Geobios最新文献

{"title":"A new rodent chronology for the late Neogene of Spain","authors":"Jan A. van Dam ,&nbsp;Pierre Mein ,&nbsp;Miguel Garcés ,&nbsp;Ronald T. van Balen ,&nbsp;Marc Furió ,&nbsp;Luis Alcalá","doi":"10.1016/j.geobios.2023.01.001","DOIUrl":"10.1016/j.geobios.2023.01.001","url":null,"abstract":"<div><p>The number of late Neogene Spanish micromammal-containing continental sections with a correlation to the Geomagnetic Time Scale is steadily growing. Nonetheless, well-calibrated sections with dense micromammal records are still rare, biostratigraphic correlations between basins are not straightforward, and ages of uncalibrated sites are poorly constrained. Here, we aim at improving the chronology of Iberian micromammal sections and sites for the interval 8.5–2 Ma by: (<em>i</em>) analyzing qualitative and quantitative similarities between rodent assemblages and turnover in the different basins, (<em>ii</em>) formulating a system of fifteen Iberian assemblage biozones, and (<em>iii</em>) constraining the ages of zone boundaries, assuming isochroneity across basins. Age uncertainty ranges for most known Iberian micromammal sites are obtained by combining regional biozone boundary ages with local magnetostratigraphic records, sedimentation rates and/or evolutionary rates. In addition, our results include new, integrated stratigraphic records from the Jumilla-La Celia and Teruel Basins, which are used to constrain the thus far poorly dated interval covering the latest Tortonian and earliest Messinian (8–7 Ma).</p></div>","PeriodicalId":55116,"journal":{"name":"Geobios","volume":null,"pages":null},"PeriodicalIF":1.6,"publicationDate":"2023-02-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"43316839","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

{"title":"Tropical forests and Combretaceae woodland at Usno in the Lower Omo Valley (Ethiopia), 3.3–3.2 Ma ago","authors":"Marie-Claude Jolly-Saad ,&nbsp;Raymonde Bonnefille","doi":"10.1016/j.geobios.2023.01.003","DOIUrl":"10.1016/j.geobios.2023.01.003","url":null,"abstract":"<div><p><span>In this paper, we describe anatomical structures of 11 fossil wood samples collected from two localities (Brown Sands and Flat Sands) of the Usno Formation, in the Lower Omo valley, Ethiopia. On the basis of former stratigraphy and new investigation, notably Ar/Ar dating of intercalated tuffs and palaeomagnetic studies, the samples are dated between 3.33 and 3.21 Ma. The identified wood samples have been collected within two distinct stratigraphic layers deposited during this time range. The oldest one from Brown Sands includes </span><em>Albizia</em> sp., <em>Entada</em> sp. and a possible Combretaceae or Leguminosae. The youngest assemblage from White Sands includes many representatives of Combretaceae including <em>Combretum molle</em> and <em>Terminalia</em> sp. associated with <em>Erythrina</em><span> sp. These assemblages strongly differ from other Miocene<span> and Pliocene wood assemblages known from Ethiopia. Palaeoenvironmental interpretation of the identified tree taxa support affinities with the extant mid-elevation </span></span><em>Albizia</em> forest replaced by <em>Combretum/Terminalia</em> woodland in about one hundred thousand years. In the Lower Omo valley, the more humid character of the Pliocene vegetation strongly contrast with the arid <em>Acacia/Commiphora</em><span> steppe widely spread over the region today. Such past vegetation attests to much wetter and favourable climatic conditions under seasonal climate. However significant changes in the floristic composition of tree cover occurring within a timespan of hundred thousand years, plays in favour of climatic and palaeo-environmental instabilities at a time when </span><em>Australopithecus afarensis</em> existed in the Turkana basin and flourished elsewhere in Ethiopia.</p></div>","PeriodicalId":55116,"journal":{"name":"Geobios","volume":null,"pages":null},"PeriodicalIF":1.6,"publicationDate":"2023-02-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"41577317","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

