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Alcheringa: An Australasian Journal of Palaeontology最新文献

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Unusual diagenesis of Cambrian chancelloriids from Greenland and Siberia 格陵兰和西伯利亚寒武纪蝶形花的异常成岩作用
Pub Date : 2024-05-12 DOI: 10.1080/03115518.2024.2348101
John S. Peel, Artem Kouchinsky
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引用次数: 0
Form-classification for microbially induced sedimentary structures 微生物诱导沉积结构的形式分类
Pub Date : 2024-05-09 DOI: 10.1080/03115518.2024.2345641
G. Retallack
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引用次数: 0
Shell microstructure of Styliolina clavulus (Tentaculita) from the Middle Devonian of Czech Republic: implications for phylogenetic affinities and biomineralization of thin-walled tentaculitids 捷克共和国中泥盆纪 Styliolina clavulus(Tentaculita)的贝壳微观结构:对薄壁触角类的系统发育亲缘关系和生物矿化的影响
Pub Date : 2024-05-06 DOI: 10.1080/03115518.2024.2342879
O. Vinn, Abdullah A. Alkahtane, M. El Hedeny, Saleh Al Farraj
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引用次数: 0
Tree-climbing in search of fruit: an ancient arboreal marsupial megafrugivore from the Miocene of Australia 爬树寻找果实:来自澳大利亚中新世的一种古老的树栖有袋类巨型食果动物
Pub Date : 2023-11-09 DOI: 10.1080/03115518.2023.2268680
Larisa DeSantis, Michael Archer, Karen Black, Suzanne Hand, Vera Korasidis
AbstractDiprotodontids, a group of large-bodied wombat-like marsupial herbivores, were broadly distributed in Australasian Cenozoic deposits. While most diprotodontids were terrestrial quadrupeds and are often compared to placental herbivores like rhinoceros and hippopotamuses, the zygomaturine diprotodontid Nimbadon lavarackorum, based on its post-cranial morphology, is thought to have occupied the treetops. Understanding the dietary ecology of N. lavarackorum during the Miocene can help clarify potential motivations for an arboreal lifestyle. Here, we conducted dental microwear texture analysis (DMTA) and stable isotope analysis (SIA) of N. lavarackorum specimens from the Riversleigh World Heritage Area and compared them to analogous extant mammals to assess the likelihood that these tree-dwelling marsupials occupied a unique ecological niche during the Miocene in Australia—arboreal megafrugivores. The DMTA of N. lavarackorum (i.e., low anisotropy and high complexity) is most similar to extant mammals that include a high proportion of fruit in their diet and is inconsistent with and statistically distinct from obligate folivores. Stable carbon isotopes of N. lavarackorum also indicate the consumption of C3 food sources, consistent with the consumption of 13C enriched fruit in a C3 forest environment. Fruits may have been a motivation for this ca 70 kg marsupial moving into or staying in the treetops—an ecological niche that is currently unoccupied in Australia today.Larisa DeSantis [larisa.desantis@vanderbilt.edu], Department of Biological Sciences, Vanderbilt University, Nashville, TN 37232, USA; Department of Earth and Environmental Sciences, Vanderbilt University, Nashville, TN 37240, USA; Michael Archer [m.archer@unsw.edu.au], Earth and Sustainability Science Research Centre, School of Biological, Earth and Environmental Sciences, University of New South Wales, Sydney, NSW, 2052, Australia; Karen Black [k.black@unsw.edu.au], Earth and Sustainability Science Research Centre, School of Biological, Earth and Environmental Sciences, University of New South Wales, Sydney, NSW, 2052, Australia; Suzanne Hand [s.hand@unsw.edu.au], Earth and Sustainability Science Research Centre, School of Biological, Earth and Environmental Sciences, University