GeobiosPub Date : 2024-10-01DOI: 10.1016/j.geobios.2024.08.004
Hao-Ran Zong , Jin-Jin Hu , Nian Wang , Yong-Jiang Huang
{"title":"Tsuga leaves from the Neogene Baoshan Basin in southwest China and their palaeoecological implications","authors":"Hao-Ran Zong , Jin-Jin Hu , Nian Wang , Yong-Jiang Huang","doi":"10.1016/j.geobios.2024.08.004","DOIUrl":"10.1016/j.geobios.2024.08.004","url":null,"abstract":"<div><div><em>Tsuga</em> (Endl.) Carrière (Pinaceae) has a rich fossil record represented by pollen, leaves, wood and seed cones. Although fossil leaves of the genus have been widely documented, most of them have not been examined microscopically, which may limit their taxonomic resolution. In this study, three-dimensionally preserved leaves and leaf fragments of <em>Tsuga</em> from the Neogene (latest Miocene to Pliocene) Baoshan Basin in western Yunnan, southwest China, were examined both morphologically and micromorphologically. The fossil leaves are characterized by flattened and bifacial shape, round to obtuse apex and petiolate base, adaxially sunken and abaxially elevated midvein, adaxial surface without stomata and with elongated, smooth-margined epidermal cells, and abaxial surface with two stomatal bands along the midvein, each stomatal band consisting of 6–8 longitudinal stomatal lines. Based on comparisons with extant species of the genus, we found that the fossil leaves show the closest affinity to <em>Tsuga dumosa</em> (D. Don) Eichler, an extant species growing in the modern western Yunnan. As modern species of <em>Tsuga</em> prefer humid conditions, our fossil find suggests a humid climate in the Baoshan Basin at the time of fossil deposition, probably due to the influence of the Indian summer monsoon from the southwest. This is consistent with previous results of quantitative palaeoclimate reconstructions using spore/pollen fossil assemblages. Our study provides new fossil evidence for the origin of modern conifer diversity in southwest China. It highlights the importance of microscopic studies in the taxonomic resolution of fossil leaves of Pinaceae.</div></div>","PeriodicalId":55116,"journal":{"name":"Geobios","volume":"86 ","pages":"Pages 107-117"},"PeriodicalIF":1.6,"publicationDate":"2024-10-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"142578306","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}
GeobiosPub Date : 2024-10-01DOI: 10.1016/j.geobios.2024.08.005
Elena Syromyatnikova , Oleg Redkozubov
{"title":"A review of the Late Miocene herpetofauna of the Keinar locality of Moldova","authors":"Elena Syromyatnikova , Oleg Redkozubov","doi":"10.1016/j.geobios.2024.08.005","DOIUrl":"10.1016/j.geobios.2024.08.005","url":null,"abstract":"<div><div>Small fossil amphibians and reptiles from the Late Miocene of the Keinar locality of Moldova are reviewed for the first time. The following taxa are described: <em>Mioproteus caucasicus</em>, <em>Chelotriton</em> sp., <em>Latonia</em> sp., <em>Pelobates</em> sp., <em>Pelophylax</em> sp., “Colubrinae” indet., <em>Natrix</em> sp., two <em>Vipera</em> spp. (“<em>Vipera aspis</em> complex” and “Oriental vipers complex”), and Squamata indet. Among them, <em>Pelobates</em> sp. exhibits the characters which occur in the Early–Late Miocene (presence of both pit-and-ridge and pustular sculptures of the frontoparietal bone) and in the Pliocene (short frontoparietal–squamosal contact) members of the genus; this combination is not observed in any other <em>Pelobates</em> species. The viperid snake of the “<em>Vipera aspis</em> complex” is recorded from Moldova for the first time.</div></div>","PeriodicalId":55116,"journal":{"name":"Geobios","volume":"86 ","pages":"Pages 25-33"},"PeriodicalIF":1.6,"publicationDate":"2024-10-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"142578304","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}
GeobiosPub Date : 2024-10-01DOI: 10.1016/j.geobios.2024.08.006
Steven L. Wick , Thomas M. Lehman
