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A report on palaeontological excavations and sampling in mudrocks: some guidelines 关于在泥岩中进行古生物挖掘和取样的报告:一些指导原则
IF 3 2区 地球科学 Q1 PALEONTOLOGY Pub Date : 2024-02-15 DOI: 10.1186/s13358-024-00305-w
Walter Etter
More than 60% of the world’s sedimentary rocks are mudrocks (Potter et al., 1980; Schieber, 1998; Potter, 2003; the term mudrock is favored here over mudstone because the latter term was used to characterize a limestone texture; Dunham, 1962). From a palaeontological perspective these are, compared to sandstones and limestones, heavily undersampled. The main reason for this is that mudrocks decay in surface exposures to small chips, which develop with sun/heat and rain into an awkward pulp. The decay of the mudstone concomitantly destroys all macrofossils which are not durable. This comprises fossils with an aragonitic or delicate calcitic shell unless they are preserved as pyritic or internal calcitic molds or preserved within calcareous concretions. Therefore, most of the fossils are not recorded in surface exposures. In addition, sedimentologic investigations of mudrocks are hampered because (i) compaction makes sedimentary structures hardly recognizableand (ii) good thin sections of mudrocks are exceedingly difficult to manufacture. For micropalaeontological investigations, mudrocks rich in organic material are especially difficult to process. Standard treatments with boiling water, sodium carbonate solution, or peroxide H2O2 generally fail to dissolve much of the sediment so that the fine fraction (and in mudrocks we usually need the 63μm-fraction) largely consists of clay particle aggregates. Yet there are methods to dissolve these aggregates. Otherwise, picking the microfossils would become extremely laborious. In this paper, some guidelines for successful palaeontological work in mudrocks are outlined. These are based on the author’s personal experience. Examples from Jurassic mudrocks of Switzerland/Europe show that such excavations can be very rewarding.
世界上 60% 以上的沉积岩都是泥岩(Potter 等人,1980 年;Schieber,1998 年;Potter,2003 年;此处使用泥岩一词而非泥岩,因为后者被用来描述石灰岩的质地;Dunham,1962 年)。从古生物学的角度来看,与砂岩和石灰岩相比,泥岩的取样严重不足。其主要原因是泥岩在地表暴露时会腐烂成小碎屑,这些碎屑在日晒/高温和雨水的作用下会形成笨拙的泥浆。泥岩的腐烂同时也破坏了所有不耐久的大型化石。这包括具有霰石质或精致钙质外壳的化石,除非它们被保存为黄铁矿或内部钙质模具,或保存在钙质凝块中。因此,大部分化石都没有记录在地表出露的化石中。此外,泥岩的沉积学研究也受到阻碍,因为 (i) 压实使沉积结构难以辨认,(ii) 制作泥岩的良好薄片极其困难。对于微古生物学研究来说,富含有机物质的泥岩尤其难以处理。用沸水、碳酸钠溶液或过氧化氢 H2O2 进行标准处理通常无法溶解大部分沉积物,因此细小部分(在泥岩中我们通常需要 63 微米部分)主要由粘土颗粒聚集而成。然而,有一些方法可以溶解这些聚集体。否则,采集微化石将变得非常费力。本文概述了在泥岩中成功开展古生物工作的一些指导原则。这些都是基于作者的个人经验。瑞士/欧洲侏罗纪泥岩中的实例表明,这种发掘工作是非常有益的。
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引用次数: 0
Simoniteuthis, a new vampyromorph coleoid with prey in its arms from the Early Jurassic of Luxembourg Simoniteuthis,一种来自卢森堡早侏罗世、怀抱猎物的新的吸血鞘类动物
IF 3 2区 地球科学 Q1 PALEONTOLOGY Pub Date : 2024-02-14 DOI: 10.1186/s13358-024-00303-y
Dirk Fuchs, Robert Weis, Ben Thuy
The evolutionary history of the cephalopod order Vampyromorpha with its only recent representative, Vampyroteuthis infernalis, the deep-sea vampire squid, is still obscure and a new specimen from the Early Jurassic of Luxembourg, provides new information on the vampyromorph morphology at this period. The new taxon Simoniteuthis michaelyi. gen. n. sp., which is based on a nearly complete gladius with associated head–arm complex, is morphologically intermediate between the families Loligosepiidae and Geopeltidae. Interestingly, the arm crown displays only four arm pairs, although an arm configuration consisting of five arm pairs should be expected in vampyromorph stem lineage representatives. This observation encouraged us to critically review the presumed homology of the filaments of Vampyroteuthis and the lost arm pair in cirrate and incirrate octopods. Moreover, two bony fishes in the mouth region implicated that Simoniteuthis michaelyi n. gen. n. sp. preyed upon them in hostile water depths, a taphonomic phenomenon called distraction sinking. By contrast to modern Vampyroteuthis infernalis, Simoniteuthis michaelyi n. gen. n. sp. roamed and hunted in shallower waters as typical for Mesozoic stem lineage vampyromorphs. According to the current fossil record, a vertical migration into deeper waters (probably associated with a shift in feeding behaviour) occurred at least since the Oligocene.
