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First tetrapod swim traces and associated ichnofauna from the Mesozoic of Algeria, North Africa 北非阿尔及利亚中生代最早的四足动物游泳痕迹和相关的鱼动物群
Pub Date : 2023-09-19 DOI: 10.1080/10420940.2023.2258261
Imad Bouchemla, Madani Benyoucef, Hendrik Klein, Mohammed Adaci
AbstractWe report tetrapod traces and associated ichnofauna from two stratigraphic, dominantly terrestrial levels of the Tiout Formation (Valanginian-latest Albian to lower Cenomanian) in Laghouat and Brezina areas, Central Saharan Atlas (Djebel Amour), northwestern Algeria and discuss their paleoecological implications. The assemblages display abundant footprints that show similarities with crocodylian swim traces assigned to Hatcherichnus known from Jurassic–Cretaceous deposits of North America and Morocco. However, there is also some similarity in shape with traces attributed to swimming pterosaurs by different authors. Because of the isolated materials from Algeria and the lack of distinct trackways, we leave the decision on the tracemaker open. The majority of the traces are tridactyl to tetradactyl imprints consisting of parallel furrows left by the claws of swimming or buoyant individuals. Tetrapod swim traces are identified, described, and figured herein for the first time from the Mesozoic of Algeria. These vertebrate fossil traces are associated with a low-diversity invertebrate marine ichnofauna, including cf. Bergaueria isp., Phycodes isp., Sinusichnus cf. seilacheri, and Thalassinoides suevicus. Together with body fossil data, including abundant fishes and non-avian dinosaurs, they indicate a diverse animal community populating a fluvial system environment with marine influence. Paleoecological and paleoenvironmental features of the Tiout Formation add new information to the ichnoassemblages previously reported from the ‘mid’-Cretaceous of North Africa.Keywords: Swim tracesinvertebrate ichnofaunacontinental intercalarypaleoecologySaharan AtlasAlgeria AcknowledgementsWe are grateful to the reviewers Martin Lockley and Adrian Hunt for their valuable comments and constructive suggestions that helped improve a preliminary version of the typescript.Disclosure statementNo potential conflict of interest was reported by the authors.Additional informationFundingThis work was supported by the General Directorate of Scientific Research and Technological Development ‘DGRSDT’ (Algeria).
摘要本文报道了阿尔及利亚西北部撒哈拉沙漠中部地区Laghouat和Brezina地区Tiout组(valangian -late Albian - lower Cenomanian)两个地层的四足动物痕迹和相关的鱼区系,并讨论了它们的古生态学意义。这些组合显示了大量的足迹,与北美和摩洛哥侏罗纪-白垩纪沉积物中已知的Hatcherichnus的鳄鱼游泳痕迹相似。然而,不同的作者认为游动翼龙在形状上也有一些相似之处。由于来自阿尔及利亚的孤立材料和缺乏明确的轨道,我们对跟踪器的决定保留开放。大多数痕迹是由游泳或浮力个体的爪子留下的平行沟组成的三足或四足印记。本文首次从阿尔及利亚中生代鉴定、描述和描绘了四足动物的游动痕迹。这些脊椎动物化石痕迹与低多样性的无脊椎海洋鱼动物群有关,包括cf. Bergaueria isp。, Phycodes isp。、seilacheri Sinusichnus和suevicus。连同包括大量鱼类和非鸟类恐龙在内的身体化石数据,它们表明在受海洋影响的河流系统环境中存在着多样化的动物群落。Tiout组的古生态和古环境特征为先前报道的北非“中”白垩纪的鱼类组合提供了新的信息。关键词:游泳痕迹无脊椎动物区系陆生跨壳生态生态学撒哈拉阿特拉斯阿尔及利亚致谢感谢审稿人Martin Lockley和Adrian Hunt提出的宝贵意见和建设性建议,帮助改进了初稿。披露声明作者未报告潜在的利益冲突。这项工作得到了阿尔及利亚科学研究和技术发展总局(DGRSDT)的支持。
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引用次数: 0
Burrow systems of modern subterranean rodents (Ctenomyidae): key neoichnologic features and recognition of fossil examples 现代地下啮齿动物(栉齿动物科)的穴居系统:关键的新学特征和化石样本的识别
Pub Date : 2023-09-19 DOI: 10.1080/10420940.2023.2258265