of New South Wales, Sydney, NSW, 2052, Australia; Vera Korasidis [vera.korasidis@unimelb.edu.au], Department of Geography, Earth and Atmospheric Sciences, University of Melbourne, Parkville, VIC, 3010, Australia.Keywords: Cenozoicdental microweardietmammalpalaeoecologyRiversleighstable isotopes AcknowledgementsWe would like to thank all museum staff, curators, and collection managers who assisted with access to this material at the American Museum of Natural History and Queensland Museum. We are thankful to J. Curtis (University of Florida) for isotopic analysis, E. Mueller for assistance with Fig. 3. We are beholden to the Waanyi Aboriginal Community of northwestern Queensland and, for their ongoing suppor
摘要双原齿兽是一类大型袋熊类有袋类食草动物,广泛分布于澳大利亚新生代沉积物中。虽然大多数双原齿类动物是陆生四足动物,经常被比作胎盘食草动物,如犀牛和河马,但根据其颅后形态,人们认为颧aturine双原齿类Nimbadon lavarackorum曾居住在树顶。了解新世时期lavarackorum的饮食生态学有助于阐明其以树栖方式生活的潜在动机。在此,我们对来自riverleigh世界遗产区的N. lavarackorum标本进行了牙齿微磨损结构分析(DMTA)和稳定同位素分析(SIA),并将其与类似的现存哺乳动物进行了比较,以评估这些树栖有袋动物在澳大利亚中新世占据独特生态位的可能性-树栖巨噬动物。N. lavarackorum的DMTA(即低各向异性和高复杂性)与现存哺乳动物最相似,在其饮食中包含高比例的水果,与专性叶食动物不一致,在统计上不同。lavarackorum的稳定碳同位素也表明了C3食物来源的消耗,与C3森林环境中富含13C的水果的消耗一致。水果可能是这种重达70公斤的有袋类动物进入或停留在树梢的动机——这一生态位目前在澳大利亚是无人占据的。Larisa DeSantis [larisa.desantis@vanderbilt.edu],范德比尔特大学生物科学系,田纳西州纳什维尔37232,美国;美国范德比尔特大学地球与环境科学系,田纳西州纳什维尔37240;Michael Archer [m.archer@unsw.edu.au],新南威尔士大学生物、地球与环境科学学院地球与可持续发展科学研究中心,新南威尔士州悉尼2052;Karen Black [k.black@unsw.edu.au],新南威尔士大学生物、地球与环境科学学院地球与可持续发展科学研究中心,新南威尔士州悉尼2052;Suzanne Hand [s.hand@unsw.edu.au],新南威尔士大学生物、地球与环境科学学院地球与可持续发展科学研究中心,新南威尔士州悉尼2052;Vera Korasidis [vera.korasidis@unimelb.edu.au],墨尔本大学地理、地球与大气科学系,维多利亚州帕克维尔3010,澳大利亚。致谢致谢致谢致谢致谢致谢致谢致谢致谢致谢致谢致谢致谢致谢致谢致谢致谢致谢致谢致谢致谢致谢致谢致谢致谢致谢致谢致谢致谢致谢致谢致谢致谢致谢致谢我们感谢J. Curtis(佛罗里达大学)的同位素分析,E. Mueller对图3的协助。我们感谢昆士兰西北部的Waanyi原住民社区,感谢他们持续不断的支持,我们感谢昆士兰公园和野生动物管理局、澳大利亚环境署、伊萨内陆地区、伊萨山市议会、菲尔·克雷瑟和新南威尔士大学的CREATE基金,以及拉克姆一家。我们也非常感谢许多学生和志愿者在里弗斯利世界遗产地的研究中给予的支持和帮助。披露声明作者未报告潜在的利益冲突。经费由国家科学基金会(1455198)、澳大利亚研究理事会[DE130100467, DP170101420]、范德比尔特大学和新南威尔士大学提供。
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引用次数: 0
Taxonomic review of the genus Dasycercus (Dasyuromorphia: Dasyuridae) using modern and subfossil material; and the description of three new species Dasycercus属(dasyuria: Dasyuridae)的现代和亚化石分类研究以及对三个新物种的描述
Pub Date : 2023-10-22 DOI: 10.1080/03115518.2023.2262083
Jake Newman-Martin, Kenny J. Travouillon, Natalie Warburton, Milo Barham, Alison J. Blyth
The genus Dasycercus (Dasyuridae: Dasyuromorphia) has a long and ongoing history of taxonomic uncertainty. Currently two species are recognized: Dasycercus cristicauda and Dasycercus blythi, with the previously named Dasycercus hillieri considered a junior synonym of D. cristicauda. This investigation integrates modern, historical and subfossil material from across Australia to provide the most comprehensive review of the genus to date. Cranial and dental morphological characters that enable phylogenetic and morphometric analysis of taxa are established. Linear discriminant analysis (LDA) and principal component analysis (PCA) of craniodental measurements, including from the type specimens of named taxa (D. cristicauda, D. hillieri and D. blythi), are used to assess the validity of each taxon. The results confirm the validity of D. cristicauda and D. blythi as species, but also reconfirm the validity of D. hillieri. As a result, much of the modern ‘D. cristicauda’ material is reassigned to D. hillieri. Three new taxa are proposed: Dasycercus woolleyae sp. nov., Dasycercus archeri sp. nov. and Dasycercus marlowi sp. nov. These six Dasycercus species are distributed across Australia’s arid zone and beyond. Based on prior investigations and the results of this taxonomic review, it is likely that only D. hillieri and D. blythi are extant. The identification of four likely extinct taxa marks the first recorded instance of modern extinction within the family Dasyuridae.