头足纲吸血鱿目(Vampyromorpha)及其唯一的近代代表--深海吸血鱿(Vampyroteuthis infernalis)的进化史仍然模糊不清,来自卢森堡早侏罗世的一个新标本为这一时期的吸血鱿形态提供了新的信息。新分类群 Simoniteuthis michaelyi.有趣的是,臂冠只显示了四对臂,而吸虫茎系代表的臂构型应该是由五对臂组成的。这一观察结果促使我们重新审视了吸血鬼鱼的细丝与圈足类和无脊八足类中失去的一对臂的假定同源性。此外,口腔区域的两条骨鱼表明,Simoniteuthis michaelyi n. gen. n. sp.与现代的无间棘螈相比,Simoniteuthis michaelyi n. gen. n. sp.在较浅的水域中游荡和捕食,是中生代茎系吸血侏儒螈的典型特征。根据目前的化石记录,至少从渐新世开始,就出现了向深水区的垂直迁移(可能与捕食行为的转变有关)。
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引用次数: 0
Pachycormid fish fed on octobrachian cephalopods: new evidence from the ‘Schistes bitumineux’ (early Toarcian) of southern Luxembourg 以八腕头足类为食的棘尾鱼:来自卢森堡南部 "Schistes bitumineux"(早期托尔克世)的新证据
IF 3 2区 地球科学 Q1 PALEONTOLOGY Pub Date : 2024-02-09 DOI: 10.1186/s13358-023-00295-1
Robert Weis, Dominique Delsate, Christian Klug, Thodoris Argyriou, Dirk Fuchs
A re-examination of the early Toarcian fish fossils preserved in public paleontological collections in Luxembourg revealed 70 specimens of large Toarcian pachycormid fish with an excellent three-dimensional preservation within calcareous nodules. Six of them are associated with octobrachian coleoid gladii in their oesophagus or stomach, an association not previously described from Luxembourg. The pachycormids are ascribed to Pachycormus macropterus (Blainville, 1818) and Saurostomus esocinus Agassiz, 1843 while the octobrachian gladii are ascribed to Teudopsis bollensis Voltz, 1836, Teudopsis sp. indet. and Loligosepiidae indet. The position and orientation of the gladii provide direct evidence of these fishes feeding on coleoids and thus a teuthophagous diet, rather than an accidental joint burial. Together with evidence from coeval deposits in Germany, these findings suggest that teuthophagy was a widespread feeding strategy at the base of the clade that contains the suspension-feeding pachycormid giants of the Jurassic–Cretaceous.
