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New pipimorphs from the Late Cretaceous of Niger 尼日尔晚白垩纪的新皮皮怪
IF 1 4区 地球科学 Q4 PALEONTOLOGY Pub Date : 2025-04-01 DOI: 10.1016/j.annpal.2024.102751
Alfred Lemierre , Salvador Bailon , Annelise Folie , Michel Laurin
In Becetèn, in southeast Niger, is one of the few mid-Upper Cretaceous (Coniacian-Santonian) fossiliferous localities in Africa where multiple anuran taxa are known. Two of them, Pachycentrata taqueti and Inbecetenanura ragei, have been described from In Becetèn. Both are pipids, a clade composed of exclusively aquatic anurans. Beside these two pipids, numerous isolated bones have also been referred to anurans within the site, but never referred to any known less inclusive taxa. Here we describe several identified cranial and postcranial bones referable to Pipidae or its stem-group, which together constitute Pipimorpha. Among these elements, three cranial elements are referred to two unnamed pipimorphs. One of these has gondwanomorph affinities (pipids + South American and African extinct pipimorphs). These conclusions are supported by our phylogenetic analyses. Numerous postcranial elements are not referable to any of the four pipimorph taxa identified at In Becetèn, although some ilia might be tentatively referred to ?Pachycentrata sp. The presence of at least four distinct anuran taxa makes In Becetèn the most diverse anuran site in Mesozoic Africa. It is also the first site in the Mesozoic where four pipimorph taxa are identified. The dominance of pipimorphs in the anuran diversity of the site suggests that In Becetèn was likely more lacustrine than previously thought.
在尼日尔东南部的becet,是非洲为数不多的中上白垩纪(coniian - santonian)化石地区之一,那里已知多个阿努拉类群。其中的两种,Pachycentrata taqueti和Inbecetenanura ragei,已经在《In becet》中被描述过。两者都是脂类动物,这是一个完全由水生无尾目动物组成的分支。除了这两种脂类外,还有许多孤立的骨头也被认为是该遗址内的无尾目动物,但从未涉及任何已知的包容性较低的分类群。在这里,我们描述了几个已确定的颅骨和颅后骨,可参考Pipidae或其茎群,它们共同构成pipiorpha。在这些元素中,三个颅元素涉及两个未命名的皮皮。其中之一具有冈氏形态的亲缘关系(皮脂类+南美和非洲灭绝的皮脂类)。这些结论得到了系统发育分析的支持。在In becet发现的四种pipimorph类群中,有许多颅后元素与其中任何一种都不相关,尽管一些ilia可能被暂定为Pachycentrata sp.。至少四种不同的无尾猿类群的存在使In becet成为非洲中生代最多样化的无尾猿遗址。这也是在中生代首次发现四种pipimorph分类群。pipiorphs在该遗址的无性动物多样性中的优势表明,in becet可能比以前认为的更像湖泊。
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引用次数: 0
Les empreintes de dinosaures du Jurassique inférieur de Peyre (Aveyron, France) : fouille récente et nouvelles données ichnologiques révélées par imagerie 3D 佩尔(法国艾维隆)侏罗纪晚期恐龙足迹:通过3D成像揭示了最近的挖掘和新的葡萄酒学数据。
IF 1 4区 地球科学 Q4 PALEONTOLOGY Pub Date : 2025-04-01 DOI: 10.1016/j.annpal.2025.102868
Jean-David Moreau , Jacques Sciau , Ethan Jean
At the end of the 20th century, dinosaur footprints were discovered at Peyre, in Aveyron (Causses Basin, southern France). At that time, the tracksite was limited to a single fossiliferous surface bearing a dozen of Lower Jurassic footprints. Recent excavations (2022–2024), led along a 23 m thick stratigraphic section revealed six additional track-bearing surfaces. Dinosaur tracksites showing such a high density of track-bearing surfaces along such a short section are uncommon in the fossil record and extremely rare in the Causses Basin. Today, the tracksite displays 126 footprints some of which reach 49 cm in length. Tracks are preserved in situ as concave epireliefs on the surface of dolomitic beds. Some footprints are well-preserved, showing details of digit, pad and claw marks. The excavation and 3D modelling by photogrammetry revealed several morphologies of tridactyl footprints. Biometric analyses combined with photogrammetric imaging indicated the co-occurrence of three ichnotaxa: Eubrontes giganteus, Grallator variabilis and Kayentapus isp. The high density of footprints unidirectionally oriented suggests repeated passages of theropods whose migrations were restricted by local physical barriers (coastlines, topography). Tracks are preserved in dolomite with cryptalgal laminites, mud cracks and ripple marks. The depositional environment is interpreted as a tidal flat periodically flooded then emerged.
