Pub Date : 2016-01-01DOI: 10.24199/J.MMV.2016.74.05
F. Novas, A. M. A. Rolando, F. Agnolín
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Pub Date : 2016-01-01DOI: 10.24199/J.MMV.2016.74.02
J. Long
Long, J.A. 2016. Quantifying scientific significance of a fossil site: the Gogo Fossil sites (Late Devonian, Western Australia) as a case study. Memoirs of Museum Victoria 74: 5–15. Assessing the scientific significance of fossil sites has up to now been largely a matter of subjective opinion with few or no metrics being employed. By applying similar metrics used for assessing academic performance, both qualitative and quantitative, to fossil sites we gain a real indication of their significance that enables direct comparison with other sites both nationally and globally. Indices suggested are those using total pages published for both peer-reviewed and combined peer-reviewed and popular publications, total citations from the papers, total impact points for site (citing palaeontologyrelated papers only), total number of very high impact papers (VHIP; journal impact factor>30) and social media metrics. These provide a measure of how much the published fossil data from a site has been utilised. The Late Devonian fossils of the Gogo Formation of Western Australia are here used as an example of how these metrics can be applied. The Gogo sites for example, have produced c.4384 pages of peer-reviewed papers (c.5458 total combined with popular works); generated papers with a total impact point score of 611, including 10 VHI papers, and generated 4009 citations. The sites have an overall h-index of 33. Combing these into a Scientific Site Significance Index (SSSI) will permit direct comparisons of site significance to be made for initiating discussions about site protection, tourism, geopark status, local heritage listings or potential future world heritage nominations.
Long, J.A. 2016。化石遗址的科学意义量化:以澳大利亚西部晚泥盆纪Gogo化石遗址为例。维多利亚博物馆回忆录74:5-15。到目前为止,评估化石遗址的科学意义在很大程度上是一个主观意见的问题,很少或根本没有使用指标。通过将用于评估学术表现的类似指标(定性和定量)应用于化石遗址,我们获得了其重要性的真实指示,从而可以与国内和全球其他遗址进行直接比较。建议的索引是使用同行评议和综合同行评议和流行出版物的总页数,论文的总引用,站点的总影响点(仅引用古生物相关论文),非常高影响论文的总数(VHIP;期刊影响因子>30)和社交媒体指标。它们提供了一种测量方法,可以衡量一个地点公布的化石数据被利用了多少。这里以西澳大利亚州Gogo组的晚泥盆世化石为例,说明如何应用这些指标。例如,Gogo网站已经产生了4384页的同行评议论文(加上流行作品总共5458页);生成的论文总影响点得分为611,其中VHI论文10篇,产生4009次引用。这些网站的总体h指数为33。将这些数据整合到科学遗址重要性指数(SSSI)中,可以对遗址的重要性进行直接比较,从而启动有关遗址保护、旅游、地质公园地位、当地遗产名录或潜在的未来世界遗产提名的讨论。
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Pub Date : 2016-01-01DOI: 10.24199/J.MMV.2016.74.13
M. Archer, Olivia Christmas, S. Hand, K. Black, P. Creaser, H. Godthelp, I. Graham, D. Cohen, D. A. Arena, Caitlin Anderson, G. Soares, Naomi Machin, R. Beck, L. A. Wilson, Troy J Myers, A. Gillespie, B. Khoo, K. Travouillon
Whollydooleya tomnpatrichorum gen. et sp. nov. is a new, highly specialised hypercarnivorous dasyuromorphian from a new mid-Cenozoic limestone deposit southwest of the Riversleigh World Heritage Area in northwestern Queensland. Dental dimensions suggest it may have weighed at least twice as much as the living Tasmanian devil (Sarcophilus harrisii). Although known only from a lower molar, it exhibits a plethora of carnivorous adaptations including a hypertrophied protoconid, tiny metaconid and a battery of vertical carnassial blades between most of the major cusps, most of which incorporate carnassial notches to immobilise materials being sheared. It is unique among dasyuromorphians in having a massive entoconid that closes the entire lingual side of the talonid. Comparison with previously known thylacinid and dasyurid hypercarnivores suggests its relationships are closer to dasyurids than thylacinids in the main because of the very large entoconid, a cusp that is relatively small to absent in all known thylacinids but commonly small to large in dasyurids. However, the extent