Dasycercus属(Dasyuridae: Dasyuromorphia)具有长期和持续的分类不确定性历史。目前已知的两个物种是:cristicauda Dasycercus和blythi Dasycercus,之前命名的Dasycercus hillieri被认为是D. cristicauda的初级同义词。这项调查整合了来自澳大利亚各地的现代、历史和亚化石材料,提供了迄今为止该属最全面的回顾。颅和牙的形态特征,使系统发育和形态计量分析的分类群建立。采用线性判别分析(LDA)和主成分分析(PCA)对已命名分类群(D. cristicauda、D. hillieri和D. blythi)的颅齿测量结果进行有效性评价。结果证实了D. cristicauda和D. blythi作为种的有效性,同时也再次证实了D. hillieri的有效性。因此,大部分现代的D。cristicauda的材料被重新分配给d.h illieri。本文提出了3个新的分类群:毛leydasycercus sp. nov.、archeri Dasycercus sp. nov.和marlowi Dasycercus sp. nov.。这6个Dasycercus分布在澳大利亚的干旱区及其他地区。根据以往的调查和本分类综述的结果,可能只有D. hillieri和D. blythi存在。四个可能灭绝的分类群的鉴定标志着在Dasyuridae家族中第一个有记录的现代灭绝实例。
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引用次数: 0
First known extinct feathertail possums (Acrobatidae, Marsupialia): palaeobiodiversity, phylogenetics, palaeoecology and palaeogeography 已知的最早灭绝的羽尾负鼠(有袋目,有袋目):古生物多样性、系统发育、古生态学和古地理学
Pub Date : 2023-08-27 DOI: 10.1080/03115518.2023.2242439
Prudence R. Fabian, M. Archer, S. Hand, R. Beck
Abstract Four new fossil feathertail possum species (Marsupialia, Diprotodontia, Phalangerida, Petauroidea, Acrobatidae) are described from late Oligocene to middle Miocene fossil deposits in the Riversleigh World Heritage Area, northwestern Queensland. They are the first pre-Pleistocene fossil representatives of this family to be described. Two species are referred to the modern genus Acrobates and two to the modern genus Distoechurus. These species are distinguished from each other and from the living Distoechurus pennatus and Acrobates pygmaeus on the basis of qualitative and quantitative characters of the first lower molar (m1), which is the only tooth known for all four fossil species. Fortunately, m1 is morphologically the most variable tooth in the cheektooth row of acrobatids, and it exhibits numerous genus- and species-specific features. Phylogenetic analyses based on dental characters strongly support monophyly of Acrobatidae relative to other petauroids, as well as providing relatively strong support for reciprocal monophyly of Acrobates and Distoechurus, including the newly described fossil members of these genera. Recognition of species of Acrobates and Distoechurus in these fossil deposits is broadly congruent with recent estimates for the time of divergence of the two modern genera based on molecular data, and also provides an additional fossil calibration point for future studies of marsupial divergence times. These fossil species provide new insights into the biogeographical and ecological history of this enigmatic family of small possums, specifically that the oldest known species of Acrobates occurred in closed forest environments (in contrast to the living species, A. pygmaeus and Acrobates frontalis, which today inhabit open sclerophyll forests and woodlands) and that Distoechurus appears to have originated in Australia, only subsequently dispersing to New Guinea before becoming extinct in its Australian homeland. Prudence R. Fabian [pruefabian@gmail.com], Michael Archer [m.archer@unsw.edu.au], Suzanne J. Hand [s.hand@unsw.edu.au], Earth and Sustainability Science Research Centre, School of Biological, Earth and Environmental Sciences, UNSW Sydney, NSW 2052, Australia; Robin M.D. Beck [r.m.d.beck@salford.ac.uk], School of Science, Engineering and Environment, University of Salford, Manchester M5 4WT, UK.
