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Oldest record of Alligator in southeastern North America 北美洲东南部最古老的短吻鳄记录
IF 2 4区 地球科学 Q1 Earth and Planetary Sciences Pub Date : 2023-01-01 DOI: 10.26879/1223
Alexander K. Hastings, B. Schubert, Jason R. Bourque, R. Hulbert
The genus Alligator has been represented by large-bodied, predatory species in southeastern North America for at least 18 million years (early Miocene), in what is now the southeastern United States. However, the first occurrences of the genus were from a smaller-bodied species, A. prenasalis , known from South Dakota and Nebraska that are about 34 million years old (latest Eocene to earliest Oligocene). Ancestors of A. prenasalis were likewise small-bodied and are from the Great Plains. This 16 mil-lion-year-gap has left open questions regarding the arrival and body size shift of Alligator from what is now the Great Plains to southeastern North America. Recently studied fossil material from Florida exhibits the oldest occurrence of Alligator in the region (about 28–26 million years ago). A well-preserved premaxilla (UF 422816) bears the diagnostic premaxillary 'notch' of Alligator . Additional material from this and two other Oligocene sites in Florida are indicative of Alligator as well. These include well-devel-oped osteoderms, which suggest possible maturity at small body size. As of now, no records of larger Alligator from this time (or older) have been recovered from the region, possibly indicating body size may not have increased in Alligator until the Miocene
短吻鳄属以体型庞大的掠食性物种为代表,在北美东南部(中新世早期)至少有1800万年的历史,也就是现在的美国东南部。然而,该属的第一次出现是来自一个体型较小的物种,a . prenasalis,已知于南达科他州和内布拉斯加州,大约有3400万年的历史(始新世晚期到渐新世早期)。A. prenasalis的祖先同样体型小,来自大平原。这一千六百万年的差距留下了关于短吻鳄从现在的大平原到北美东南部的到来和体型变化的悬而未决的问题。最近研究了佛罗里达的化石材料,发现了该地区最古老的短吻鳄(大约2800万到2600万年前)。保存完好的前颌(UF 422816)具有鳄鱼的诊断前颌“缺口”。来自这个和佛罗里达另外两个渐新世遗址的其他材料也表明短吻鳄存在。这些包括发育良好的骨皮,这表明可能在小的体型下成熟。到目前为止,在该地区还没有发现这个时期(或更早时期)更大的短吻鳄的记录,这可能表明短吻鳄的体型直到中新世才增加
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引用次数: 0
New species and evolution of the foraminiferal family Janischewskinidae in the middle–upper Mississippian of South China 华南中-上密西西比有孔虫科Janischewskinidae新种及其演化
IF 2 4区 地球科学 Q1 Earth and Planetary Sciences Pub Date : 2023-01-01 DOI: 10.26879/1238
Chaolu Liu, D. Vachard, P. Pedro, I. Coronado
Rich foraminiferal assemblages from the Bama Platform in South China allow clarifying the systematics, composition, and biostratigraphy of the family Janischewski-nidae. The family is comprised of four genera, Janischewskina, Cribrospira, Bibradya, and Parajanischewskina . The genera Rhodesinella and Groessensella are considered to be synonyms of Cribrospira and Bibradya , respectively
华南巴马台地丰富的有孔虫组合有助于澄清Janischewski-nidae科的系统、组成和生物地层学。该科由四个属组成,Janischewskina, Cribrospira, Bibradya和Parajanischewskina。Rhodesinella属和Groessensella属分别被认为是Cribrospira和Bibradya的同义词
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引用次数: 0
The Middle Devonian acanthodian Orcadacanthus n. gen. from the Orcadian Basin of Scotland 产于苏格兰奥克迪亚盆地的中泥盆世棘棘蛇属
IF 2 4区 地球科学 Q1 Earth and Planetary Sciences Pub Date : 2023-01-01 DOI: 10.26879/1240
M. Newman, Jan de Blaauwen, C. Burrow, Roger Jones, R. Davidson
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引用次数: 1
The anatomy and diversity of the pterosaurian sternum 翼龙胸骨的解剖结构和多样性
IF 2 4区 地球科学 Q1 Earth and Planetary Sciences Pub Date : 2023-01-01 DOI: 10.26879/1261
D. Hone
,