20世纪末,在法国南部阿韦隆(Aveyron)的佩尔(Peyre)发现了恐龙脚印。当时,这个足迹地点仅限于一个化石表面,上面有十几个下侏罗纪的脚印。最近的挖掘(2022-2024),沿着23米厚的地层剖面,发现了六个额外的轨道表面。在化石记录中,在这么短的一段时间内,显示出如此高密度的脚印表面的恐龙足迹遗址是罕见的,在科斯盆地更是极为罕见。今天,这个足迹站点展示了126个足迹,其中一些长达49厘米。痕迹在白云岩层表面以凹状上浮雕的形式保存下来。有些脚印保存完好,显示了手指、脚掌和爪印的细节。通过摄影测量的挖掘和三维建模揭示了三趾类足迹的几种形态。生物特征分析结合摄影测量成像结果表明,该地区共存在3个鱼类群:Eubrontes giganteus、Grallator variabilis和Kayentapus isp。高密度的单向足迹表明兽脚亚目恐龙的迁徙受到当地物理障碍(海岸线、地形)的限制。痕迹被保存在白云岩中,带有隐晶层,泥裂缝和波纹痕迹。沉积环境被解释为潮汐滩周期性地被淹没然后出现。
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引用次数: 0
The affinities of the extinct giant tortoise “Testudo” punica from the Pliocene of Tunisia with the genus Titanochelon 突尼斯上新世已灭绝的巨龟“Testudo”与泰坦龙属的亲缘关系
IF 1 4区 地球科学 Q4 PALEONTOLOGY Pub Date : 2025-04-01 DOI: 10.1016/j.annpal.2025.102754
Evangelos Vlachos
The discovery of giant tortoises around the Mediterranean has transformed our understanding of their evolutionary history, with recent findings suggesting complex lineage dispersals between Africa and Europe. Historically, Mediterranean tortoise species were considered isolated, but studies now suggest that some African lineages may have migrated to Europe, while other distinct groups inhabited Mediterranean islands. “Testudopunica from Tunisia, a giant tortoise from the early Pliocene, requires re-examination to assess its lineage accurately. This study re-evaluates its morphology within this newly complex phylogenetic context, highlighting the need for further research on circum-Mediterranean tortoise evolution.
在地中海附近发现的巨型陆龟改变了我们对它们进化史的理解,最近的发现表明,非洲和欧洲之间存在复杂的谱系分散。历史上,地中海陆龟被认为是孤立的,但现在的研究表明,一些非洲血统可能已经迁移到欧洲,而其他不同的群体则居住在地中海岛屿上。来自突尼斯的“Testudo”punica是上新世早期的一种巨型龟,需要重新检查才能准确地评估其血统。本研究在这一新的复杂系统发育背景下重新评估了其形态,强调了进一步研究环地中海陆龟进化的必要性。
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引用次数: 0
A rare occurrence of Lamellaptychus (ammonoid jaw) from the Tethyan Himalaya and updated Indian aptychus record 特提斯-喜马拉雅地区罕见的板爪龙(氨样颚)与更新的印度板爪龙记录
IF 1 4区 地球科学 Q4 PALEONTOLOGY Pub Date : 2025-04-01 DOI: 10.1016/j.annpal.2025.102756
Suraj Bhosale , Bhawanisingh G. Desai , Ketan Chaskar , Archchi Sarkar
The jaw apparatuses of ammonoids are rarely discovered in the fossil record. Here, we describe the first and sole record of the aptychus type lower jaw of ammonoid Lamellaptychus lamellosus (Parkinson, 1811) from the Tethyan Himalaya. The aptychus was collected from the Demul section, representing the succession of Upper member of the Spiti Shale Formation. It is discovered from a micaceous silty clay horizon with bivalves (Inoceramus), serpulids, gastropods, ?brachiopods, crinoid ossicles, belemnites and ammonites. The age-diagnostic ammonites, ?Streblites (Oppeliidae) and cf. Aulacosphinctes sp. (Himalayitidae), suggest a Late Tithonian (Ponti–Microcanthum zones) age for the aptychus. The para-species L. lamellosus is recorded for the first time and attributed to oppeliid, though in-situ material is required for a conclusive result. Given the latest advances in the aptychus study, the previous Indian records are re-evaluated. The results suggest that L. kachhensis (Trauth, 1938) from Kachchh Basin is a para-subspecies of L. sparsilamellosus (Gümbel, 1861) rather than a valid para-species of Lamellaptychus genus. In addition, a closer observation of placenticeratid ammonite jaws from the Cretaceous of Narmada Basin shows that bivalves were misidentified as aptychi.