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引用次数: 0
A new broad-snouted fossil carettochelyid turtle from a previously unknown Caenozoic deposit in Sarawak, Malaysia 在马来西亚沙捞越的一个以前不为人知的新生代沉积物中发现的一种新的宽嘴龟化石
Pub Date : 2023-08-21 DOI: 10.1080/03115518.2023.2243503
A. White, M. Archer, S. Hand, H. Godthelp, A. Gillespie
Abstract Fossils of pan-carettochelyid turtles are known from most continents of the world, except Antarctica. The fossils that have been described indicate a group of estuarine turtles that have little modified their body form since the Cretaceous. The only species for which ecological data exist is the extant Carettochelys insculpta, found in estuarine or fresh waters in Australia and New Guinea. Here we report the discovery of an incomplete skull of a previously unknown carettochelyid Carettochelys niahensis sp. nov. from an undated fossil deposit within or beneath a Miocene marine limestone formation in Niah Great Cave, Sarawak, Malaysia. The skull exhibits many anatomical features characteristic of this turtle group but differs from previously known taxa in that it has a broad, nasal orifice that is proportionately wider than in other carettochelyids and relatively shallow but wider temporal arches. Some aspects of the palaeoecology of this turtle are inferred. Arthur White [arfawhite@gmail.com] Earth and Sustainability Science Research Centre, School of Biological, Earth and Environmental Sciences, University of New South Wales, Sydney 2052, Australia; Michael Archer [m.archer@unsw.edu.au] Earth and Sustainability Science Research Centre, School of Biological, Earth and Environmental Sciences, University of New South Wales, Sydney 2052, Australia; Suzanne J. Hand [s.hand@unsw.edu.au] Earth and Sustainability Science Research Centre, School of Biological, Earth and Environmental Sciences, University of New South Wales, Sydney 2052, Australia; Henk Godthelp [hjgodthelp@gmail.com]; Anna K. Gillespie [a.gillespie@unsw.edu.au] Earth and Sustainability Science Research Centre, School of Biological, Earth and Environmental Sciences, University of New South Wales, Sydney 2052, Australia.