对保存在卢森堡公共古生物藏品中的早期托阿克鱼化石进行的重新研究发现,有70件大型托阿克鱼类标本在钙质结核中三维保存完好。其中六件标本的食道或胃部与八腕类的鞘状角鲨有关联,这种关联以前从未在卢森堡描述过。棘皮动物被归类为 Pachycormus macropterus(Blainville,1818 年)和 Saurostomus esocinus Agassiz,1843 年,而八瓣膜角闪虫被归类为 Teudopsis bollensis Voltz,1836 年、Teudopsis sp.indet.和 Loligosepiidae indet.。角闪石的位置和方向提供了直接证据,证明这些鱼类以褐藻为食,因此是以褐藻为食,而不是偶然的合葬。这些发现与来自德国同时期沉积物的证据一起表明,在包含侏罗纪-白垩纪悬浮取食的棘皮动物巨类的支系底部,teuthophagy是一种普遍的取食策略。
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引用次数: 0
Callovian corals from the Swiss Jura 瑞士汝拉山脉的胼胝珊瑚
IF 3 2区 地球科学 Q1 PALEONTOLOGY Pub Date : 2024-01-25 DOI: 10.1186/s13358-023-00298-y
Hannes Löser, Andreas Wetzel, Bernhard Hostettler
Twelve solitary and platy, colonial coral taxa assigned to the families Microsolenidae, Misistellidae, Montlivaltiidae, Rayasmiliidae, and Thamnasteriidae are described and illustrated from the Callovian (Ifenthal Formation, Herznach Member) of the area of Andil near Liesberg, about 20 km WSW of the town of Basel, Switzerland. The platy growth forms and the presence of five species of the superfamily Cyclolitoidea suggests that these corals lived under low-level light conditions.
本研究描述并展示了瑞士巴塞尔镇西偏西约 20 公里处利斯堡附近安迪尔地区的 Callovian(Ifenthal Formation,Herznach 成员)中的 12 个单生和板状、群生珊瑚类群,这些类群分别属于 Microsolenidae、Misistellidae、Montlivaltiidae、Rayasmiliidae 和 Thamnasteriidae 科。板状的生长形态和 Cyclolitoidea 超科五个物种的存在表明,这些珊瑚生活在低光照条件下。
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引用次数: 0
Updated cranial and mandibular description of the Late Cretaceous (Maastrichtian) baenid turtle Saxochelys gilberti based on micro-computed tomography scans and new information on the holotype-shell association 基于微型计算机断层扫描和关于主模式与贝壳关联的新信息,更新晚白垩世(马斯特里赫特)贝类海龟 Saxochelys gilberti 的头骨和下颌骨描述
IF 3 2区 地球科学 Q1 PALEONTOLOGY Pub Date : 2024-01-23 DOI: 10.1186/s13358-023-00301-6
Gaël E. Spicher, Tyler R. Lyson, Serjoscha W. Evers
Saxochelys gilberti is a baenid turtle from the Late Cretaceous Hell Creek Formation of the United States of America known from cranial, shell, and other postcranial material. Baenid turtles are taxonomically diverse and common fossil elements within Late Cretaceous through Eocene faunas. Detailed anatomical knowledge is critical to understanding the systematics and morphological evolution of the group. This is particularly important as baenids represent an important group of continental vertebrates that survived the mass extinction event associated with the Cretaceous/Paleogene boundary. High-resolution micro-computed tomography scanning of the holotype skull reveals additional anatomical details for the already well-known Saxochelys gilberti. This includes the revision of some anatomical statements from the original description, but also detailed knowledge on internal anatomical features of the braincase and the description of a well-preserved axis (cervical vertebra 2). Our new detailed description and previous work on the shell and postcrania make Saxochelys one of the best-described, nearly complete baenid turtles, which are often only known from either isolated shell or cranial material. A revised phylogenetic analysis confirms the position of Saxochelys gilberti as a derived baenid (Eubaeninae) more closely related to Baena arenosa than to Eubaena cephalica.