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引用次数: 0
Approaching the Khersonian Crisis: Fish otoliths from the upper Bessarabian (middle Sarmatian s.l.; Late Miocene) of Jurkine (Kerch Peninsula, Crimea) 接近Khersonian危机:来自上Bessarabian(中萨尔马泰s.l)的鱼耳石晚中新世)Jurkine(克里米亚刻赤半岛)
IF 2 4区 地球科学 Q1 Earth and Planetary Sciences Pub Date : 2023-01-01 DOI: 10.26879/1300
W. Schwarzhans, A. Bratishko, Y. Vernyhorova
After its separation from the world ocean, the Paratethys formed a large inland marine water body during the Serravallian and Tortonian (Middle to Late Miocene) with a diverse environmental setting that underwent multiple fast and short-lived ecological changes. The trapped bony fish fauna either adapted to the rapid ecological changes (forced endemism) or perished. A major event during the late Sarmatian s.l. (Kherso-nian; late Tortonian; Late Miocene) was the Khersonian Crisis in the Eastern Para-tethys, which is postulated to have
Paratethys与世界海洋分离后,在Serravallian和Tortonian(中新世中晚)形成了一个大型内陆海洋水体,其环境背景多样,经历了多次快速而短暂的生态变化。被困硬骨鱼区系要么适应了快速的生态变化(强迫地方性),要么灭绝。萨尔马提亚晚期的一件大事。托尔顿阶后期;晚中新世)是东部Para-tethys的Khersonian危机,这被认为是有
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引用次数: 0
New primates from the Eocene of Saskatchewan, Canada: Revision of the primates from the Cypress Hills Formation with description of new taxa 加拿大萨斯喀彻温省始新世灵长类新种:柏树山组灵长类新种的修订及新分类群描述
IF 2 4区 地球科学 Q1 Earth and Planetary Sciences Pub Date : 2023-01-01 DOI: 10.26879/1246
Jonathan M. G. Perry, A. Dutchak, J. Theodor
True primates in the Canadian fossil record are known from only the Eocene epoch of southwestern Saskatchewan. They were originally described in the 1980s from two sets of localities: the Lac Pelletier localities (Duchesnean) and the Swift Current Creek (SCC) locality (Uintan). Additional fieldwork and sample sorting were carried out over the last decade. The present study includes a description of new primate dental material from the Swift Current Creek (SCC) locality. We name a new genus and two new species and revise the known primates for both the Lac Pelletier and SCC faunas. The Cypress Hills region of Saskatchewan likely represented a haven for small primates in the Eocene and may have supported an endemic primate fauna.
在加拿大的化石记录中,真正的灵长类动物只出现在萨斯喀彻温省西南部的始新世。它们最初是在20世纪80年代从两个地方描述的:Lac Pelletier地区(Duchesnean)和Swift Current Creek (SCC)地区(Uintan)。在过去十年中进行了额外的实地调查和样本分类。目前的研究包括对Swift Current Creek (SCC)地区新的灵长类动物牙齿材料的描述。我们命名了一个新属和两个新种,并修改了Lac Pelletier和SCC动物群的已知灵长类动物。萨斯喀彻温省的柏树山地区可能代表了始新世小型灵长类动物的避难所,并可能支持特有的灵长类动物群。
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引用次数: 0
A Pliocene goodeid fish of the Paleolake Amajac, Sanctórum, Hidalgo, Mexico 墨西哥伊达尔戈Sanctórum古阿马亚克湖的一条上新世好鱼
IF 2 4区 地球科学 Q1 Earth and Planetary Sciences Pub Date : 2023-01-01 DOI: 10.26879/1259
C. Caballero-Viñas, J. Alvarado‐Ortega, Kleyton Magno Cantalice Severiano
The splitfin fossil species Paleocharacodon guzmanae gen. and sp. nov. is erected based on the osteological study of 14 fossil male and female specimens recovered in the Pliocene deposits of the Paleolake Amajac, in Sanctórum, Hidalgo, Mexico. This new cyprinodontiform fish exhibits the diagnostic features of the family Goodeidae and subfamily Goodeinae; like all the goodeids, its premaxilla has a straight distal end, and its premaxillary ascending process is small; and, like the goodeines, this new species was viviparous, its first anal fin ray is rudimentary, and the males show an andropodium. Although