Maria Cristina Cardonatto, Ricardo Néstor Melchor
AbstractThis study is aimed to identify the distinctive ichnologic features of burrow systems of two ctenomyid species of extant solitary and subterranean rodents (Ctenomys azarae and C. talarum occidentalis) from La Pampa Province (Argentina). A total of 12 active burrows from different biogeographic provinces were cast with polyurethane foam, then excavated and the entire system was mapped. Ctenomyid burrow systems are shallow (average depth 0.30 m), branched, and subhorizontal with several plugged entrances, having a main tunnel and secondary ones arranged in a single level. Curved length, tortuosity, fractal dimension branching angles, and the scarcity or absence of chambers are similar in both species. The average horizontal diameter is 66 mm, the burrow cross-section is subcircular to vertical elliptical, and entrance ramps slope at an average of 22°. Surface ornamentation in the form of sets of three curved claw traces composing a chevron pattern is dominant. Ctenomys azarae is distinguished from C. talarum occidentalis by the presence of food caches and wider sets of claw traces. Ctenomyidae burrows are easily distinguished from those of Octodontidae and Caviidae using the relative diameter index. The outlined criteria are applied to identify fossil examples of Late Miocene-Holocene ctenomyid burrows.Keywords: Semi-arid environmentrodent burrowCtenomysburrow cross-sectionsurface ornamentationclaw tracesfossil tetrapod burrow AcknowledgmentsThis research is part of the doctoral thesis in Biology by MCC at the Universidad Nacional del Comahue (San Carlos de Bariloche, Río Negro Province, Argentina). Permission to work in the Gran Salitral area was granted by the Dirección de Recursos Naturales, Government of La Pampa Province. This work was funded by project PICT2019-114 from the Agencia Nacional de Promoción Científica y Tecnológica of Argentina and project G22 from Universidad Nacional de La Pampa to RNM. We especially thank Enrique Justo and family (owners of La Florida), Hugo Cerda (owner of Puesto La Porfía), and the Cobo family (from Naicó) for allowing us to work in their land and their hospitality. Marta Kin, Fátima Mendoza Belmontes, Luciana Cobo and Nahuel Espinoza are thanked for help during fieldwork.Disclosure statementNo potential conflict of interest was reported by the author(s).Additional informationFundingThis work was supported by Agencia Nacional de Promoción Científica y Tecnológica [PICT2019-114] and Consejo Nacional de Investigaciones Científicas y Técnicas [PIP 2021-2023-146].
摘要本研究旨在鉴定阿根廷拉Pampa省现存两种独居和地下啮齿动物(Ctenomys azarae和C. talarum occidentalis)的穴居系统的独特技术特征。采用聚氨酯泡沫塑料浇筑了12个不同生物地理省份的活动洞穴,然后进行挖掘并绘制了整个系统。栉虫穴道系统较浅(平均深度0.30 m),呈分支状,呈亚水平分布,有几个堵塞的入口,主隧道和次隧道排列在同一水平层。弯曲的长度,弯曲度,分形维数分支角,和室的稀缺性或缺乏性在这两个种是相似的。平均水平直径为66 mm,坑道断面为近圆形至垂直椭圆形,入口坡道坡度平均为22°。表面纹饰以三组弯曲的爪痕组成的纹样为主。azarae与C. talarum occidentalis的区别在于存在食物贮藏和更宽的爪痕。利用相对直径指数可以很容易地将毛线蛛科的洞穴与八齿蛛科和穴蛛科的洞穴区分开来。所概述的标准被用于鉴定晚中新世-全新世栉水母洞穴的化石实例。关键词:半干旱环境啮齿动物洞穴刺齿动物洞穴横截面表面纹饰爪痕化石四足动物洞穴致谢本研究是阿根廷国立Comahue大学(San Carlos de Bariloche, Río Negro Province, Argentina) MCC生物学博士论文的一部分拉潘帕省政府Dirección de Recursos Naturales批准在大萨利特拉尔地区工作。这项工作由阿根廷国家机构Promoción Científica y Tecnológica的PICT2019-114项目和拉潘帕国立大学向RNM提供的G22项目资助。我们特别感谢Enrique Justo及其家族(La Florida的所有者)、Hugo Cerda (Puesto La Porfía的所有者)和Cobo家族(来自Naicó),感谢他们允许我们在他们的土地上工作,也感谢他们的热情好客。感谢Marta Kin, Fátima Mendoza Belmontes, Luciana Cobo和Nahuel Espinoza在实地工作中的帮助。披露声明作者未报告潜在的利益冲突。本研究得到了国家机构Promoción Científica y Tecnológica [PICT2019-114]和国家调查委员会Científicas y tacimnicas [PIP 2021-2023-146]的支持。