{"title":"A new broad-snouted fossil carettochelyid turtle from a previously unknown Caenozoic deposit in Sarawak, Malaysia","authors":"A. White, M. Archer, S. Hand, H. Godthelp, A. Gillespie","doi":"10.1080/03115518.2023.2243503","DOIUrl":"https://doi.org/10.1080/03115518.2023.2243503","url":null,"abstract":"Abstract Fossils of pan-carettochelyid turtles are known from most continents of the world, except Antarctica. The fossils that have been described indicate a group of estuarine turtles that have little modified their body form since the Cretaceous. The only species for which ecological data exist is the extant Carettochelys insculpta, found in estuarine or fresh waters in Australia and New Guinea. Here we report the discovery of an incomplete skull of a previously unknown carettochelyid Carettochelys niahensis sp. nov. from an undated fossil deposit within or beneath a Miocene marine limestone formation in Niah Great Cave, Sarawak, Malaysia. The skull exhibits many anatomical features characteristic of this turtle group but differs from previously known taxa in that it has a broad, nasal orifice that is proportionately wider than in other carettochelyids and relatively shallow but wider temporal arches. Some aspects of the palaeoecology of this turtle are inferred. Arthur White [arfawhite@gmail.com] Earth and Sustainability Science Research Centre, School of Biological, Earth and Environmental Sciences, University of New South Wales, Sydney 2052, Australia; Michael Archer [m.archer@unsw.edu.au] Earth and Sustainability Science Research Centre, School of Biological, Earth and Environmental Sciences, University of New South Wales, Sydney 2052, Australia; Suzanne J. Hand [s.hand@unsw.edu.au] Earth and Sustainability Science Research Centre, School of Biological, Earth and Environmental Sciences, University of New South Wales, Sydney 2052, Australia; Henk Godthelp [hjgodthelp@gmail.com]; Anna K. Gillespie [a.gillespie@unsw.edu.au] Earth and Sustainability Science Research Centre, School of Biological, Earth and Environmental Sciences, University of New South Wales, Sydney 2052, Australia.","PeriodicalId":272731,"journal":{"name":"Alcheringa: An Australasian Journal of Palaeontology","volume":"22 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"2023-08-21","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"133198392","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 0
Two new species of ektopodontid marsupial from the lower deposits of the Etadunna Formation (latest Oligocene), South Australia and a phylogenetic hypothesis for the Ektopodontidae 南澳大利亚Etadunna组(晚渐新世)下沉积层ektopodontid有袋类两新种及Ektopodontidae的系统发育假说
Pub Date : 2023-08-03 DOI: 10.1080/03115518.2023.2227252
J. Case
Abstract Molar morphologies of the latest Oligocene genera, Chunia and Ektopodon, are easy to distinguish, but species determinations are more difficult. As more specimens have been collected, more maxillary fragments with molars and/or alveoli and a portion of the rostrum preserved are available. With a suite of maxillae now known, new ektopodontid features have revealed themselves, including the shortening of the rostrum compared to other families of contemporary possums. The facial angulation represented by the flexure of the rostrum at the boundary between P3 and the molar row results in the rostrum being angled differently than the molar row. Ektopodontids have a significantly greater angulation and thus shorter faces, compared to that seen in contemporary phalangeriform possums. Two new species of the genus Chunia, from the lower Etadunna Formation, South Australia, can be distinguished from the type species, Chunia illuminata, of the Ditjimanka Local Fauna. Differences in molar morphologies and the degree of facial angulation distinguish a new species of Chunia from the lowest faunal zone and the Minkina Local Fauna (facial angulation of 52°) from C. illuminata from the next higher faunal zone (Ditjimanka Local Fauna), which has a greater facial angulation of 63°, while a second new species of Chunia, also from the Dijimanka Local Fauna, has a facial angulation of 58° and intermediate molar traits. The degree of facial shortening is a valid discriminator between species of ektopodontid marsupials as it coincides with the species level differences in dental morphology. Additionally, C. omega from the Tarkarooloo Local Fauna is placed in new genus, Ngathachunia, as it is outside of the hypodigms for both of the previously described genera, Chunia and Ektopodon. A well-supported phylogenetic hypothesis for the family indicates the species of Ektopodon form a monophyletic clade, while the species of Chunia are paraphyletic. Judd A. Case [jcase@ewu.edu], Department of Biology, Eastern Washington University, Cheney, WA 99004, USA. Case, J.A., Month, 202X. Two new species of ektopodontid marsupial from the lower deposits of the Etadunna Formation (latest Oligocene), South Australia and a phylogenetic hypothesis for the Ektopodontidae. Alcheringa XXX, X–X. ISSN 0311-5518.