{"title":"A new species of Pleuromeia (Lycopsid) from the upper Middle Triassic of Northern China and discussion on the spatiotemporal distribution and evolution of the genus","authors":"Shenghui Deng,&nbsp;Yuanzheng Lu,&nbsp;Ru Fan,&nbsp;Xueying Ma,&nbsp;Dan Lyu,&nbsp;Zhong Luo,&nbsp;Yanqi Sun","doi":"10.1016/j.geobios.2022.10.001","DOIUrl":"https://doi.org/10.1016/j.geobios.2022.10.001","url":null,"abstract":"<div><p><em>Pleuromeia</em><span> Corda is an iconic lycopod genus in the Early Triassic floras of the world. </span><em>Pleuromeia</em><span> fossils<span> are very significant in stratigraphy and palaeoenvironmental interpretation and have been regarded as an important Lower Triassic index fossil. Although some recent studies show that the genus occurred in the lower part of the Middle Triassic, no definite </span></span><em>Pleuromeia</em> has been reported from the late Middle Triassic and the younger strata so far. In this paper, some reproductive organ fossils of <em>Pleuromeia</em> from the upper Middle Triassic Tongchuan Formation in Shaanxi Province (belonging to the Ordos Basin), North China, are described for the first time, belonging to the new species <em>Pleuromeia obovata</em><span> Deng nov. sp. Highly accurate dating results of tuff layers indicate that the age of the new species is between 241.06 ± 0.12 Ma and 241.558 ± 0.093 Ma, equivalent to the early Ladinian. This is the youngest species of genus </span><em>Pleuromeia</em> so far. Spatiotemporal distribution of <em>Pleuromeia</em><span> indicates that the genus first appeared in the Induan (Early Triassic) in North China, occurred widespread and flourished in both Laurasia and Gondwana<span> during the Olenekian (late Early Triassic), declined from the Anisian (early Middle Triassic), survived in the Ladinian in North China, and may have gone extinct as early as the end of the Middle Triassic. North China may well have included the place of origination and the last habitats of this genus.</span></span></p></div>","PeriodicalId":55116,"journal":{"name":"Geobios","volume":null,"pages":null},"PeriodicalIF":1.6,"publicationDate":"2022-12-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"136932336","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

{"title":"The conodont genus Neognathodus Dunn, 1970, lower to middle Pennsylvanian, Amazonas Basin, Western Gondwana: Biostratigraphic and paleoenvironmental analysis","authors":"Andrés Felipe Rojas Mantilla ,&nbsp;Ana Karina Scomazzon ,&nbsp;Sara Nascimento ,&nbsp;Renata dos Santos Alvarenga ,&nbsp;Valesca Brasil Lemos ,&nbsp;Paulo Alves de Souza","doi":"10.1016/j.geobios.2022.10.002","DOIUrl":"https://doi.org/10.1016/j.geobios.2022.10.002","url":null,"abstract":"<div><p>Conodonts are very abundant, present a wide occurrence worldwide and high evolutionary rates during the Paleozoic and the Triassic, providing the recognition of more than 240 biozones over the 300 million years of their geological history. <em>Neognathodus</em> comprises species useful as biostratigraphic markers for the early-to-middle Pennsylvanian succession. In this paper, we analyze the record of this genus within the Amazonas Basin, northern Brazil, based on 18 wells and several outcropping sections, including limestone exploratory mines, related to the marine deposits of the Tapajós Group (Monte Alegre, Itaituba and Nova Olinda formations). Taxa have been revised, updated and some have been reclassified according to current international taxonomy. All records of this genus were morphologically analyzed using stereomicroscope and Scanning Electronic Microscope images, allowing the recognition of six species<em>: N. symmetricus</em>, <em>N. bassleri</em>, <em>N. medadultimus</em>, <em>N. atokaensis</em>, <em>N. bothrops</em>, and <em>N. roundyi.</em> The occurrences of these species as well their areal distribution in the basin were detailed, resulting in several modeling stratigraphic maps. Four biozones are proposed herein, in ascending stratigraphic order: (<em>i</em>) <em>N. symmetricus-N. bassleri</em> interval Zone, (<em>ii</em>) <em>N. bassleri-N. symmetricus</em> interval Zone, (<em>iii</em>) <em>N. atokaensis</em> taxon range Zone, and (<em>iv</em>) <em>N. atokaensis-N. bassleri</em><span> interval Zone. A middle Bashkirian<span> to middle Moscovian age is assigned to the studied marine deposits of the Tapajós Group. </span></span><em>Neognathodus</em> is related worldwide to neritic, warm and oxygenated water environments both in high energy proximal contexts and in lower energy more distal environments, slightly deeper waters and periodically affected by storms.</p></div>","PeriodicalId":55116,"journal":{"name":"Geobios","volume":null,"pages":null},"PeriodicalIF":1.6,"publicationDate":"2022-12-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"136932337","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