{"title":"A rare ‘flat-headed’ pachycephalosaur (Dinosauria: Pachycephalosauridae) from West Texas, USA, with morphometric and heterochronic considerations","authors":"Steven L. Wick , Thomas M. Lehman","doi":"10.1016/j.geobios.2024.08.006","DOIUrl":"10.1016/j.geobios.2024.08.006","url":null,"abstract":"<div><div>A juvenile pachycephalosaur frontal from the upper Aguja Formation (Late Cretaceous: middle Campanian) of West Texas, USA is unusually thin dorsoventrally, even compared to ‘flat’ frontals of young individuals pertaining to other pachycephalosaur taxa. The specimen is most comparable morphologically and morphometrically to <em>Stegoceras validum</em>. However, it is much thinner than any ‘juvenile’ example of that species, and also differs in the elongate form and radial arrangement of the surficial tubercles, as well as occurrence of radial grooves along the lateral margins of the bone. Such differences are unlikely a reflection of intraspecific variation. Instead, the Aguja specimen likely represents a previously unknown juvenile semaphoront from the southern Western Interior, referred herein to <em>Stegoceras</em> sp. and likely extends the distribution of this widespread Campanian genus. A morphometric evaluation suggests that the holotype specimen of <em>Texacephale langstoni</em>, also from the Aguja Formation, is probably an adult semaphoront of <em>Stegoceras.</em> However, both specimens represent different ontogenetic stages with dissimilar morphologies and so their potential conspecifity remains equivocal. The new Aguja specimen described herein likely represents a ‘paedomorphic’ Campanian pachycephalosaur – one where the onset of doming is displaced until well into ontogeny – a heterochronic attribute <em>Stegoceras</em> sp. shares with <em>S. validum</em> and <em>Pachycephalosaurus wyomingensis.</em> Where an adequate ontogenetic sample is available for comparison, other pachycephalosaur taxa do not seem to exhibit a similar growth progression, and so this appears to be a significant taxonomic characteristic. That some pachycephalosaurs delayed doming of the skull roof during growth is enigmatic, but it may have been an expression of sexual dimorphism, an aid in species recognition, or a response to harsh environmental conditions.</div></div>","PeriodicalId":55116,"journal":{"name":"Geobios","volume":"86 ","pages":"Pages 89-106"},"PeriodicalIF":1.6,"publicationDate":"2024-10-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"142578309","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}
GeobiosPub Date : 2024-10-01DOI: 10.1016/j.geobios.2024.08.007
Panagiotis Skandalos , Fatma Arzu Demirel , Mehmet Cihat Alçiçek , Serdar Mayda , Lars W. van den Hoek Ostende
{"title":"Early Pliocene Spalacinae from the locality of Afşar, western Turkey","authors":"Panagiotis Skandalos , Fatma Arzu Demirel , Mehmet Cihat Alçiçek , Serdar Mayda , Lars W. van den Hoek Ostende","doi":"10.1016/j.geobios.2024.08.007","DOIUrl":"10.1016/j.geobios.2024.08.007","url":null,"abstract":"<div><div>Spalacinae are an unusual component of the fossil record around the world with a limited geographical distribution. The revisited section of Afşar includes one of the richest collections of Spalacinae in Turkey. From Afşar 1, near the base of the section we recovered <em>Pliospalax</em> cf. <em>macoveii</em> while in Afşar 2, at the top of the section we distinguish the species <em>P. tourkobouniensis</em>. The current research includes the first record of the last-mentioned species outside of Europe. Both spalacines indicate a dry and open space environment and, in accordance with the Arvicolinae, suggest that Afşar 1 can be attributed to MN 15 while Afşar 2 is correlated to MN 16.</div></div>","PeriodicalId":55116,"journal":{"name":"Geobios","volume":"86 ","pages":"Pages 11-23"},"PeriodicalIF":1.6,"publicationDate":"2024-10-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"142578303","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}
GeobiosPub Date : 2024-10-01DOI: 10.1016/j.geobios.2024.08.002
Íñigo Vitón , María José Comas-Rengifo , Luís V. Duarte , Antonio Goy