{"title":"Two new species of ektopodontid marsupial from the lower deposits of the Etadunna Formation (latest Oligocene), South Australia and a phylogenetic hypothesis for the Ektopodontidae","authors":"J. Case","doi":"10.1080/03115518.2023.2227252","DOIUrl":"https://doi.org/10.1080/03115518.2023.2227252","url":null,"abstract":"Abstract Molar morphologies of the latest Oligocene genera, Chunia and Ektopodon, are easy to distinguish, but species determinations are more difficult. As more specimens have been collected, more maxillary fragments with molars and/or alveoli and a portion of the rostrum preserved are available. With a suite of maxillae now known, new ektopodontid features have revealed themselves, including the shortening of the rostrum compared to other families of contemporary possums. The facial angulation represented by the flexure of the rostrum at the boundary between P3 and the molar row results in the rostrum being angled differently than the molar row. Ektopodontids have a significantly greater angulation and thus shorter faces, compared to that seen in contemporary phalangeriform possums. Two new species of the genus Chunia, from the lower Etadunna Formation, South Australia, can be distinguished from the type species, Chunia illuminata, of the Ditjimanka Local Fauna. Differences in molar morphologies and the degree of facial angulation distinguish a new species of Chunia from the lowest faunal zone and the Minkina Local Fauna (facial angulation of 52°) from C. illuminata from the next higher faunal zone (Ditjimanka Local Fauna), which has a greater facial angulation of 63°, while a second new species of Chunia, also from the Dijimanka Local Fauna, has a facial angulation of 58° and intermediate molar traits. The degree of facial shortening is a valid discriminator between species of ektopodontid marsupials as it coincides with the species level differences in dental morphology. Additionally, C. omega from the Tarkarooloo Local Fauna is placed in new genus, Ngathachunia, as it is outside of the hypodigms for both of the previously described genera, Chunia and Ektopodon. A well-supported phylogenetic hypothesis for the family indicates the species of Ektopodon form a monophyletic clade, while the species of Chunia are paraphyletic. Judd A. Case [jcase@ewu.edu], Department of Biology, Eastern Washington University, Cheney, WA 99004, USA. Case, J.A., Month, 202X. Two new species of ektopodontid marsupial from the lower deposits of the Etadunna Formation (latest Oligocene), South Australia and a phylogenetic hypothesis for the Ektopodontidae. Alcheringa XXX, X–X. ISSN 0311-5518.","PeriodicalId":272731,"journal":{"name":"Alcheringa: An Australasian Journal of Palaeontology","volume":"116 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"2023-08-03","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"133629689","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 0
Quaternary plant macrofossils from Robertson Cave, Naracoorte, South Australia: reproductive structures 南澳大利亚Naracoorte Robertson洞穴第四纪植物宏观化石:生殖结构
Pub Date : 2023-07-03 DOI: 10.1080/03115518.2023.2246149
Rachel A. Atkins, R. Hill, K. Hill, S. Munroe, E. Reed
Abstract The World Heritage Naracoorte Caves in southeastern South Australia are important palaeontological sites known primarily for their diverse vertebrate fossils. Some of the caves also contain well-preserved Quaternary plant macrofossils, but little palaeobotanical research has been undertaken to date. Here, we describe the angiosperm plant taxa represented by macrofossils of reproductive structures that have been extracted from the Robertson Cave sediment deposit; this has an age range of 820–24,230 years BP. We identified 29 angiosperm taxa representing 20 families. These represent some of the plant species that grew in the Naracoorte region during the Quaternary, and form a database for future plant identification and palaeovegetation reconstructions. Rachel A. Atkins [rachel.atkins@adelaide.edu.au], School of Biological Sciences, The University of Adelaide, Adelaide, South Australia 5005, Australia and Environment Institute, The University of Adelaide, Adelaide, South Australia 5005, Australia; Robert S. Hill [bob.hill@adelaide.edu.au], School of Biological Sciences, The University of Adelaide, Adelaide, South Australia 5005, Australia and Environment Institute, The University of Adelaide, Adelaide, South Australia 5005, Australia; Kathryn E. Hill [kathryn@debillenvironmental.com.au], School of Biological Sciences, The University of Adelaide, Adelaide, South Australia 5005, Australia and DeBill Environmental, 13 Hawkesbury Ave, Kilburn, South Australia 5084, Australia; Samantha E.M. Munroe [Samantha.Munroe@csiro.au], School of Biological Sciences, The University of Adelaide, Adelaide, South Australia 5005; Elizabeth H. Reed [liz.reed@adelaide.edu.au], School of Biological Sciences, The University of Adelaide, Adelaide, South Australia 5005, Australia, Environment Institute, The University of Adelaide, Adelaide, South Australia 5005, Australia, and Earth and Biological Sciences (Palaeontology), South Australian Museum, Adelaide, South Australia 5000, Australia.