of enlargement of the entoconid suggests that it is not closely related to previously known Cenozoic hypercarnivorous dasyurids in the genera Dasyurus, Glaucodon, Sarcophilus or any of the other previously described Cenozoic dasyurids. Although the early late Miocene Ganbulanyi djadjinguli is only known from an upper molar, the reduced area of its protocone suggests a correspondingly reduced rather than hypertrophied entoconid in its as-yet-unknown lower molars. Reconsideration of the structure of the talonid in species of Sarcophilus even suggests that within that Quaternary lineage, the entoconid may have been entirely lost, with the posteriorly displaced metaconid taking its functional place as an occlusal counterpart for the blades of the protocone. The large size of the new species signals the earliest indication within the dasyurid radiation of a late Cenozoic trend towards gigantism that became evident in many lineages of Australian marsupials. While the age is uncertain, on the basis of associated taxa such as species of Ekaltadeta, it is probably either mid or late Miocene in age. Geological features of the deposit suggest it was formed within a pool in a cave environment that periodically underwent desiccation. Some grains suggest an aeolian as well as an alluvial and pluvial origin for the deposit. This may relate to current understanding about environmental change that took place in the region following the mid Miocene climate oscillation.
在昆士兰州西北部的里弗斯利世界遗产区西南的一个新的中新生代石灰岩矿床中,发现了一种新的、高度特化的高肉食性大形态动物(Whollydooleya tomnpatrichorum gen. et sp. 11)。牙齿尺寸表明,它的体重可能至少是现存塔斯马尼亚魔鬼(Sarcophilus harrisii)的两倍。虽然只从下臼齿中发现,但它表现出了大量的食肉性适应,包括肥大的原锥体、微小的后锥体和大多数主要尖头之间的一系列垂直肉食叶片,其中大多数都包含肉食切口,以固定被剪切的材料。它的独特之处在于它有一个巨大的内突,封闭了整个舌侧的距骨。与先前已知的袋狼类和袋狼类超食肉动物的比较表明,它与袋狼类的关系比袋狼类更接近,主要是因为它有非常大的内圆锥,一个在所有已知的袋狼类中相对较小或没有的尖,而在袋狼类中通常从小到大。然而,内圆锥的扩大程度表明,它与先前已知的新生代Dasyurus属、Glaucodon属、Sarcophilus属或任何其他先前描述的新生代dasyurids没有密切的关系。虽然晚中新世早期Ganbulanyi djadjinguli仅从上磨牙得知,但其原锥体面积的减少表明其下磨牙的内锥体相应减少,而不是肥大。对Sarcophilus物种的talonid结构的重新考虑甚至表明,在第四纪谱系中,内锥体可能已经完全消失,后移位的后锥体取代了原锥体叶片的功能位置。新物种的巨大体型标志着在新生代晚期的dasyurid辐射中最早的迹象,这种趋势在澳大利亚有袋动物的许多谱系中都很明显。虽然时代不确定,但根据相关分类群,如Ekaltadeta种,其时代可能是中新世中期或晚中新世。该矿床的地质特征表明,它是在一个周期性经历干燥的洞穴环境中的一个水池中形成的。一些颗粒表明,该矿床的成因既可能是风成的,也可能是冲积和洪积的。这可能与目前对中新世中期气候振荡后该地区发生的环境变化的理解有关。
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Pub Date : 2016-01-01DOI: 10.24199/J.MMV.2016.74.08
Doris Seegets-Villiers, B. Wagstaff
Seegets-Villiers, D.E. and Wagstaff, B.E. 2016. Morphological variation of stratigraphically important species in the genus Pilosisporites Delcourt & Sprumont, 1955 in the Gippsland Basin, southeastern Australia. Memoirs of Museum Victoria 74: 81–91. Three hundred and ninety eight mudstone samples of Early Cretaceous age from the onshore part of the Gippsland Basin in southeastern Australia were used to ascertain the morphological variation in three species of spores in the genus Pilosisporites. In Australia all species of Pilosisporites are biostratigraphically useful and this study confirms that in the Gippsland Basin the ranges of Pilosisporites notensis, Pilosisporites parvispinosus and Pilosisporites grandis are as defined by some previous authors. Morphological variations of these three taxa from the published descriptions are discussed. In the case of P. grandis and P. parvispinosus the main variation was in the size of specimens, however P. notensis showed sculpture variations in regard to element size, type and distribution. Two distinct types of this species were defined with only one occurring in the youngest part of the section. Modern fern species can exhibit similar spore sculpture and size variations as a result of polyploidy. This could possibly be the cause of the variations in all three species of Pilosisporites and also their short-lived, in geological terms, species ranges.