{"title":"Biochronostratigraphy and palaeobiogeography of Echioceratidae (Ammonitina) from the Raricostatum Zone (Aplanatum Subzone) in NW Iberia","authors":"Íñigo Vitón , María José Comas-Rengifo , Luís V. Duarte , Antonio Goy","doi":"10.1016/j.geobios.2024.08.002","DOIUrl":"10.1016/j.geobios.2024.08.002","url":null,"abstract":"<div><div>This paper examines the uppermost Sinemurian and lowermost Pliensbachian ammonite fauna recorded in NW Iberia with a special focus on Echioceratidae from the Aplanatum Subzone. In total, 852 specimens have been collected bed-by-bed from five reference sections from the Asturian, Basque-Cantabrian, and Lusitanian basins. Echioceratidae, namely <em>Paltechioceras</em> genus, represent 86.2% of the sample, Polymorphitidae (<em>Leptonotoceras</em> genus) the 10%, and less than 4% of the specimens are Eoderoceratidae, Phricodoceratidae, or Oxynoticeratidae. This study describes five species of <em>Paltechioceras</em>, namely <em>P. tardecrescens</em>, <em>P. oosteri</em>, <em>P. recticostatum</em>, <em>P. elicitum</em>, and <em>P. romanicum</em>. They allow a biochronostratigraphic division for the studied basins and its worldwide correlation. One of the species, <em>P. romanicum</em>, is the latest one registered in all the studied sections, occurring directly below the Sinemurian–Pliensbachian boundary. The disappearance of this widely distributed species marks the echioceratids extinction. This work reviews the global events described around the Sinemurian–Pliensbachian transition (the Sinemurian–Pliensbachian boundary event). Finally, we present a palaeobiogeographical analysis of the <em>Paltechioceras</em> species described, giving more information to discuss the opening of the Hispanic Corridor during the late Sinemurian.</div></div>","PeriodicalId":55116,"journal":{"name":"Geobios","volume":"86 ","pages":"Pages 65-87"},"PeriodicalIF":1.6,"publicationDate":"2024-10-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"142578308","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"OA","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
GeobiosPub Date : 2024-10-01DOI: 10.1016/j.geobios.2024.08.003
Rodrigo L. Tomassini , Claudia I. Montalvo , José I. Cuitiño , María Susana Bargo , Sergio F. Vizcaíno
{"title":"Tuff deposits as preservational context for a Miocene continental mammal assemblage from Patagonia, Argentina","authors":"Rodrigo L. Tomassini , Claudia I. Montalvo , José I. Cuitiño , María Susana Bargo , Sergio F. Vizcaíno","doi":"10.1016/j.geobios.2024.08.003","DOIUrl":"10.1016/j.geobios.2024.08.003","url":null,"abstract":"<div><div>The CO tuff is one of the volumetrically largest volcaniclastic events so far recorded in the Early-Middle Miocene Santa Cruz Formation (Patagonian Argentina). It represents aeolian processes, related with westerlies, that reworked and transported enormous quantities of volcanic ash from the Andes into the continental interior that accumulated in fluvial floodplain deposits. This volcanic event generated a major environmental change at ∼17 Ma (Burdigalian) and hostile living conditions for the biota of the area, at least during the time of deposition. We performed here a comprehensive study including taxonomic, sedimentological, and taphonomic aspects of the mammal assemblage recovered from this tuff deposit. The assemblage is constituted by representatives of Microbiotheria, Paucituberculata, Folivora, Cingulata, Rodentia, Notoungulata, and Litopterna, reflecting a wide mammalian diversity. The formation of the assemblage can be linked to a normal attritional model, in which the death of the individuals and subsequent deposition and burial of their remains would have occurred gradually over time, simultaneously with the accumulation of volcanic ash, at the place of death or very close to it. The time between the death and burial would have been relatively short, in accordance with the rapid and continuous influx of volcanic ash to the depositional environment. This multidisciplinary study allows us to interpret and reconstruct the possible taphonomic pathways of the mammal assemblage and to provide novel information on this particular preservation context linked to volcanically-influenced fluvial environments.