南澳大利亚东南部的纳拉库特洞穴是重要的古生物学遗址,主要以其多样的脊椎动物化石而闻名。一些洞穴还含有保存完好的第四纪植物大化石,但迄今为止很少进行古植物学研究。本文描述了从Robertson洞穴沉积物中提取的以生殖结构大化石为代表的被子植物分类群;年龄范围为820-24,230 BP。共鉴定出20科29个被子植物类群。这些植物代表了第四纪时期Naracoorte地区生长的一些植物物种,并为未来的植物鉴定和古植被重建建立了数据库。Rachel A. Atkins [rachel.atkins@adelaide.edu.au],阿德莱德大学生物科学学院,阿德莱德,南澳大利亚5005;阿德莱德大学环境研究所,阿德莱德,南澳大利亚5005;Robert S. Hill [bob.hill@adelaide.edu.au],阿德莱德大学生物科学学院,阿德莱德,南澳大利亚5005,澳大利亚;阿德莱德大学环境研究所,阿德莱德,南澳大利亚5005;Kathryn E. Hill [kathryn@debillenvironmental.com.au],阿德莱德大学生物科学学院,阿德莱德,南澳大利亚5005,澳大利亚;德比尔环境,13霍克斯伯里大街,基尔本,南澳大利亚5084;Samantha E.M. Munroe [Samantha.Munroe@csiro.au],阿德莱德大学生物科学学院,阿德莱德,南澳大利亚5005;Elizabeth H. Reed [liz.reed@adelaide.edu.au],阿德莱德大学生物科学学院,阿德莱德,南澳大利亚5005,澳大利亚;阿德莱德大学环境研究所,阿德莱德,南澳大利亚5005,澳大利亚;地球与生物科学(古生物学),南澳大利亚博物馆,阿德莱德,南澳大利亚5000,澳大利亚。
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引用次数: 0
Partial skeleton from the Paleocene of New Zealand illuminates the early evolutionary history of the Phaethontiformes (tropicbirds) 新西兰古新世的部分骨骼揭示了Phaethontiformes(热带鸟类)的早期进化史
Pub Date : 2023-07-03 DOI: 10.1080/03115518.2023.2246528
G. Mayr, V. D. De Pietri, L. Love, A. Mannering, E. Crouch, C. Reid, R. Scofield
Abstract We describe a new stem group representative of the Phaethontiformes (tropicbirds) from the Paleocene Waipara Greensand in New Zealand. The fossil consists of a partial skeleton with a nearly complete skull and represents the first unambiguous record of the Phaethontiformes from the Paleocene of the Southern Hemisphere. Clymenoptilon novaezealandicum gen. et sp. nov. has a proportionally shorter pelvis than Prophaethon shrubsolei from the early Eocene London Clay and appears to have been less adapted to foraging in an aquatic environment at or below sea-level. It is furthermore distinguished from P. shrubsolei and Lithoptila abdounensis from the late Paleocene/early Eocene of Morocco in a proportionally smaller foramen magnum of the skull. Together with other plesiomorphic features, this suggests that C. novaezealandicum is the sister taxon of a clade including Lithoptila, Prophaethon and crown group Phaethontiformes, and as one of the oldest stem group phaethontiforms the new species may indicate a Southern Hemispheric centre of origin of tropicbirds. After a recently described bony-toothed bird, C. novaezealandicum is the second seabird species from the Waipara Greensand to show affinities to taxa from the early Paleogene of the Northern Hemisphere. The wide early Paleogene distribution of the Phaethontiformes stands in sharp contrast to the geographic restriction of coeval diving