菊石的颚器在化石记录中很少被发现。本文描述了在特提斯喜马拉雅地区发现的第一个也是唯一的单爪龙Lamellaptychus lamellosus (Parkinson, 1811)的颚型下颌。在Demul剖面中采集的爪龙代表了斯皮提页岩组上段的演替。它是在云母质粉质粘土层中发现的,有双壳类动物、蛇形动物、腹足类动物、腕足类动物、海百合类小骨动物、蓝柱石和菊石。由Streblites (Oppeliidae)和cf. Aulacosphinctes sp.(喜马拉雅科)这两种菊石的年龄判断,表明该爪龙的年龄为晚梯东世(Ponti-Microcanthum带)。这是首次记录到的副种,并将其归为oppeliid,但需要现场资料才能得出结论。鉴于对aptychus研究的最新进展,之前的印度记录被重新评估。结果表明,Kachchh盆地的L. kachhensis (Trauth, 1938)是L. sparsilamellosus (g mbel, 1861)的准亚种,而不是Lamellaptychus属的准种。此外,对纳尔马达盆地白垩纪placenticeratid菊石颌骨的进一步观察表明,双壳类被误认为aptychi。
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引用次数: 0
First insight on macroinvertebrates of Chebket Es Sellaoua (NE Algeria): Some significant ammonites from the lower Mantelliceras mantelli Zone (lower Cenomanian) 对Chebket Es Sellaoua(阿尔及利亚东北部)大型无脊椎动物的首次认识:来自Mantelliceras mantelli带(下Cenomanian)的一些重要菊石
IF 1 4区 地球科学 Q4 PALEONTOLOGY Pub Date : 2025-04-01 DOI: 10.1016/j.annpal.2025.102870
Abdelkader Oudni , Riadh Aouissi , Rachel Kruft Welton , El Hadi Mazouz , Nouh Rebouh , Abdelkader Khiari
The present work is the first paleontological study on the macroinvertebrates of Chebket Es Sellaoua in Northeastern Algeria, a Cenomanian formation rich in ammonites. Twelve ammonoid species belonging to 9 genera, 7 families and 1 order from the lower Cenomanian Mantelliceras mantelli Zone, are systematically described and illustrated. Among them, Phylloceras (Goretophylloceras) subalpinum (d’Orbigny), Puzosia compressa (Kossmat), and Mantelliceras picteti (Hyatt) are recorded for the first time in this location. The Mantelliceras mantelli Zone represents the first two thirds of the whole lower Cenomanian. Two subzones are reported in this Zone: the first one is marked by the abundance of Desmoceras (Desmoceras) latidorsatum (Michelin) and Ostingoceras costulatum (Pervinquière) and coincides with the Sharpeiceras schlueteri Subzone. The second one corresponds to the Mantelliceras saxbii Subzone associated with Puzosia compressa, Mantelliceras picteti and Scaphites spp. The present ammonites are well known from the western Neo-Tethys (Europe, North Africa, Middle East) and the eastern Neo-Tethys (Africa, Madagascar and India) in addition to other areas of the world.