Saxochelys gilberti 是一种产自美国晚白垩世地狱溪地层的海龟,根据颅骨、贝壳和其他颅后材料可知。在晚白垩世至始新世的动物群中,鳖类在分类上多种多样,是常见的化石元素。详细的解剖学知识对于了解该类群的系统学和形态演变至关重要。这一点尤为重要,因为白垩纪/古近纪边界大灭绝事件中幸存下来的一个重要大陆脊椎动物类群就是蟒蛇类。对主模式头骨的高分辨率微型计算机断层扫描揭示了已经广为人知的 Saxochelys gilberti 的更多解剖细节。这包括对原始描述中的一些解剖说明的修订,以及对脑壳内部解剖特征的详细了解和对一个保存完好的轴的描述(颈椎2)。我们新的详细描述以及之前在壳和颅后的研究工作使萨克索氏龟成为描述最完整、几乎完整的巴氏龟类之一,而这些龟类通常只能从孤立的壳或颅骨材料中获知。经过修订的系统发育分析确认了 Saxochelys gilberti 的位置,它是一种衍生的海龟类(Eubaeninae),与 Baena arenosa 的亲缘关系比与 Eubaena cephalica 的亲缘关系更近。
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引用次数: 0
A new pachypleurosaur (Reptilia: Sauropterygia) from the Middle Triassic of southwestern China and its phylogenetic and biogeographic implications 中国西南中三叠世的一种新的棘皮龙(爬行动物门:Sauropterygia)及其系统发育和生物地理学意义
IF 3 2区 地球科学 Q1 PALEONTOLOGY Pub Date : 2024-01-05 DOI: 10.1186/s13358-023-00292-4
Yi-Wei Hu, Qiang Li, Jun Liu
After the devastating Permo-Triassic Mass Extinction, several new groups of large reptilian predators invaded the sea in the early part of the Triassic. Among these predators, sauropterygians, consisting of placodonts, pachypleurosaurs, nothosaurs and pistosaurs (including the iconic plesiosaurs), displayed the greatest diversity at both the generic and species levels, and persisted from the Early Triassic to the Late Cretaceous. Here, we report a new species of Pachypleurosauria, Dianmeisaurus mutaensis sp. nov., from a recently discovered Lagerstätte in the Upper Member of the Anisian Guanling Formation. The only known specimen of the new species was collected from a quarry near Muta village, Luxi County, Yunnan Province, South China. Our new phylogenetic analysis based on a novel data matrix recovered the new taxon as a sister group to Dianmeisaurus gracilis—a small pachypleurosaur from the Middle Triassic Luoping biota. The new phylogenetic analysis also collapsed the monophyly of the traditionally recognized Eusauropterygia. Pistosauroidea, Majiashanosaurus, and Hanosaurus comprise the consecutive sister groups to a new clade including Pachypleurosauria and Nothosauroidea. A monophyletic Pachypleurosauria, within which the clade consisting of Dianmeisaurus and Panzhousaurus occupies the basal-most position, is recovered by this study. The clade consisting of Dawazisaurus and Dianopachysaurus forms the sister group to the remaining pachypleurosaurs included in this study. Since Dianmeisaurus, Panzhousaurus, Dawazisaurus, and Dianopachysaurus are all exclusively known from South China, our study provides further evidence to the hypothesis that pachypleurosaurs had a palaeobiogeographic origin in the eastern Tethys.
在毁灭性的二叠纪-三叠纪大灭绝之后,一些新的大型爬行动物掠食者群体在三叠纪早期入侵海洋。在这些食肉动物中,由胎龙类、厚背龙类、矛龙类和活龙类(包括标志性的矛龙类)组成的长颈龙类在属和种的层次上都表现出了最大的多样性,并从早三叠世一直延续到晚白垩世。在此,我们报告了一个新的厚鼻龙类物种--Dianmeisaurus mutaensis sp.该新种的唯一已知标本采集于中国南方云南省泸西县木塔村附近的采石场。我们基于一个新的数据矩阵进行了新的系统发生分析,发现该新类群与中三叠世罗平生物群中的小型棘皮龙 Dianmeisaurus gracilis 是姊妹群。新的系统发育分析还打破了传统意义上的Eusauropterygia的单系性。腕龙属(Pistosauroidea)、马家山龙属(Majiashanosaurus)和汉龙属(Hanosaurus)连续成为包括厚鼻龙属(Pachypleurosauria)和腕龙属(Nothosauroidea)在内的新支系的姐妹群。本研究发现了一个单系的厚鼻龙类,其中由滇缅龙和盘喙龙组成的支系处于最基干的位置。由滇缅龙和盘龙组成的支系是本研究中其余厚鼻龙的姊妹群。由于滇缅龙、盘瓠龙、道崎龙和滇鹟龙都是华南地区的唯一已知龙类,我们的研究为厚背龙的古地理起源于特提斯东部的假说提供了进一步的证据。
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引用次数: 0
Swiss ichthyosaurs: a review. 瑞士鱼龙:综述。
IF 3 2区 地球科学 Q1 PALEONTOLOGY Pub Date : 2024-01-01 Epub Date: 2024-09-01 DOI: 10.1186/s13358-024-00327-4
Christian Klug, Timur Sivgin, Feiko Miedema, Beat Scheffold, Achim G Reisdorf, Iwan Stössel, Erin E Maxwell, Torsten M Scheyer