seabirds, and different factors appear to have limited the dispersal of aquatic and pelagic seabird taxa in the early Paleogene. Gerald Mayr [Gerald.Mayr@senckenberg.de], Senckenberg Research Institute and Natural History Museum Frankfurt, Ornithological Section, Senckenberganlage 25, D-60325 Frankfurt am Main, Germany; Vanesa L. De Pietri [vanesa.depietri@canterbury.ac.nz], University of Canterbury, School of Earth and Environment, Private Bag 4800, Christchurch 8140, New Zealand; Al Mannering [alman@slingshot.co.nz], Canterbury Museum, Rolleston Avenue, Christchurch 8050, New Zealand; Leigh Love [lvlove@xtra.co.nz], PO Box 49, Waipara 7483, New Zealand; Erica Crouch [e.crouch@gns.cri.nz], GNS Science, 1 Fairway Drive, Lower Hutt 5040, New Zealand; Catherine Reid [catherine.reid@canterbury.ac.nz], University of Canterbury, School of Earth and Environment, Private Bag 4800, Christchurch 8140, New Zealand; R. Paul Scofield [pscofield@canterburymuseum.com], Canterbury Museum, Rolleston Avenue, Christchurch 8050, New Zealand, and University of Canterbury, School of Earth and Environment, Private Bag 4800, Christchurch 8140, New Zealand.
摘要描述了新西兰怀帕拉格林桑古新世Phaethontiformes(热带鸟类)的一个新的茎群代表。该化石由部分骨架和一个几乎完整的头骨组成,代表了南半球古新世Phaethontiformes的第一个明确记录。在始新世早期的伦敦粘土中,novaezealandicum gen. et sp. 11 .的盆骨比Prophaethon shrubsolei的盆骨短,似乎不太适应在海平面或海平面以下的水生环境中觅食。此外,它与摩洛哥古新世晚期/始新世早期的P. shrubsolei和Lithoptila abdounensis的区别在于头骨的大孔相对较小。结合其他多形性特征,这表明C. novaezealandicum是包括Lithoptila, Prophaethon和crown group Phaethontiformes在内的分支的姐妹分类群,并且作为最古老的茎组Phaethontiformes之一,该新种可能表明热带鸟类的起源中心位于南半球。在最近发现的一种骨齿鸟之后,C. novaezealandicum是来自怀帕拉格林桑的第二个与北半球早期古近纪类群有亲缘关系的海鸟物种。古近纪早期phaethalloformes的广泛分布与同时期潜水海鸟的地理限制形成鲜明对比,不同的因素似乎限制了古近纪早期水生和远洋海鸟类群的分布。Gerald Mayr [Gerald.Mayr@senckenberg.de], Senckenberg研究所和法兰克福自然历史博物馆,鸟类科,Senckenberg lagage 25, D-60325 Frankfurt am Main,德国;Vanesa L. De Pietri [vanesa.depietri@canterbury.ac.nz],坎特伯雷大学地球与环境学院,Private Bag 4800,基督城8140,新西兰;阿尔·曼纳林[alman@slingshot.co.nz],坎特伯雷博物馆,罗勒斯顿大道,新西兰克赖斯特彻奇8050;Leigh Love [lvlove@xtra.co.nz],新西兰怀帕拉7483邮政信箱49号;Erica Crouch [e.crouch@gns.cri.nz], GNS Science, 1 Fairway Drive, Lower Hutt 5040,新西兰;Catherine Reid [catherine.reid@canterbury.ac.nz],坎特伯雷大学地球与环境学院,Private Bag 4800,基督城8140,新西兰;R. Paul Scofield [pscofield@canterburymuseum.com],坎特伯雷博物馆,罗勒斯顿大道,基督城8050,新西兰;坎特伯雷大学,地球与环境学院,私人袋4800,基督城8140,新西兰。
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引用次数: 0
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Alcheringa: An Australasian Journal of Palaeontology
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