本文首次对阿尔及利亚东北部富含菊石的Cenomanian地层Chebket Es Sellaoua的大型无脊椎动物进行了古生物学研究。本文系统地描述了下诺曼尼亚Mantelliceras mantelli带7科1目9属的12种氨类生物。其中,Phylloceras (Goretophylloceras) subalpinum (d’orbigny)、Puzosia compressa (Kossmat)和Mantelliceras picteti (Hyatt)为该地点首次记录。Mantelliceras mantelli带代表了整个下塞诺曼尼亚的前三分之二。该区有两个亚带:第一个亚带的特征是Desmoceras (Desmoceras) latidorsatum (Michelin)和Ostingoceras costulatum (pervinqui)的丰度,与Sharpeiceras schlueteri亚带重合。第2个属于Mantelliceras saxbii亚带,与Puzosia compressa、Mantelliceras picteti和Scaphites spp有关。现今的菊石主要分布在新特提斯西部(欧洲、北非、中东)和新特提斯东部(非洲、马达加斯加和印度)以及世界其他地区。
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引用次数: 0
Mise en évidence d’une formation siliceuse oligocène de type meulière dans le nord du bassin d’Aquitaine (Saint-Jean-d’Angle, Charente-Maritime, SO France) 阿基坦盆地北部(Saint-Jean-d ' Angle, Charente-Maritime,法国东南部)渐新世磨石型硅地层的证据
IF 1 4区 地球科学 Q4 PALEONTOLOGY Pub Date : 2025-01-01 DOI: 10.1016/j.annpal.2024.102753
Didier Neraudeau , Roch-Alexandre Benoit
Outcrops of fossiliferous Palaeogene deposits are identified for the first time in the northern part of the Aquitaine Basin, at Saint-Jean-d’Angle, locality of Malaigre, in the Rochefort area (Charente-Maritime). They provide silicified deposits of a millstone facies, with a fossiliferous content rich in charophyte remains (gyrogonites, stems, “roots”) and in freshwater gastropods (hydrobioids, limnaeids). A preliminary study of the charophytes allowed to observe in the more or less translucent siliceous matrix gyrononites close to the genera Lychnothamnus, Sphaerochara and Harrisichara. On the palaeogeographical and palaeoenvironmental points of view, these silicified facies give evidence of the marine regression started during the late Eocene that lead to the continentalisation of the northern Aquitaine and the regional development of lacustrine areas.
在Rochefort地区(Charente-Maritime) Malaigre地区的Saint-Jean-d 'Angle地区的Aquitaine盆地北部首次发现了古近系化石矿床的露头。它们提供了磨石相的硅化矿床,其化石含量丰富的绿藻残骸(螺纹石、茎、“根”)和淡水腹足类动物(水生类、沼生类)。初步研究允许在接近Lychnothamnus属,Sphaerochara属和Harrisichara属的半透明硅质基质回光镜岩中观察到蕨蕨。从古地理和古环境的角度来看,这些硅化相证明了晚始新世开始的海相退退,导致了阿基坦北部的大陆化和湖泊地区的区域发展。
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引用次数: 0
Systematics and taphonomy of Pliocene Gastropoda (Mollusca) from the Dahra Mountains, NW Algeria 阿尔及利亚西北部达拉山上新世腹足动物(软体动物)的系统学和分类学
IF 1 4区 地球科学 Q4 PALEONTOLOGY Pub Date : 2025-01-01 DOI: 10.1016/j.annpal.2024.102752
Madani Benyoucef , Bernard Landau
Palaeontological investigation of the Pliocene Tahria and Slama formations in the Lower Chelif Basin (NW Algeria) led us to collect significant gastropod assemblages for taxonomic and taphonomic purposes. There is presently a very complete inventory list of Pliocene gastropods from Algeria, with 16 species from the Zanclean Tahria Formation and 54 species from the Piacenzian Slama Formation, some of which are recorded for the first time from the Pliocene of the Mediterranean. The northwestern Algeria gastropods represent a shallow-water, fully marine fauna, sandy substrate, and show a typical Upper Pliocene Mediterranean assemblage. The gastropod shells show significant taphonomic alteration; most specimens are abraded and decalcified to a variable degree. Fragmentation was mainly a result of mechanical and biological processes. Bioerosion traces are uncommon, but when they are present, they are predominantly those of predatory gastropods (Oichnus simplex and Oichnus paraboloides), polychaete activity (Maeandropolydora isp.), and acrothoracican barnacle borings (Rogerella isp.). Integration of taphonomical, palaeoecological, and sedimentological characteristics of the gastropod-bearing beds suggests sedimentological concentrations originated from discontinuous processes of winnowing and bypassing sediments, most likely due to storm action in the shoreface depositional environment.