Switzerland is an ichthyosaur country: it has a rich record of marine reptile fossils, particularly the fish-shaped ichthyosaurs, and the according research. Here, we provide an overview over the 12 or more genera and at least 13 species plus numerous fragmentary remains of ichthyosaurs from the Triassic to the Cretaceous that have been discovered in twelve cantons thus far, of which four species are based on Swiss holotypes. This wealth of ichthyosaur species can be explained by their abundance in the Middle Triassic conservation deposits (Konservat Lagerstätte) of Monte San Giorgio, as well as occasional discoveries in strata of Middle Triassic to Early Cretaceous age. The moderate abundance of outcrops in reasonable conditions in combination with the long history of palaeontological research in Switzerland explains this good fossil record. In addition to this unique overview, we provide more data for further studies and update the knowledge of these taxa.

瑞士是一个鱼龙之国:它拥有丰富的海洋爬行动物化石记录,尤其是鱼形鱼龙化石,并进行了相应的研究。在此,我们概述了迄今为止在瑞士12个州发现的三叠纪至白垩纪鱼龙的12属或更多属,至少13种,以及大量的鱼龙残骸,其中4种鱼龙的原型来自瑞士。圣乔治山中三叠世保护矿床(Konservat Lagerstätte)中鱼龙种类丰富,在中三叠世至早白垩世的地层中偶尔也有发现。适度丰富的露头地质条件,加上瑞士悠久的古生物学研究历史,造就了这一良好的化石记录。除了这一独特的概述之外,我们还为进一步研究提供了更多数据,并更新了对这些类群的认识。
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引用次数: 0
Complex dental wear analysis reveals dietary shift in Triassic placodonts (Sauropsida, Sauropterygia). 复杂的牙齿磨损分析揭示了三叠纪胎龙类(Sauropsida, Sauropterygia)的饮食转变。
IF 3 2区 地球科学 Q1 PALEONTOLOGY Pub Date : 2024-01-01 Epub Date: 2024-02-05 DOI: 10.1186/s13358-024-00304-x
Kinga Gere, András Lajos Nagy, Torsten M Scheyer, Ingmar Werneburg, Attila Ősi

Placodonts were durophagous reptiles of the Triassic seas with robust skulls, jaws, and enlarged, flat, pebble-like teeth. During their evolution, they underwent gradual craniodental changes from the Early Anisian to the Rhaetian, such as a reduction in the number of teeth, an increase in the size of the posterior palatal teeth, an elongation of the premaxilla/rostrum, and a widening of the temporal region. These changes are presumably related to changes in dietary habits, which, we hypothesise, are due to changes in the type and quality of food they consumed. In the present study, the dental wear pattern of a total of nine European Middle to Late Triassic placodont species were investigated using 2D and 3D microwear analyses to demonstrate whether there could have been a dietary shift or grouping among the different species and, whether the possible changes could be correlated with environmental changes affecting their habitats. The 3D analysis shows overlap between species with high variance between values and there is no distinct separation. The 2D analysis has distinguished two main groups. The first is characterised by low number of wear features and high percentage of large pits. The other group have a high feature number, but low percentage of small pits. The 2D analysis showed a correlation between the wear data and the size of the enlarged posterior crushing teeth. Teeth with larger sizes showed less wear feature (with higher pit ratio) but larger individual features. In contrast, the dental wear facet of smaller crushing teeth shows more but smaller wear features (with higher scratch number). This observation may be related to the size of the food consumed, i.e., the wider the crown, the larger food it could crush, producing larger features. Comparison with marine mammals suggests that the dietary preference of Placochelys, Psephoderma and Paraplacodus was not exclusively hard, thick-shelled food. They may have had a more mixed diet, similar to that of modern sea otters. The diet of Henodus may have included plant food, similar to the modern herbivore marine mammals and lizards.