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引用次数: 0
New records of Ctenopholeus in the early Devonian Hunsrück Slate of Bundenbach, SW Germany 德国西南部Bundenbach早泥盆世hunsr<e:1> ck岩中栉龙的新记录
Pub Date : 2023-09-14 DOI: 10.1080/10420940.2023.2258264
Markus J. Poschmann, Dirk Knaust, Thomas Schindler
AbstractThe rare trace fossil Ctenopholeus kutscheri Seilacher & Hemleben, originally described from the type area of the early Devonian Hunsrück Slate at Gemünden (Germany), refers to initially open horizontal tunnels with vertically to obliquely oriented serial shafts opening to the sediment-water interface. Occurrences of frequent and partly exceptionally large specimens from Bundenbach, tentatively assigned here to C. kutscheri, reveal that these burrows, were constructed in larger numbers in the Hunsrück Slate. This happened when environmental conditions were favorable for the producer(s). Contributing factors presumably include substrate cohesion and stability being suitable for the maintenance of open burrow systems, as well as sustainable food resources during the time interval when the burrows were occupied. The new material confirms that the course of the shafts in C. kutscheri varies from almost straight to slightly bent to circular in cleavage plane view and may overlap with morphologies observed in Heliochone hunsrueckiana Seilacher & Hemleben. Holothurians and, more likely, crustaceans are discussed as possible producers of C. kutscheri from the Hunsrück Slate.Keywords: Early DevonianHunsrück SlateCtenopholeusfrequent occurrencecrustacea AcknowledgementsWe thank Wouter Südkamp (Hausen) for initially communicating the Herrenberg rock fall and Hermann Lintz (Niddatal) for providing photographs of a specimen from his collection. Ryusuke Kimitsuki and Murray Gingras (both Edmonton) kindly helped to improve Figure 1. We also thank the mayor of Bundenbach, Mrs. Verena Mächtel, for permission of access to the Herrenberg Mine and Christian Wild for guidance. We are very grateful to Sören Jensen (Badajoz), the anonymous reviewers, and the journal editors for comments that improved this contribution.Disclosure statementNo potential conflict of interest was reported by the authors.
摘要Ctenopholeus kutscheri Seilacher & Hemleben化石是德国gem nden早泥盆世hunsr ck板岩类型区发现的罕见化石,指的是一种具有垂直或斜向连续竖井的初开水平隧道,通向沉积物-水界面。在Bundenbach出现的频繁和部分特别大的标本,暂定为C. kutscheri,表明这些洞穴在hunsr ck板岩中建造的数量更多。当环境条件对生产者有利时,这种情况就会发生。可能的影响因素包括基质的凝聚力和稳定性,适合维持开放的洞穴系统,以及在洞穴被占用的时间间隔内可持续的食物资源。新材料证实,C. kutscheri的轴在解理面上从几乎笔直到略微弯曲到圆形不等,并且可能与heliochoone hunsrueckiana Seilacher & Hemleben观察到的形态重叠。holothurian和更有可能的甲壳类动物被认为是hunsr ck板岩中C. kutscheri的可能生产者。关键词:早泥盆世hunsr ck板岩岩虫孔频繁发生cecrustacea感谢Wouter s dkamp (Hausen)最初介绍了Herrenberg岩落,并感谢Hermann Lintz (Niddatal)提供了他收集的标本的照片。Ryusuke Kimitsuki和Murray Gingras(都来自埃德蒙顿)帮助改进了图1。我们还要感谢本登巴赫市长维伦娜夫人Mächtel,她允许我们进入赫伦堡矿,并感谢克里斯蒂安·维尔德的指导。我们非常感谢Sören Jensen (Badajoz)、匿名审稿人和期刊编辑的意见,他们的意见改进了这篇文章。披露声明作者未报告潜在的利益冲突。
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引用次数: 0
Effects of X-ray computed tomography (CT) on the ichnologic interpretation of the Mira River estuary sediment core, SW Portugal x射线计算机断层扫描(CT)对葡萄牙西南部米拉河河口沉积物岩心的技术解释的影响