Seegets-Villiers, D.E.和Wagstaff, B.E. 2016。Delcourt & Sprumont, 1955年在澳大利亚东南部的Gippsland盆地发现的具有重要地层学意义的Pilosisporites属物种的形态变化。维多利亚博物馆回忆录74:81-91。本文利用澳大利亚东南部吉普斯兰盆地陆上早白垩世的338个泥岩样本,确定了毛孢属3种孢子的形态变异。在澳大利亚,所有的Pilosisporites都具有生物地层学意义,本研究证实了在Gippsland盆地,Pilosisporites notensis、Pilosisporites parvispinosus和Pilosisporites grandis的分布范围与前人的定义一致。从已发表的描述中讨论了这三个分类群的形态变化。大种属和小种属的差异主要表现在标本的大小上,而小种属在元素的大小、类型和分布上表现出雕刻性差异。这个物种被定义为两种不同的类型,只有一种出现在该剖面最年轻的部分。由于多倍体,现代蕨类植物可以表现出类似的孢子雕刻和大小变化。这可能是所有三种毛氏岩的差异的原因,也可能是它们短暂的地质物种范围的原因。
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Pub Date : 2016-01-01DOI: 10.24199/J.MMV.2016.74.22
Ernest L. Lundelelius
{"title":"Palorchestes from the Pliocene Hamilton Local Fauna, Victoria, Australia","authors":"Ernest L. Lundelelius","doi":"10.24199/J.MMV.2016.74.22","DOIUrl":"https://doi.org/10.24199/J.MMV.2016.74.22","url":null,"abstract":"","PeriodicalId":53647,"journal":{"name":"Memoirs of Museum Victoria","volume":"29 1","pages":"325-330"},"PeriodicalIF":0.0,"publicationDate":"2016-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"90806689","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}
Pub Date : 2016-01-01DOI: 10.24199/J.MMV.2016.74.12
E. Fitzgerald
Fitzgerald, E.M.G. 2016. A late Oligocene waipatiid dolphin (Odontoceti: Waipatiidae) from Victoria, Australia. Memoirs of Museum Victoria 74: 117–136. A partial odontocete skeleton comprising isolated teeth, forelimb elements, ribs, and vertebrae is described from the upper Oligocene (Chattian) Jan Juc Marl of Jan Juc, Victoria, southeast Australia. Its dental and forelimb characters most closely resemble those of the late Oligocene Waipatia and Sulakocetus from New Zealand and the Caucasus, respectively; thus the Jan Juc odontocete is referred to an indeterminate species in the family Waipatiidae (Platanistoidea). This specimen represents the first report of Waipatiidae in Australia, expands the taxonomic diversity of Australian Oligocene Cetacea, and shows that Waipatiidae occurred in the Chattian cetacean assemblages of both Australia and New Zealand.