{"title":"A new genus and species of eurypterid (Chelicerata, Eurypterida) from the Lower Devonian Xiaxishancun Formation of Yunnan, southwestern China","authors":"Jiashu Wang ,&nbsp;Lu Liu ,&nbsp;Jinzhuang Xue ,&nbsp;James C. Lamsdell ,&nbsp;Paul A. Selden","doi":"10.1016/j.geobios.2022.09.001","DOIUrl":"10.1016/j.geobios.2022.09.001","url":null,"abstract":"<div><p><span>Eurypterids constituted an important component of Paleozoic marine ecosystems, but their fossil record has been mainly reported from North America and Europe, and the evolution of this group in other regions such as East Asia remains poorly understood. A new eurypterid, </span><em>Malongia mirabilis</em><span> nov. gen., nov. sp., is described from the Lower Devonian (Lochkovian) Xiaxishancun Formation of Qujing, Yunnan, southwestern China. The holotype shows a ventral prosoma with appendages II–VI and part of the opisthosoma. The characters indicating a dolichopterid affinity of the new taxon include: metastoma anterior cordate and basally truncated; appendage III bearing multiple enlarged spines; appendage V nonspiniferous; long appendage VI with expanded distal podomere and narrow triangular VI-7a; subrhomboidal coxa of appendage VI with a rounded principal tooth. </span><em>Malongia</em> nov. gen. is the fourth genus described within the Dolichopteridae Kjellesvig-Waering and Størmer, 1952, other members of which are <em>Dolichopterus</em> Hall, 1859, <em>Clarkeipterus</em> Kjellesvig-Waering, 1966, and <em>Ruedemannipterus</em> Kjellesvig-Waering, 1966; it represents the only record of this family in South China.</p></div>","PeriodicalId":55116,"journal":{"name":"Geobios","volume":null,"pages":null},"PeriodicalIF":1.6,"publicationDate":"2022-12-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"42293067","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

{"title":"Fossil lizards and snakes (Diapsida, Squamata) from the Late Miocene hominid locality of Haritalyangar, India","authors":"Ningthoujam Premjit Singh ,&nbsp;Shubham Deep ,&nbsp;Andrej Čerňanský ,&nbsp;Ramesh Kumar Sehgal ,&nbsp;Abhishek Pratap Singh ,&nbsp;Navin Kumar ,&nbsp;Piyush Uniyal ,&nbsp;Saroj Kumar ,&nbsp;Kewal Krishan ,&nbsp;Rajeev Patnaik","doi":"10.1016/j.geobios.2022.10.003","DOIUrl":"10.1016/j.geobios.2022.10.003","url":null,"abstract":"<div><p><span>The Late Miocene<span> hominid-bearing locality in Haritalyangar, India, has yielded remains of fossil lizards and snakes. The material consists of the following taxa: </span></span><em>Varanus</em> and an indeterminate anguimorph, <em>Python</em>, a colubrid and a natricid. These squamates are documented from this region for the first time. A co-existence of <em>Varanus</em> and <em>Python</em>, two iconic squamates, is demonstrated. The overall fauna, which is dominated by both large and small semi-aquatic and terrestrial taxa, indicates seasonally wet sub-humid to semi-arid climate in the area during the Late Miocene, ∼9.1 Ma. Moreover, the mean annual temperature must have been high in the region at that time (not less than 15–18.6 °C, similar to the mean annual temperature in this area today), indicated by the occurrence of important thermophilic elements such as <em>Varanus</em> and <em>Python</em>.</p></div>","PeriodicalId":55116,"journal":{"name":"Geobios","volume":null,"pages":null},"PeriodicalIF":1.6,"publicationDate":"2022-12-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"47776851","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