通过对阿尔及利亚下切里夫盆地上新世塔利亚和斯拉玛组的古生物学研究,我们收集到了重要的腹足类组合,用于分类和分类目的。阿尔及利亚目前有一个非常完整的上新世腹足类清单,其中有16种来自桑克利亚塔利亚组,54种来自皮亚琴支斯拉马组,其中一些是地中海上新世首次记录的。阿尔及利亚西北部腹足类为浅水、全海生动物群、砂质基底,是典型的上新世地中海组合。腹足类动物的壳在语音学上有明显的变化;大多数标本都有不同程度的磨损和脱钙。破碎主要是机械和生物过程的结果。生物侵蚀痕迹不常见,但当它们存在时,它们主要是掠食性腹足类(Oichnus simplex和Oichnus paraboloides),多毛纲(Maeandropolydora isp.)和acro胸类藤壶(Rogerella isp.)的生物侵蚀痕迹。腹足类地层的地形学、古生态学和沉积学特征综合表明,沉积物的富集源于沉积物的不连续筛选和绕过过程,最有可能是由于滨面沉积环境中的风暴作用。
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引用次数: 0
Oryctocephalus salteri biozone (Wuliuan, Miaolingian) in the Sumna Valley, Spiti, Himalaya 喜马拉雅斯皮提苏姆纳山谷的萨尔氏稻头菌生物带(苗岭五流)
IF 1 4区 地球科学 Q4 PALEONTOLOGY Pub Date : 2025-01-01 DOI: 10.1016/j.annpal.2024.102749
Garry Singla , Birendra P. Singh , Om Narain Bhargava , Ramanpreet Kaur , Vishal Verma
We precisely demarcate the Oryctocephalus salteri biozone in the Cambrian Parahio Member (Kunzam La Formation) well exposed on the southwest-facing slope above the right bank of the Sumna River, Spiti. The FAD and LAD of O. salteri are located at 46.5 m and 60.8 m respectively, indicating a 14.3 m local stratigraphic range of the taxon along the section in Sumna Valley, Spiti. The O. salteri biozone is demarcated with a precise stratigraphic range of the eponymous species. This biozone contains trilobites O. salteri, Kunmingaspis stracheyi, Poriagraulos sp., Ziboaspis hostilis, Hundwarella memor, and Xingrenaspis hoboi. Based on the presence of the key taxon Hundwarella, the O. salteri biozone of the Kunzam La Formation (Spiti) is correlated with the Tonkinella-Hundwarella bearing level in the Nutunus Formation, Kashmir region.
在斯皮提苏姆纳河右岸西南向斜坡上,对寒武系Parahio段(Kunzam La组)的orytocephalus salteri生物带进行了精确的划分。salteri的FAD和LAD分别位于46.5 m和60.8 m,表明该分类群在Spiti Sumna Valley剖面上的局部地层范围为14.3 m。用同名物种的精确地层范围划分了O. salteri生物带。该生物带主要有三叶虫O. salteri、Kunmingaspis stracheyi、Poriagraulos sp.、Ziboaspis hostiis、hundwarela memoror和Xingrenaspis hoboi。基于关键分类群hundwarela的存在,将Kunzam La组(Spiti) O. salteri生物带与Nutunus组tonkinella - hundwarela的含盐水平进行了对比。
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引用次数: 0
Brachiopod biodiversity and characteristics from the Campanian Stratotype region (Les Charentes and Dordogne, France) 坎帕尼亚层型地区(Les Charentes和Dordogne)腕足类生物多样性及其特征
IF 1 4区 地球科学 Q4 PALEONTOLOGY Pub Date : 2025-01-01 DOI: 10.1016/j.annpal.2024.102750
Danièle Gaspard, Florent Goussard
With the purpose to reveal the Campanian heritage in the stratotype region, we took the opportunity to highlight, among the diverse fauna, the brachiopods: benthic marine invertebrates reported since the 19th century but never really detailed till now. The phylum Brachiopoda, present since the Cambrian, decreased in number of orders after the Permian-Triassic crisis with a replacement of taxa and another crisis after the Jurassic, but representatives are still present during the Cretaceous, even the Campanian till now. The limits of this stage were explicit since the mid 19th century for the basal part with the first occurrence of Rhynchonella globata, and the reports of several authors during the 20th century for the upper boundary. Noteworthy species (one Craniiformea and nearly twenty Rhynchonelliformea) are studied and positioned in a context with lithostratigraphic units, biozones, and six formations (Fm) named after different drillings. Using tomography to reveal the brachidium of some species was highly helpful. The environments in which lived the brachiopod species, from the lower to the upper Campanian, are evoked.