菲茨杰拉德,E.M.G. 2016。澳洲维多利亚晚渐新世怀氏海豚(齿鲸科:怀氏海豚科)。维多利亚博物馆回忆录74:117-136。在澳大利亚东南部维多利亚州Jan Juc的上渐新世(Chattian) Jan Juc marc中,描述了一具由孤立的牙齿、前肢元素、肋骨和椎骨组成的部分齿齿动物骨架。牙齿和前肢特征分别与新西兰晚渐新世的Waipatia和高加索地区的Sulakocetus最为相似;因此,Jan Juc齿齿兽是指在Waipatiidae (platanisto总科)的一个不确定的物种。该标本是澳大利亚首次报道的Waipatiidae,扩大了澳大利亚渐新世鲸目的分类多样性,表明Waipatiidae出现在澳大利亚和新西兰的Chattian鲸目组合中。
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Pub Date : 2016-01-01DOI: 10.24199/J.MMV.2016.74.15
N. Pledge
Pledge, N.S. 2016. New specimens of ektopodontids (Marsupialia: Ektopodontidae) from South Australia. Memoirs of Museum Victoria 74: 173–187. Knowledge about the extinct phalangeroid family Ektopodontidae is increased by the discovery of new material from several localities. Previously unknown teeth of Chunia illuminata and Ektopodon stirtoni are described respectively from White Sands Basin and Mammalon Hill, Lake Palankarinna, Lake Eyre Basin, South Australia, with M1 being recorded for the first time for any species of Chunia., and a full maxilla of Ektopodon stirtoni showing the positional relationship between P3 and M1 for the first time; this is even more extreme than the arrangement postulated previously. Another species Ektopodon litolophus has been described on the basis of an M1 found at the Leaf Locality, Lake Ngapakaldi, Lake Eyre Basin. Material from Lake Tarkarooloo, referred to Ektopodon stirtoni, is redescribed as a new species Ektopodon tommosi. Comparisons of M1 of Chunia and Ektopodon species now allow evolutionary trends, such as increasing number of cusps on the molar lophs, and simplification of the cusps, to be discerned.
{"title":"New specimens of ektopodontids (Marsupialia: Ektopodontidae) from South Australia","authors":"N. Pledge","doi":"10.24199/J.MMV.2016.74.15","DOIUrl":"https://doi.org/10.24199/J.MMV.2016.74.15","url":null,"abstract":"Pledge, N.S. 2016. New specimens of ektopodontids (Marsupialia: Ektopodontidae) from South Australia. Memoirs of Museum Victoria 74: 173–187. Knowledge about the extinct phalangeroid family Ektopodontidae is increased by the discovery of new material from several localities. Previously unknown teeth of Chunia illuminata and Ektopodon stirtoni are described respectively from White Sands Basin and Mammalon Hill, Lake Palankarinna, Lake Eyre Basin, South Australia, with M1 being recorded for the first time for any species of Chunia., and a full maxilla of Ektopodon stirtoni showing the positional relationship between P3 and M1 for the first time; this is even more extreme than the arrangement postulated previously. Another species Ektopodon litolophus has been described on the basis of an M1 found at the Leaf Locality, Lake Ngapakaldi, Lake Eyre Basin. Material from Lake Tarkarooloo, referred to Ektopodon stirtoni, is redescribed as a new species Ektopodon tommosi. Comparisons of M1 of Chunia and Ektopodon species now allow evolutionary trends, such as increasing number of cusps on the molar lophs, and simplification of the cusps, to be discerned.","PeriodicalId":53647,"journal":{"name":"Memoirs of Museum Victoria","volume":"121 1","pages":"173-187"},"PeriodicalIF":0.0,"publicationDate":"2016-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"78426746","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}
Pub Date : 2016-01-01DOI: 10.24199/J.MMV.2016.74.20
L. Schwartz
Schwartz, L.R.S. 2016. A revised faunal list and geological setting for Bullock Creek, a Camfieldian site from the Northern Territory of Australia. Memoirs of Museum Victoria 74: 263–290. The Camfield beds, in which the Bullock Creek Local Fauna occurs, is a freshwater carbonate unit deposited in a braided-meandering river environment in which abandoned channels formed oxbow lakes. Fossil quarries in the Small Hills outcrop occur in stratigraphically superposed beds. Despite this, there are no detectable changes to the fauna obtained at different levels that demonstrate a significant biochronologic time difference. Within the small mammal fauna, macropodoids are the most abundant group at Bullock Creek. Two species have been described, Balbaroo camfieldensis and Nambaroo bullockensis. A number of other macropodid taxa are also present. A diverse ‘possum’ fauna is found here, in addition to the miralinids Barguru maru and Barguru kayir, including the phalangerid Wyulda sp. cf. asherjoeli. Dasyuromorphians are also present, as are yaraloid peramelemorphians, including a species referred to Yarala.