Pub Date : 2023-05-30 DOI: 10.1080/10420940.2023.2212120
Alina Shchepetkina, Teresa Drago, Jacqueline Santos, Ana Alberto
AbstractComputed tomography (CT) is a relatively new technique in ichnofossil analysis, which permits superior identification of individual trace fossils, their morphology, infill, tiering relationships, and preservation potential, thus providing better environmental interpretations. It also allows non-professional ichnologists to interpret trace fossils in 3D slices with ease, especially in relatively homogeneous and mud-rich sediments. Herein, CT imagery results have been compared with conventional core logging results based on two push core samples from a muddy tidal flat of the Mira River estuary, Portugal. CT images provide a significantly more accurate description of cores and their environmental interpretation due to enhanced visibility of physical and biogenic sedimentary structures. They also reveal complex tiering relationships between burrows with preferential preservation of deeper tiers. The appearance of stacked Scalichnus-like and other siphonichnidal burrows made by infaunal bivalves indicates discontinuous deposition on a tidal flat likely caused by seasonally related fluctuations in an estuarine environment.Keywords: CT scanningtieringequilibrichniapaleoenvironmental analysisestuary AcknowledgementsThis work is devoted to Dr. George S. Pemberton, who was the leading author’s Ph.D. supervisor, mentor, and “ichnological father”. Drs. Francisco Fatela and Conceição Freitas from the University of Lisbon are thanked for their valuable help in the organization of fieldwork and obtention of the push cores.Disclosure statementNo potential conflict of interest was reported by the author(s).Additional informationFundingThe study was funded by the Portuguese Fundação para a Ciência e a Tecnologia (FCT) I.P./MCTES through national funds (PIDDAC) – UIDB/50019/2020 under the project “UIDP/50019/2020 – Financiamento Plurianual de Unidades de I&D 2020-2023 – IDL” and co-funded by European funds (POCI), Regional Operational Programmes (COMPETE) and national funds (FCT) under the project “European Multidisciplinary Seafloor and Water Column Observatory (Portugal) - EMSO-PT (PINFRA/22157/2016)” in the scope of “Portuguese Roadmap of Research Infrastructures”. Jacqueline Santos received financial support through grant IPMA-2020-011-BI (under the project EMSOPT) and Ana Alberto through PhD grant UIBD/151497/2021 (IDL).
摘要计算机断层扫描(CT)技术是一种相对较新的化石分析技术,它可以更好地识别单个化石的形态、填充、层序关系和保存潜力,从而提供更好的环境解释。它还允许非专业技术人员轻松地在3D切片中解释痕量化石,特别是在相对均匀和富含泥浆的沉积物中。本文将CT成像结果与常规岩心测井结果进行了比较,这些岩心是基于葡萄牙米拉河河口泥质潮滩的两个推式岩心样本。由于增强了物理和生物成因沉积结构的可见性,CT图像提供了更准确的岩心描述及其环境解释。它们还揭示了洞穴之间复杂的分层关系,并优先保存更深的层。由水生双壳类动物形成的类似于scalichnus和其他虹吸管状洞穴的堆积表明,在潮汐滩上的不连续沉积可能是由河口环境中与季节相关的波动引起的。本文作者是主要作者的博士导师、导师和“技术之父”George S. Pemberton博士。Drs。感谢里斯本大学的Francisco Fatela和concep o Freitas在组织实地考察和关注推核方面提供的宝贵帮助。披露声明作者未报告潜在的利益冲突。本研究由葡萄牙 技术基金会(FCT) ip /MCTES通过国家基金(PIDDAC) - UIDB/50019/2020在“UIDP/50019/2020 - 2020-2023 - IDL”项目下资助,并由欧洲基金(POCI)共同资助。在“葡萄牙研究基础设施路线图”范围内的“欧洲多学科海底和水柱观测站(葡萄牙)- EMSO-PT (PINFRA/22157/2016)”项目下的区域业务计划(COMPETE)和国家基金(FCT)。Jacqueline Santos获得了IPMA-2020-011-BI (EMSOPT项目下)的资助,Ana Alberto获得了UIBD/151497/2021 (IDL)的博士资助。
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