{"title":"New data on the new micromammalian localities of Afoud (Aït Kandoula Basin, Morocco) at the Mio-Pliocene boundary: Biochronological, paleoecological and paleobiogeographic implications","authors":"Salamet Mahboubi,&nbsp;Jérôme Surault,&nbsp;Mouloud Benammi","doi":"10.1016/j.geobios.2022.06.003","DOIUrl":"10.1016/j.geobios.2022.06.003","url":null,"abstract":"<div><p>Small mammal remains have been discovered in three new outcrops from the Afoud locality. This site is significant from a paleontological point of view because it has yielded fauna of European affinities (<em>Castillomys</em>, <em>Occitanomys</em>, <em>Stephanomys, Eliomys,</em> and <em>Prolagus</em>). The presence of two different species of <em>Arvicanthis</em><span><span><span><span> from the Afoud locality represents the oldest record in North Africa. The association of small mammals from the AF12-2 deposits provides an approximate view of the local environment and climate at the time of the formation of this locality. This faunal assemblage indicates a warm, temperate, semi-arid climate and an open vegetation cover of wooded savannah. </span>Fossil assemblages documented in this paper expand our knowledge on the Late Miocene–Early </span>Pliocene small mammal communities of the Aït Kandoula Basin. This study provides useful data for understanding the </span>paleobiogeography<span><span> of the Mediterranean region<span> and faunal exchanges between North Africa and the Iberian Peninsula that took place before the </span></span>Messinian<span> Salinity Crisis.</span></span></span></p></div>","PeriodicalId":55116,"journal":{"name":"Geobios","volume":null,"pages":null},"PeriodicalIF":1.6,"publicationDate":"2022-10-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"49493062","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

{"title":"Distinction of Sivatherium from Libytherium and a new species of Libytherium (Giraffidae, Ruminantia, Mammalia) from the Siwaliks of Pakistan (Miocene)","authors":"María Ríos ,&nbsp;Sayyed Ghyour Abbas ,&nbsp;Muhammad Akbar Khan ,&nbsp;Nikos Solounias","doi":"10.1016/j.geobios.2022.06.002","DOIUrl":"10.1016/j.geobios.2022.06.002","url":null,"abstract":"<div><p>This study deals with the issues around the synonymization of the large extinct giraffid genera <em>Libytherium</em> and <em>Sivatherium</em>. We performed a morphological and biometrical analysis of the cranial remains of these giraffid genera and resolved this question by formulating criteria to distinguish <em>Libytherium</em> from <em>Sivatherium</em>, and to justify their systematic position within the Giraffidae. The present study also reports a new species of the genus <em>Libytherium</em>, <em>Libytherium proton</em> nov. sp. from the Chinji Formation (late Middle Miocene) and the Dhok Pathan Formation (Late Miocene) of the Siwalik Group of the Indian subcontinent. This extends the biogeographic and biostratigraphic range of <em>Libytherium</em> because this taxon had never been reported from the Siwaliks, Asia and the Miocene before this study. This study also initiates a detailed reassessment of the African and Siwalik material currently attributed to genus <em>Sivatherium</em> (and some other genera) and their proper allocation within the Giraffidae.</p></div>","PeriodicalId":55116,"journal":{"name":"Geobios","volume":null,"pages":null},"PeriodicalIF":1.6,"publicationDate":"2022-10-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"43403193","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