{"title":"A revised faunal list and geological setting for Bullock Creek, a Camfieldian site from the Northern Territory of Australia","authors":"L. Schwartz","doi":"10.24199/J.MMV.2016.74.20","DOIUrl":"https://doi.org/10.24199/J.MMV.2016.74.20","url":null,"abstract":"Schwartz, L.R.S. 2016. A revised faunal list and geological setting for Bullock Creek, a Camfieldian site from the Northern Territory of Australia. Memoirs of Museum Victoria 74: 263–290. The Camfield beds, in which the Bullock Creek Local Fauna occurs, is a freshwater carbonate unit deposited in a braided-meandering river environment in which abandoned channels formed oxbow lakes. Fossil quarries in the Small Hills outcrop occur in stratigraphically superposed beds. Despite this, there are no detectable changes to the fauna obtained at different levels that demonstrate a significant biochronologic time difference. Within the small mammal fauna, macropodoids are the most abundant group at Bullock Creek. Two species have been described, Balbaroo camfieldensis and Nambaroo bullockensis. A number of other macropodid taxa are also present. A diverse ‘possum’ fauna is found here, in addition to the miralinids Barguru maru and Barguru kayir, including the phalangerid Wyulda sp. cf. asherjoeli. Dasyuromorphians are also present, as are yaraloid peramelemorphians, including a species referred to Yarala.","PeriodicalId":53647,"journal":{"name":"Memoirs of Museum Victoria","volume":"NS20 8 1","pages":"263-290"},"PeriodicalIF":0.0,"publicationDate":"2016-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"77829488","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}
Pub Date : 2016-01-01DOI: 10.24199/J.MMV.2016.74.14
R. Beck, N. Warburton, M. Archer, S. Hand, K. Aplin
We present the first detailed descriptions of postcranial elements of the fossil marsupial mole Naraboryctes philcreaseri (Marsupialia: Notoryctemorphia), from early Miocene freshwater limestone deposits in the Riversleigh World Heritage Area, northwestern Queensland. Qualitative functional analysis of these elements suggest that Na. philcreaseri was very well-adapted for burrowing, albeit somewhat less so than the living marsupial moles Notoryctes typhlops and N. caurinus. Quadratic discriminant analysis of limb measurements suggests that Na. philcreaseri was subterranean, and its Index of Fossorial Ability is almost identical to that of Notoryctes species, being among the highest known for any mammal. These results suggest that notoryctemorphians evolved their specialised, “mole-like” subterranean lifestyle prior to the early Miocene. Given that forested environments predominated in Australia until the middle-late Miocene, this transition to subterranean behaviour may have occurred via burrowing in forest floors, in which case fossorial mammals that live in tropical rainforests today (such as the placental golden moles Chrysospalax trevelyani and Huetia leucorhina) may represent reasonable living analogues for early notoryctemorphians. However, alternative scenarios, such as a cave-dwelling or semi-aquatic ancestry, should be considered. Phylogenetic analysis using a Bayesian total evidence dating approach places Naraboryctes as sister to Notoryctes with strong support (Bayesian posterior probability = 0.91), and indicates that Naraboryctes and Notoryctes diverged 30.3 MYA (95% HPD: 17.7-46.3 MYA). The age and known morphology of Na. philcreaseri does not preclude its being ancestral to Notoryctes. Using estimates of divergence times and ratios of nonsynonymous to synonymous substitutions per site, we infer that the nuclear gene “Retinol-binding protein 3, interstitial” (RBP3), which plays a key role in vision, became inactive in the Notoryctes lineage ~5.4 MYA (95% HPD: 4.5-6.3 MYA). This is much younger than previous published estimates, and postdates considerably the