</div></div>","PeriodicalId":55116,"journal":{"name":"Geobios","volume":"86 ","pages":"Pages 35-47"},"PeriodicalIF":1.6,"publicationDate":"2024-10-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"142578305","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 Insights on the Upper Triassic Silves Group in Algarve Basin, Portugal: Palynological, paleophytogeography and paleoclimatology advances","authors":"Margarida Vilas-Boas , Zélia Pereira , Simonetta Cirilli , Paulo Fernandes","doi":"10.1016/j.geobios.2024.08.001","DOIUrl":"10.1016/j.geobios.2024.08.001","url":null,"abstract":"<div><div>This paper presents the results of palynostratigraphic studies in the Silves Group in the Algarve Basin, Portugal. From bottom to top comprises the Silves Sandstones, the Silves Marl-Carbonate Evaporitic Complex, and the Volcano-Sedimentary Series. This study aims to detail the age of the Silves Group, bracketing the Triassic-Jurassic transition, using palynology. For this purpose, 250 samples were collected from 14 main sections. Previous results from a section above the Variscan unconformity, enabled to date the base of the Silves Sandstones and the onset of the Mesozoic sedimentary cycle in the Algarve Basin to lower Carnian. In this work, the top of the Silves Sandstones, containing <em>Camerosporites secatus</em>, <em>Enzonalasporites vigens</em>, <em>Granuloperculatipollis rudis</em>, <em>Lagenella martinii</em>, <em>Patinasporites densus</em>, <em>Samaropollenites speciosus</em>, and <em>Vallasporites ignacii</em>, is dated to the upper Carnian. The base of the Silves Marl-Carbonate Evaporitic Complex, consisting of <em>Alisporites</em> sp., <em>Araucariacites australis</em>, <em>Classopollis meyerianus</em>, <em>Classopollis torosus</em>, <em>Paracirculina quadruplicis</em> and <em>Triadispora</em> sp., indicates an upper Carnian age. The presence of <em>Alisporites diaphanus</em>, <em>Araucariacites australis</em>, <em>Cerebropollenites macroverrucosus, Classopollis meyerianus</em>, <em>Classopollis torosus</em>, <em>Perinopollenites elatoides</em>, <em>Calamospora mesozoica</em>, and <em>Kraeuselisporites reissingeri</em> allows to date the top of the Silves Marl-Carbonate Evaporitic Complex as upper Rhaetian-lower Hettangian. This study allows to date the Silves Group in the Algarve Basin from the lower Carnian to lower Hettangian (Triassic-Jurassic boundary) for the first time. The Carnian microflora provides new insights of the Onslow Microflora in the Western Tethys.</div></div>","PeriodicalId":55116,"journal":{"name":"Geobios","volume":"86 ","pages":"Pages 49-64"},"PeriodicalIF":1.6,"publicationDate":"2024-10-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"142578307","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"OA","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
GeobiosPub Date : 2024-10-01DOI: 10.1016/j.geobios.2024.06.001
Sampa Kundu, Mahasin Ali Khan
{"title":"A new epifoliar melioloid fungus from the Siwalik (Miocene) of Himachal sub-Himalaya and its palaeoecological implications","authors":"Sampa Kundu, Mahasin Ali Khan","doi":"10.1016/j.geobios.2024.06.001","DOIUrl":"10.1016/j.geobios.2024.06.001","url":null,"abstract":"<div><div>A new fossil epifoliar ascomycete (Ascomycota), <em>Meliolinites miocenicus</em> nov. sp. (fossil Meliolaceae), occurs <em>in situ</em> on a compressed monocot leaf from middle Siwalik (Late Miocene, ca. 12–8 Ma) sediments of Himachal Pradesh, Western Himalaya. The fossil consists of a well-preserved mycelium of superficial, brown to dark brown, septate, thick-walled, branched hyphodiate hyphae; a sub-globose, dark brown putative ascoma, and an oblong to broadly cylindrical, five-celled, four-septate, mature germinating ascospore. The new fossil differs from earlier reported melioloid fossils primarily in the morphology of appressoria. <em>Meliolinites miocenicus</em> nov. sp. on its host is evidence of the existence of a biotrophic relationship at the time of deposition. Qualitative climate data using plant megafossils recovered from the same fossil locality indicate that <em>M. miocenicus</em> nov. sp. and its host thrived in a warm and humid tropical environment.</div></div>","PeriodicalId":55116,"journal":{"name":"Geobios","volume":"86 ","pages":"Pages 1-10"},"PeriodicalIF":1.6,"publicationDate":"2024-10-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"142578302","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}