P. guzmanae displays numerous primitive features, it is not possible to place it in any of the goodeine tribes, which currently are vaguely defined by osteological features. This new species seems to be closely related to Characodon; both share a peculiar osteological character; the articular facet for the quadrate is a donut-like structure, in which the retroarticular forms the central region, and a couple of semicircular anguloarticular processes form the surrounding part. This species differs from other goodeids mainly in two features; it has a posttemporal bone with small anteroventral processes, and the openings of its supraorbital canal show the formula12a, 2b-3a, 3b-4a, 4b-5a, and 5b-7. The discovery of this extinct goodeid species in the great Pánuco-Salado Basin on the eastern slope of Mexican territory represents an unexpected historical element. Carmen Caballero-Viñas. Departamento de Paleontología, Instituto de Geología, Universidad Nacional Autónoma de México. Circuito de la Investigación S/N, Ciudad Universitaria, Coyoacán, Ciudad de México, 04510, Mexico. c-caballero@live.com.mx Jesús Alvarado-Ortega. Departamento de Paleontología, Instituto de Geología, Universidad Nacional Autónoma de México. Circuito de la Investigación S/N, Ciudad Universitaria, Coyoacán, Ciudad de México, 04510, México. alvarado@geología.unam.mx Kleyton Magno Cantalice Severiano. Departamento de Paleontología, Instituto de Geología, Universidad CABALLERO-VIÑAS ET AL.: PLIOCENE GOODEID FROM MEXICO 2 Nacional Autónoma de México. Circuito de la Investigación S/N, Ciudad Universitaria, Coyoacán, Ciudad de México, 04510, México. kleytonmc@geologia.unam.mx
根据对墨西哥伊达尔戈Sanctórum古阿马亚克湖上新世沉积物中发现的14个雌雄化石标本的骨学研究,建立了古马尼亚古裂片化石种古马尼亚古特征龙gen. and sp. 11 .。这一新棘齿鱼表现出鳖科和鳖亚科的诊断特征;与所有的好齿类一样,其前颌远端直,前颌上突小;而且,像古德尼鱼一样,这个新物种是胎生的,它的第一个肛门鳍是初级的,雄性有一个雄蕊柱体。尽管古氏古猿显示出许多原始特征,但不可能将其归入任何古迪恩部落,目前这些古迪恩部落是由骨学特征模糊定义的。这个新种似乎与characterodon有密切的亲缘关系;两者都有一种特殊的骨学特征;方椎体的关节突是一个环状结构,其中关节后形成中心区域,几个半圆形关节外突形成周围部分。本种不同于其他好蛛主要有两个特征;它有颞骨和小的前腹突,其眶上管开口显示公式12a, 2b-3a, 3b-4a, 4b-5a和5b-7。在墨西哥领土东坡的Pánuco-Salado大盆地中发现的这种已灭绝的优良物种代表了一个意想不到的历史因素。卡门Caballero-Vinas。墨西哥国立大学Autónoma Geología研究所Paleontología系。墨西哥墨西哥城,04510,墨西哥,墨西哥,墨西哥,墨西哥,墨西哥,墨西哥,墨西哥,墨西哥,墨西哥,墨西哥,墨西哥,墨西哥,墨西哥,墨西哥,墨西哥c-caballero@live.com.mx Jesús阿尔瓦拉多-奥尔特加。墨西哥国立大学Autónoma Geología研究所Paleontología系。电子线路Investigación s.s.n, Ciudad Universitaria, Coyoacán, Ciudad de msamico, 04510, msamico。alvarado@geologia.unam。克雷顿·马格诺·坎塔利斯·塞维利亚诺。Paleontología系,Geología研究所,CABALLERO-VIÑAS等:上新世古数据来自墨西哥2国家Autónoma de msamxico。电子线路Investigación s.s.n, Ciudad Universitaria, Coyoacán, Ciudad de msamico, 04510, msamico。kleytonmc@geologia.unam.mx
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引用次数: 0
Differentiating convergent pathologies in turtle shells using computed tomographic scanning of modern and fossil bone 用现代骨和化石骨的计算机断层扫描区分龟壳的会聚性病理
IF 2 4区 地球科学 Q1 Earth and Planetary Sciences Pub Date : 2023-01-01 DOI: 10.26879/1230
Stephanie K Drumheller, Hannah F. Maddox, M. Stocker, Christopher R. Noto
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引用次数: 0
A reconsideration of the palinuroid family Synaxidae (Crustacea, Decapoda), with a new member from the Upper Jurassic of southern Poland 波兰南部上侏罗统一新成员的再讨论:刺足科(甲壳纲,十足目)
IF 2 4区 地球科学 Q1 Earth and Planetary Sciences Pub Date : 2023-01-01 DOI: 10.26879/1252
René H. B. Fraaije, B. V. van Bakel, J. Jagt, M. Krobicki, À. Ossó, F. Palero, J. Wallaard