为了揭示层型地区的坎帕尼亚遗产,我们借此机会在各种动物中强调了腕足类动物:自19世纪以来报道的底栖海洋无脊椎动物,但直到现在才真正详细介绍。自寒武纪以来就存在的腕足动物门,在二叠纪-三叠纪危机之后出现了分类群的更替和侏罗纪之后的另一次危机之后,目数有所减少,但在白垩纪,甚至坎帕尼亚纪至今仍有代表存在。这一阶段的界限从19世纪中期开始就明确了,在基岩部分首次发现了球形红球藻,在20世纪有几位作者报道了其上界。值得注意的物种(1个颅形目和近20个rhynchonelliforma)在岩石地层单元、生物带和6个以不同钻探命名的地层(Fm)的背景下进行了研究和定位。使用断层扫描来显示某些物种的臂部是非常有帮助的。从下坎帕尼亚到上坎帕尼亚,这些腕足动物生活的环境被唤起。
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引用次数: 0
An articulated skeleton of the neoselachian shark Palaeocarcharias from the Late Jurassic Canjuers Lagerstätte (southeastern France) 来自晚侏罗世Canjuers Lagerstätte(法国东南部)的新塞拉基亚鲨鱼古carcharias的关节骨架
IF 1 4区 地球科学 Q4 PALEONTOLOGY Pub Date : 2025-01-01 DOI: 10.1016/j.annpal.2024.102738
Guillaume Guinot , Romain Vullo , Karin Peyer , Vincent Reneleau
We report and describe the only articulated shark specimen collected from the Tithonian Canjuers Lagerstätte (Var, southeastern France). This specimen displays several anatomical and morphological features that support its attribution to the monotypic genus Palaeocarcharias. The specimen is furthermore confidently assigned to the species P. stromeri, whose articulated skeletal remains have been reported from coeval deposits in the Eichstätt area (Bavaria, southern Germany). The systematic position of this genus has been debated since its first description and remains controversial with recent works placing it as a basal lamniform or sister to the Lamniformes-Carcharhiniformes clade. The nearly complete specimen from Canjuers provides new anatomical information that complements previous descriptions based on the German material. Taken together, the morpho-anatomical features observed in Palaeocarcharias indicate that this genus is related to woobegong sharks (Orectolobiformes: Orectolobidae).
我们报告并描述了唯一从Tithonian Canjuers收集的关节鲨鱼标本Lagerstätte (Var,法国东南部)。该标本显示了一些解剖学和形态学特征,支持其归属于单型属古carcharias。该标本进一步被确定为P. stromeri物种,其关节骨骼遗骸已在Eichstätt地区(德国南部巴伐利亚)的同时期沉积物中报告。该属的系统位置自首次描述以来一直存在争议,最近的研究将其定位为基板形或板形- carcharhiniformes分支的姐妹。来自Canjuers的几乎完整的标本提供了新的解剖学信息,补充了先前基于德国材料的描述。综上所述,在古carcharias中观察到的形态解剖学特征表明,该属与海獭鲨(海獭目:海獭科)有亲缘关系。
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引用次数: 0
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Annales de Paleontologie
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