GeobiosPub Date : 2024-08-01DOI: 10.1016/j.geobios.2023.12.010
George D. Koufos
{"title":"Updating the fauna and age of the Neogene-Quaternary large mammal sites of Greece","authors":"George D. Koufos","doi":"10.1016/j.geobios.2023.12.010","DOIUrl":"10.1016/j.geobios.2023.12.010","url":null,"abstract":"<div><p>The Neogene-Quaternary continental deposits cover large areas of Greece and several fossil mammal sites have been discovered in the country. There are several collections of large fossil mammals for this time span, which provide important data for the fauna biochronology, correlations, palaeoecology and palaeogeography of the area. The last lists with the fauna, age and biochronology of the Greek large mammal localities were given in 2006 for the Neogene and in 2001 for the Quaternary. Extensive research over the last twenty years provided several new localities, and many data and information were published. Therefore, an updating of the lists was more than necessary, and the present article deals with it; it covers the time span untill June 2023. Lists include all faunal information as the systematic classification, chronology, biostratigraphic correlation of the faunas, and main bibliography. It is worth mentioning that some of the Greek localities are key-localities for the Eastern Mediterranean region, e.g., Pikermi, Axios Valley, Villafranchian collection. These faunas are important for the comparison and identification of new collections, correlations, palaeoecology, and palaeogeography of Neogene European mammals.</p></div>","PeriodicalId":55116,"journal":{"name":"Geobios","volume":"85 ","pages":"Pages 35-57"},"PeriodicalIF":1.6,"publicationDate":"2024-08-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"141699690","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}
GeobiosPub Date : 2024-08-01DOI: 10.1016/j.geobios.2023.12.008
Brigitte Meyer-Berthaud , Candys Bert , Anne-Laure Decombeix , Marion Lacand , Merlin Ramel , Ralph Thomas Becker , Christian Klug , Ahmed El Hassani , Abdelfatah Tahiri
{"title":"The euphyllophytes of a new Givetian plant assemblage from the eastern Anti-Atlas, Morocco","authors":"Brigitte Meyer-Berthaud , Candys Bert , Anne-Laure Decombeix , Marion Lacand , Merlin Ramel , Ralph Thomas Becker , Christian Klug , Ahmed El Hassani , Abdelfatah Tahiri","doi":"10.1016/j.geobios.2023.12.008","DOIUrl":"10.1016/j.geobios.2023.12.008","url":null,"abstract":"<div><p><span>The Middle Devonian is a transitional period for the first vascular plants, which acquire modern vegetative and reproductive structures, diversify considerably and, within the euphyllophytes, evolve the first representatives of modern plant groups, the monilophytes and lignophytes. However, the dynamics of this diversification across the different paleocontinents remains obscure, particularly within Gondwana. The upper Givetian locality of Oum el Jerane, in southeastern Morocco, has yielded a new assemblage of anatomically preserved plant remains whose description contributes to a better understanding of the floras of the northern margin of Gondwana during the Middle Devonian. The euphyllophytes include one iridopterid, </span><em>Arachnoxylon minor</em><span>, two cladoxylopsids, one of which represents the new genus </span><em>Jerana</em>, and two aneurophytales affiliated with the genus <em>Triloboxylon</em><span>. The cladoxylopsid remains from Oum el Jerane correspond to relatively small plants compared to the well-known coeval cladoxylopsids of Laurussia. Compared to the taxonomic composition of the four phytochoria recently defined for the Middle Devonian, the Oum el Jerane plant assemblage corresponds to the ‘subtropical’ phytochorion, which is close to the ‘Laurussia’ phytochorion, but which would correspond to drier environmental conditions.</span></p></div>","PeriodicalId":55116,"journal":{"name":"Geobios","volume":"85 ","pages":"Pages 58-78"},"PeriodicalIF":1.6,"publicationDate":"2024-08-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"141701658","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}