Supplementary information: The online version contains supplementary material available at 10.1186/s13358-024-00304-x.

板齿龙是三叠纪海域的多食性爬行动物,具有坚固的头骨和颌骨,以及增大、扁平、鹅卵石状的牙齿。在进化过程中,它们经历了从早安尼期到雷特期的颅齿变化,如牙齿数量减少、后腭齿增大、前颌骨/喙延长以及颞部增宽。我们推测,这些变化可能与饮食习惯的改变有关,而饮食习惯的改变是由于他们食用的食物种类和质量发生了变化。本研究利用二维和三维显微磨损分析,研究了欧洲中三叠世至晚三叠世9个胎生类物种的牙齿磨损模式,以证明不同物种之间是否存在饮食习惯的转变或分组,以及这些可能的变化是否与影响其栖息地的环境变化有关。三维分析表明,不同物种之间存在重叠,不同数值之间的差异很大,没有明显的区分。二维分析将物种分为两大类。第一组的特征是磨损特征数量少,大坑比例高。另一组特征数量多,但小凹坑比例低。二维分析表明,磨损数据与增大的后压碎齿的大小之间存在相关性。尺寸较大的牙齿磨损特征较少(凹坑比例较高),但单个特征较大。相反,较小破碎齿的牙齿磨损面显示出较多但较小的磨损特征(划痕数较多)。这一观察结果可能与食物的大小有关,即牙冠越宽,可破碎的食物越大,产生的特征也越大。与海洋哺乳动物的比较表明,Placochelys、Psephoderma 和 Paraplacodus 的食物偏好并不完全是坚硬的厚壳食物。它们的食物可能更杂,类似于现代海獭的食物。Henodus的食物可能包括植物性食物,类似于现代食草动物海洋哺乳动物和蜥蜴:在线版本包含补充材料,可查阅 10.1186/s13358-024-00304-x。
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引用次数: 0
Thalattosauria in time and space: a review of thalattosaur spatiotemporal occurrences, presumed evolutionary relationships and current ecological hypotheses. 时间和空间中的雷龙:雷龙时空分布、推测的进化关系和当前生态学假说综述。
IF 3 2区 地球科学 Q1 PALEONTOLOGY Pub Date : 2024-01-01 Epub Date: 2024-09-26 DOI: 10.1186/s13358-024-00333-6
Dylan Bastiaans

In the wake of the greatest mass extinction in Earth's history, the End-Permian Mass Extinction, the Triassic was a time of recovery and innovation. Aided by warm climatic conditions and favorable ecological circumstances, many reptilian clades originated and rapidly diversified during this time. This set the stage for numerous independent invasions of the marine realm by several reptilian clades, such as Ichthyosauriformes and Sauropterygia, shaping the oceanic ecosystems for the entire Mesozoic. Although comparatively less speciose, and temporally and latitudinally more restricted, another marine reptile clade, the Thalattosauriformes, stands out because of their unusual and highly disparate cranial, dental and skeletal morphology. Research on Thalattosauriformes has been hampered by a historic dearth of material, with the exception of rare material from Lagerstätten and highly fossiliferous localities, such as that from the UNESCO world heritage site of Monte San Giorgio. Consequently, their evolutionary origins and paleobiology remain poorly understood. The recent influx of new material from southwestern China and North America has renewed interest in this enigmatic group prompting the need for a detailed review of historic work and current views. The earliest representatives of the group may have been present from the late Early Triassic onwards in British Columbia. By the Ladinian the group had achieved a wide distribution across the northern hemisphere, spanning the eastern Panthalassic as well as the eastern and western Tethyan provinces. Distinct morphological and likely ecological differences exist between the two major clades of Thalattosauriformes, the Askeptosauroidea and the Thalattosauroidea, with the latter showing a higher degree of cranial and skeletal morphological disparity. In-group relationships remain poorly resolved beyond this bipartition. Overall, thalattosaurs may be closely related to other marine reptile groups such as ichthyopterygians and sauropterygians. However, their exact position within Diapsida remains elusive. Future focal points should utilize modern digital paleontological approaches to explore the many fragmentary specimens of otherwise poorly sampled localities.