age of Na. philcreaseri, implying that RBP3 was active in this fossil taxon; hence, Na. philcreaseri may have retained a functional visual system. Our estimate for the inactivation of RBP3 in the Notoryctes lineage coincides with palaeobotanical evidence for a major increase in the abundance of grasses in Australia, which may indicate the appearance of more open environments, and hence selection pressure on notoryctemorphians to spend less time on the surface, leading to relaxed selection on RBP3. Ultimately, however, a fuller understanding of the origin and evolution of notoryctemorphians-including when and why they became “mole-like”-will require improvements in the Palaeogene fossil record of mammals in Australia
{"title":"Going underground: Postcranial morphology of the early miocene marsupial mole naraboryctes philcreaseri and the evolution of fossoriality in notoryctemorphians","authors":"R. Beck, N. Warburton, M. Archer, S. Hand, K. Aplin","doi":"10.24199/J.MMV.2016.74.14","DOIUrl":"https://doi.org/10.24199/J.MMV.2016.74.14","url":null,"abstract":"We present the first detailed descriptions of postcranial elements of the fossil marsupial mole Naraboryctes philcreaseri (Marsupialia: Notoryctemorphia), from early Miocene freshwater limestone deposits in the Riversleigh World Heritage Area, northwestern Queensland. Qualitative functional analysis of these elements suggest that Na. philcreaseri was very well-adapted for burrowing, albeit somewhat less so than the living marsupial moles Notoryctes typhlops and N. caurinus. Quadratic discriminant analysis of limb measurements suggests that Na. philcreaseri was subterranean, and its Index of Fossorial Ability is almost identical to that of Notoryctes species, being among the highest known for any mammal. These results suggest that notoryctemorphians evolved their specialised, “mole-like” subterranean lifestyle prior to the early Miocene. Given that forested environments predominated in Australia until the middle-late Miocene, this transition to subterranean behaviour may have occurred via burrowing in forest floors, in which case fossorial mammals that live in tropical rainforests today (such as the placental golden moles Chrysospalax trevelyani and Huetia leucorhina) may represent reasonable living analogues for early notoryctemorphians. However, alternative scenarios, such as a cave-dwelling or semi-aquatic ancestry, should be considered. Phylogenetic analysis using a Bayesian total evidence dating approach places Naraboryctes as sister to Notoryctes with strong support (Bayesian posterior probability = 0.91), and indicates that Naraboryctes and Notoryctes diverged 30.3 MYA (95% HPD: 17.7-46.3 MYA). The age and known morphology of Na. philcreaseri does not preclude its being ancestral to Notoryctes. Using estimates of divergence times and ratios of nonsynonymous to synonymous substitutions per site, we infer that the nuclear gene “Retinol-binding protein 3, interstitial” (RBP3), which plays a key role in vision, became inactive in the Notoryctes lineage ~5.4 MYA (95% HPD: 4.5-6.3 MYA). This is much younger than previous published estimates, and postdates considerably the age of Na. philcreaseri, implying that RBP3 was active in this fossil taxon; hence, Na. philcreaseri may have retained a functional visual system. Our estimate for the inactivation of RBP3 in the Notoryctes lineage coincides with palaeobotanical evidence for a major increase in the abundance of grasses in Australia, which may indicate the appearance of more open environments, and hence selection pressure on notoryctemorphians to spend less time on the surface, leading to relaxed selection on RBP3. Ultimately, however, a fuller understanding of the origin and evolution of notoryctemorphians-including when and why they became “mole-like”-will require improvements in the Palaeogene fossil record of mammals in Australia","PeriodicalId":53647,"journal":{"name":"Memoirs of Museum Victoria","volume":"54 1","pages":"151-171"},"PeriodicalIF":0.0,"publicationDate":"2016-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"81319219","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}
