnan University, Kunming 650500, China
| | - Michaela Preick
- Institute for Biochemistry and Biology, University of Potsdam, Karl-Liebknecht-Strasse 24–25, 14476 Potsdam, Germany
| | - Jiaming Hu
- State Key Laboratory of Biogeology and Environmental Geology, China University of Geosciences, Wuhan 430078, China
- School of Earth Sciences, China University of Geosciences, Wuhan 430074, China
| | - Bo Xiao
- State Key Laboratory of Biogeology and Environmental Geology, China University of Geosciences, Wuhan 430078, China
- School of Earth Sciences, China University of Geosciences, Wuhan 430074, China
| | - Linying Wang
- Faculty of Materials Science and Chemistry, China University of Geosciences, Wuhan 430078, China
| | - Miaoxuan Deng
- School of Environmental Studies, China University of Geosciences, Wuhan 430078, China
| | - Sizhao Liu
- Department of Scientific Research, Dalian Natural History Museum, Dalian 116023, China
| | - Fengqin Chang
- Institute for Ecological Research and Pollution Control of Plateau Lakes, School of Ecology and Environmental Science, Yunnan University, Kunming 650500, China
| | - Guilian Sheng
- State Key Laboratory of Biogeology and Environmental Geology, China University of Geosciences, Wuhan 430078, China
- School of Environmental Studies, China University of Geosciences, Wuhan 430078, China
| | - Xulong Lai
- State Key Laboratory of Biogeology and Environmental Geology, China University of Geosciences, Wuhan 430078, China
- School of Earth Sciences, China University of Geosciences, Wuhan 430074, China
| | - Michael Hofreiter
- Institute for Biochemistry and Biology, University of Potsdam, Karl-Liebknecht-Strasse 24–25, 14476 Potsdam, Germany
- Correspondence: (M.H.); (J.Y.); Tel.: +49-331-977-6321 (M.H.); +86-027-6788-3022 (J.Y.)
| | - Junxia Yuan
- State Key Laboratory of Biogeology and Environmental Geology, China University of Geosciences, Wuhan 430078, China
- Faculty of Materials Science and Chemistry, China University of Geosciences, Wuhan 430078, China
- Correspondence: (M.H.); (J.Y.); Tel.: +49-331-977-6321 (M.H.); +86-027-6788-3022 (J.Y.)
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