在地球历史上最严重的大灭绝--二叠纪末大灭绝之后,三叠纪是一个恢复和创新的时期。在温暖的气候条件和有利的生态环境的帮助下,许多爬行动物支系在这一时期起源并迅速多样化。这为几个爬行动物支系(如鱼龙形目和长尾目)多次独立入侵海洋领域创造了条件,从而塑造了整个中生代的海洋生态系统。另一个海洋爬行动物支系--雷龙形目(Thalattosauriformes)虽然在种类上相对较少,在时间和纬度上受到的限制也更多,但由于其头盖骨、牙齿和骨骼形态的不同寻常和高度差异而脱颖而出。除了来自拉格施泰滕(Lagerstätten)和化石丰富的地方(如联合国教科文组织世界遗产圣乔治山)的稀有材料外,有关雷龙类的研究一直以来都受到材料匮乏的阻碍。因此,人们对它们的进化起源和古生物学仍然知之甚少。最近,来自中国西南部和北美的大量新材料再次引起了人们对这一神秘类群的兴趣,因此有必要对历史研究和当前观点进行详细回顾。该类群最早的代表可能出现在不列颠哥伦比亚早三叠世晚期。到了拉迪尼安时期,该类群已广泛分布于北半球,横跨泛泰西期东部以及泰西亚省东部和西部。雷龙类的两个主要支系--Askeptosauroidea和Thalattosauroidea之间存在着明显的形态差异和可能的生态差异,后者的头骨和骨骼形态差异程度更高。除了这两个类群之外,类群内部的关系仍然没有得到很好的解决。总体而言,厚背龙可能与其他海洋爬行动物类群(如鱼龙类和长龙类)关系密切。然而,它们在双翅目中的确切位置仍然难以确定。未来的研究重点应利用现代数字古生物学方法来探索取样较少的地方的许多零碎标本。
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引用次数: 0
Special Issue: 100 years of scientific excavations at UNESCO World Heritage Site Monte San Giorgio and global research on Triassic marine Lagerstätten. 特刊:联合国教科文组织世界遗产圣乔治山科学发掘 100 周年及三叠纪海洋 Lagerstätten 全球研究。
IF 3 2区 地球科学 Q1 PALEONTOLOGY Pub Date : 2024-01-01 Epub Date: 2024-10-01 DOI: 10.1186/s13358-024-00328-3
Christian Klug, Torsten M Scheyer, Nicole Klein, Jun Liu, Daniele Albisetti, Heinz Furrer, Rudolf Stockar

Only a few Swiss fossil localities are known globally and of which, the UNESCO World Heritage Site Monte San Giorgio, which extends from Switzerland into Italy, is the most important one. Following the discovery of the occurrence of articulated skeletons of marine reptiles in the local mines, large excavations were organized by Bernhard Peyer from the University of Zurich starting 1924. With this collection of articles, we commemorate the successful excavations and research, which initiated the publication of a series of monographies, mostly on the vertebrates but also on the invertebrates of this locality. Especially with the discovery of several remarkably similar Konservat-Lagerstätten in China, the discoveries from Monte San Giorgio gained global relevance. New methodologies such as computed tomography produced a wealth of new data, particularly on endocranial anatomy of several tetrapods.

全球已知的瑞士化石地点寥寥无几,其中最重要的是联合国教科文组织世界遗产圣乔治山,它从瑞士一直延伸到意大利。在当地的矿井中发现海洋爬行动物有节骨骼后,苏黎世大学的伯恩哈德-佩耶(Bernhard Peyer)从 1924 年开始组织了大规模的发掘工作。通过这组文章,我们纪念了这次成功的发掘和研究,并由此开始出版了一系列专著,其中大部分是关于该地区的脊椎动物,但也包括无脊椎动物。特别是在中国发现了几处极为相似的 Konservat-Lagerstätten 之后,圣乔治山的发现在全球范围内引起了关注。计算机断层扫描等新方法产生了大量新数据,特别是关于几种四足动物的颅内解剖学数据。
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Swiss Journal of Palaeontology
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