Representatives of the family Synaxidae, commonly referred to as furry lobsters, are rare constituents of modern-day marine communities, while their fossil record suggests that they were more common in the past, in reefal settings during the Late Jurassic across Europe, from where at least three species have been recorded
通常被称为“毛龙虾”的联螯虾科的代表是现代海洋生物群落中罕见的组成部分,而它们的化石记录表明,它们在过去更常见,在晚侏罗世整个欧洲的珊瑚礁环境中,至少有三个物种被记录下来
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引用次数: 0
Linking burrow morphology to the behaviors of predatory soil arthropods: Applications to continental ichnofossils 将穴居形态与掠夺性土壤节肢动物的行为联系起来:在大陆鱼化石上的应用
IF 2 4区 地球科学 Q1 Earth and Planetary Sciences Pub Date : 2023-01-01 DOI: 10.26879/1257
Daniel I. Hembree
Predatory arthropods are known from terrestrial environments since the Silurian. Many of these animals have developed morphological and behavioral adaptations for living within soil environments. Ichnofossils are common in Paleozoic paleosols, yet most are of uncertain origin and may record a hidden diversity of predatory arthropods. These ichnofossils are especially important given the relatively poor preservation potential of soil invertebrates in the environments they inhabit. To better understand the morphology and uses of predatory soil arthropod burrows, laboratory experiments were conducted with centipedes, scorpions, whip scorpions, and spiders. Specimens were placed in sediment-filled terrariums for 1 to 36 weeks. The animals were observed continuously using digital recordings to monitor their behaviors and use of their burrows. Open burrows were cast and described qualitatively and quantitatively. The animals burrowed using various techniques including intrusion, compression, excavation, and backfilling. Some burrows were occupied for short intervals (2-5 days) before being abandoned, whereas others were permanently occupied. Burrows ranged from simple vertical shafts to complex, branching networks that served as temporary to permanent dwellings, and most were used as sites for ambush predation or as prey traps. The different predatory arthropods produced unique burrows that could be linked to specific behaviors. Distinct burrow features were linked to predatory activities including vertical shafts, multiple surface openings, branching tunnel networks, and expanded chambers. These data can be applied to continental ichnofossils to improve our understanding of the evolution of terrestrial predatory arthropods, their distribution through time, and interpretations of the paleoecology of ancient soil ecosystems. Daniel I. Hembree. Department of Earth and Planetary Sciences, University of Tennessee Knoxville, Knoxville, Tennessee 37996, USA, dhemre2@utk.edu
自志留纪以来,食肉节肢动物在陆地环境中就已为人所知。这些动物中的许多已经发展出适应土壤环境的形态和行为。鱼化石在古生代古土壤中很常见,但大多数起源不确定,可能记录了食肉节肢动物的隐藏多样性。考虑到土壤无脊椎动物在它们栖息的环境中相对较差的保存潜力,这些鱼化石尤为重要。为了更好地了解掠食性土壤节肢动物洞穴的形态和用途,对蜈蚣、蝎子、鞭蝎和蜘蛛进行了室内实验。标本放置在充满沉积物的水族箱中1至36周。研究人员通过数字记录对这些动物进行持续观察,以监控它们的行为和对洞穴的使用。对开放的洞穴进行浇铸,并进行定性和定量描述。这些动物使用各种技术挖洞,包括侵入、压缩、挖掘和回填。有些洞穴在被遗弃之前会被占用很短的时间(2-5天),而其他洞穴则会被永久占用。洞穴从简单的竖井到复杂的分支网络,作为临时或永久的住所,大多数被用作伏击捕食或猎物陷阱的场所。不同的掠食性节肢动物产生了独特的洞穴,这些洞穴可能与特定的行为有关。不同的洞穴特征与捕食活动有关,包括垂直竖井,多个表面开口,分支隧道网络和扩展的腔室。这些数据可以应用于大陆鱼化石,以提高我们对陆生掠食性节肢动物的进化、它们的时间分布和古代土壤生态系统古生态学的理解。丹尼尔·亨布里。田纳西大学诺克斯维尔分校地球与行星科学系,美国田纳西州诺克斯维尔37996,dhemre2@utk.edu
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引用次数: 0
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Palaeontologia Electronica
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