Pub Date : 2016-01-01DOI: 10.24199/J.MMV.2016.74.28
M. Tyler, G. Prideaux
Tyler, M.J. and Prideaux, G.J. 2016. Early to middle Pleistocene occurrences of Litoria, Neobatrachus and Pseudophryne (Anura) from the Nullarbor Plain, Australia: first frogs from the “frog-free zone”. Memoirs of Museum Victoria 74: 403–408. Frogs have the least understood fossil record of all major vertebrate groups in Australia. Here we report on pelvic remains of three Pleistocene frog species from the Nullarbor Plain, a large region of Australia where no living or fossil frogs had previously been discovered. One ilium, characterised by a small acetabular fossa with an indistinct peripheral rim, a broad dorsal prominence and enlarged supra-acetabular zone, is recognised here as representative of a new species of hylid, Litoria lundeliusi sp. nov. Three other ilia bear the hallmark generic attributes of the small myobatrachid Pseudophryne, two species of which co-occur today over much of southwestern Australia. A second larger myobatrachid is the best represented of the three species, and its ilial morphology matches that of the extant Neobatrachus sudelli. All three species were present in the early Pleistocene, but only N. sudelli is recorded in the middle Pleistocene. The loss of Litoria and Pseudophryne would be consistent with the disappearance of significant bodies of free water from the region, but the cause of the apparent extirpation of N. sudelli, which inhabits arid parts of Australia today, remains a mystery.
{"title":"Early to middle Pleistocene occurrences of Litoria, Neobatrachus and Pseudophryne (Anura) from the Nullarbor Plain, Australia: first frogs from the “frog-free zone”","authors":"M. Tyler, G. Prideaux","doi":"10.24199/J.MMV.2016.74.28","DOIUrl":"https://doi.org/10.24199/J.MMV.2016.74.28","url":null,"abstract":"Tyler, M.J. and Prideaux, G.J. 2016. Early to middle Pleistocene occurrences of Litoria, Neobatrachus and Pseudophryne (Anura) from the Nullarbor Plain, Australia: first frogs from the “frog-free zone”. Memoirs of Museum Victoria 74: 403–408. Frogs have the least understood fossil record of all major vertebrate groups in Australia. Here we report on pelvic remains of three Pleistocene frog species from the Nullarbor Plain, a large region of Australia where no living or fossil frogs had previously been discovered. One ilium, characterised by a small acetabular fossa with an indistinct peripheral rim, a broad dorsal prominence and enlarged supra-acetabular zone, is recognised here as representative of a new species of hylid, Litoria lundeliusi sp. nov. Three other ilia bear the hallmark generic attributes of the small myobatrachid Pseudophryne, two species of which co-occur today over much of southwestern Australia. A second larger myobatrachid is the best represented of the three species, and its ilial morphology matches that of the extant Neobatrachus sudelli. All three species were present in the early Pleistocene, but only N. sudelli is recorded in the middle Pleistocene. The loss of Litoria and Pseudophryne would be consistent with the disappearance of significant bodies of free water from the region, but the cause of the apparent extirpation of N. sudelli, which inhabits arid parts of Australia today, remains a mystery.","PeriodicalId":53647,"journal":{"name":"Memoirs of Museum Victoria","volume":"113 1","pages":"403-408"},"PeriodicalIF":0.0,"publicationDate":"2016-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"76804898","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}