{"title":"Oligocene-Miocene marine mammals from Belgrade Quarry, North Carolina","authors":"Robert W. Boessenecker","doi":"10.1016/j.geobios.2022.08.002","DOIUrl":"10.1016/j.geobios.2022.08.002","url":null,"abstract":"<div><p><span>A diverse but fragmentary assemblage of fossil cetaceans is reported from the Oligocene-Miocene Belgrade Formation of North Carolina. This assemblage preserves many odontocetes including four xenorophids (</span><em>Albertocetus</em>, <em>Echovenator</em> sp., cf. <em>Cotylocara</em>, and <em>Xenorophus</em> sp.), a possible waipatiid (cf. Waipatiidae), a giant agorophiid-grade dolphin (<em>Ankylorhiza</em>), a shark-toothed dolphin (cf. <em>Squalodon</em>), longirostrine “swordfish” dolphins (Eurhinodelphinidae), a longirostrine eoplatanistid dolphin (cf. <em>Eoplatanista</em>), a longirostrine squalodelphinid dolphin, a possible early delphinidan (Kentriodontidae), as well as an eomysticetid baleen whale (<em>Eomysticetus</em><span> sp.) and sirenian<span> fragments. Most of these taxa are characteristic of or unique to Oligocene deposits (Xenorophidae, cf. Waipatiidae, </span></span><em>Ankylorhiza</em>, <em>Eomysticetus</em><span>) whereas others are more typical of early or middle Miocene deposits (cf. </span><em>Eoplatanista</em>, Eurhinodelphinidae, cf. <em>Squalodon</em>, Squalodelphinidae, Kentriodontidae). The Belgrade Formation at Belgrade Quarry is dated to 25.95–21.12<!--> <!-->Ma, approximating the Oligocene-Miocene transition. The transitional composition of the Belgrade cetacean assemblage suggests gradual changes between Oligocene to Miocene cetacean faunas, to be verified by the discovery of more complete remains from the poorly sampled earliest Miocene (Aquitanian).</p></div>","PeriodicalId":55116,"journal":{"name":"Geobios","volume":null,"pages":null},"PeriodicalIF":1.6,"publicationDate":"2022-10-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"44874917","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

{"title":"Description of new Pliocene to Early Pleistocene deer (Cervidae, Mammalia) remains from the Siwalik Hills in Pakistan with a discussion on paleobiogeography of cervids from the Indian subcontinent","authors":"Roman Croitor ,&nbsp;Muhammad Akbar Khan ,&nbsp;Sayyed Ghyour Abbas ,&nbsp;Muhammad Adeeb Babar ,&nbsp;Muhammad Asim ,&nbsp;Muhammad Akhtar","doi":"10.1016/j.geobios.2022.08.001","DOIUrl":"10.1016/j.geobios.2022.08.001","url":null,"abstract":"<div><p>This article presents a description of new antler remains from five fossiliferous sites (Sardhok, Panjan Sher Shahana, Puran, Jari Kas, and Potha) of the Upper Siwaliks in Pakistan. The systematic study of the antler material revealed the presence of six cervid forms: <em>Metacervocerus punjabiensis</em>, <em>Rucervus</em> sp., <em>Panolia</em> sp., <em>Hyelaphus</em> sp., <em>Praesinomegaceros bakri</em>, and a poorly represented large cervid that shows a certain affinity with “<em>Eucladoceros</em> sp.” from the Early Pleistocene of Kuruksai (Tajikistan). The remains of <em>Panolia</em> represent the earliest known paleontological record of this cervid lineage. Unlike <em>Metacervocerus</em> and <em>Rucervus</em> that have had phylogenetically closely related counterparts in east and north of the Alpine-Himalayan mountain belt, the evolution of <em>Panolia</em> took place in the Indian subcontinent. The entry of <em>Panolia</em> lineage into the Indian subcontinent marks its phylogenetic split from the main <em>Cervus</em>/<em>Rusa</em> evolutionary branch. The earliest dispersal events of cervids into the Indian subcontinent was preceded by the late Miocene evolutionary radiation and ecological diversification of the subfamily Cervinae in Southeastern Asia. <em>Praesinomegaceros</em> and <em>Metacervocerus</em> most probably entered the Indian subcontinent via Central Asia. Possibly, this is also the case of “<em>Eucladoceros</em> sp.” from Kuruksai (Tajikistan). The dispersal ways of <em>Panolia</em> and <em>Rucervus</em> remain unclear. The dispersals of small-sized cervids (<em>Muntiacus</em> and <em>Hyelaphus</em>) into the Indian subcontinent was triggered by the establishment of the 100-ky glaciation cycle during the Middle Pleistocene: the sea level dropped during glacial peaks and opened to them the dispersal route from Sundaland in the South.</p></div>","PeriodicalId":55116,"journal":{"name":"Geobios","volume":null,"pages":null},"PeriodicalIF":1.6,"publicationDate":"2022-10-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"42902461","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}