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Pastillus aethiopicus n. sp. (Coleoptera: Cybocephalidae), a new fossil beetle from Miocene Ethiopian amber and a taxonomic key to the species of Pastillus Endrödy-Younga 埃塞俄比亚棘足棘虫(鞘翅目:棘足棘虫科):中新世埃塞俄比亚琥珀中发现的一种新甲虫化石和棘足棘虫Endrödy-Younga的分类关键
IF 1.7 3区 地球科学 Q1 Earth and Planetary Sciences Pub Date : 2024-04-01 DOI: 10.1016/j.palwor.2023.04.004
Trevor Randall Smith , Karol Szawaryn

We describe a new species of Cybocephalidae (Coleoptera) from Ethiopian Miocene amber, Pastillus aethiopicus n. sp. This is the second beetle species discovered in that fossiliferous amber deposit. It is the fourth species described in the extant genus Pastillus Endrödy-Younga and the first fossil species discovered. Pastillus is reviewed, the species diagnosed, listed, keyed, and distribution data recorded. Additionally, checklists of fossil Cybocephalidae, and African Cybocephalidae fauna are provided.

这是埃塞俄比亚中新世琥珀中发现的第二个甲虫物种。这是现存 Pastillus Endrödy-Younga 属中描述的第四个物种,也是发现的第一个化石物种。本文对 Pastillus 进行了综述,对该物种进行了诊断、列表、键控,并记录了其分布数据。此外,还提供了鲤形目化石和非洲鲤形目动物群的清单。
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引用次数: 0
Convergent evolution of encrusting calcareous tubeworms 包壳石灰质管虫的聚合进化
IF 1.7 3区 地球科学 Q1 Earth and Planetary Sciences Pub Date : 2024-04-01 DOI: 10.1016/j.palwor.2023.04.001
Olev Vinn , Manfred Jäger , Jakub Słowiński , Michał Zatoń

In the present paper we trace the patterns of convergent evolution of encrusting calcareous polychaetes and tentaculitoids with respect to the morphology and function of their tubes. Both clades have morphologically similar tubes. Six of the eight basic morphotypes of encrusting tubeworms occur both in calcareous polychaetes and in tentaculitoids. All six encrusting tentaculitoid tubeworm morphotypes distinguished have analogues among serpulid and sabellid polychaetes. Both tentaculitoids and polychaetes with calcareous tubes have a similar plesiomorphic morphotype, which is characterized by substrate parallel, irregular growth away from the initial point of encrustation. Dominance of similarities in the order of evolution of morphotypes in the calcareous tubeworms indicates that despite genetic differences, ecological similarities (suspension feeding) and similarities in the tube material (calcareous), as well as body plan (worm-like) had a strong control over the evolution of calcareous tubeworms. The calcareous tubeworm life modes likely appeared in the order of increasing dependence on the type of substrate. In general, possible antipredatory strategies (spines, keels, cryptic and endobiotic mode of life) of calcareous tubeworms are evolutionarily old. The plesiomorphic general hard substrate encrusters are evolutionarily the most successful and have the longest stratigraphic range both in tube-dwelling polychaetes and tentaculitoids. Innovations, such as attachment of the tube by basal projections were developed in some microconchid tentaculitoids but not in calcareous polychaetes; budding tubes occur in both taxa, however, in microconchid tentaculitoids it was a brief evolutionary event, whereas in polychaetes such pseudocolonies have a long stratigraphic range. The ability to live in brackish and fresh waters by some tentaculitoids and tube-dwelling polychaetes seems not to be associated with any particular tube morphotype.

在本文中,我们追溯了包壳钙质多毛类和触手类在其管的形态和功能方面的趋同进化模式。这两个支系都有形态相似的管道。在钙质多毛类和触手纲中都出现了八种基本形态的包壳管虫,其中六种都出现在钙质多毛类和触手纲中。所有六种不同的触手管虫形态在蛇形多毛类和剑形多毛类中都有相似之处。具有钙质管的触手纲和多毛类都有类似的多形形态,其特点是基质平行、不规则地从最初的结壳点向外生长。在钙管虫的形态进化顺序中,相似性占主导地位,这表明尽管存在遗传差异,但生态相似性(悬浮取食)、管材料相似性(钙质)以及体型相似性(蠕虫状)对钙管虫的进化具有很强的控制作用。钙质管虫的生活模式可能是按照对基质类型的依赖程度依次递增的顺序出现的。总的来说,钙质管虫可能的反捕食策略(刺、龙骨、隐居和内生生活方式)在进化过程中是古老的。在管栖多毛类和触手类中,多形性的一般硬底质食茧虫在进化过程中最为成功,其地层范围也最长。一些创新,如通过基部突起附着管子,在一些微壳触手类中得到了发展,但在钙质多毛类中却没有;出芽管子在这两个类群中都有出现,但在微壳触手类中这只是一个短暂的进化过程,而在多毛类中,这种假结晶体的地层范围很长。一些触手类和管栖多毛类动物在咸水和淡水中生活的能力似乎与任何特定的管形态无关。
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引用次数: 0
A Keichousaurus-bearing regurgitalite from the Middle Triassic Xingyi Fauna, Dingxiao of Xingyi City, Guizhou, South China 贵州兴义市鼎霄中三叠世兴义动物群中的一种含有反流化石的基周龙
IF 1.7 3区 地球科学 Q1 Earth and Planetary Sciences Pub Date : 2024-04-01 DOI: 10.1016/j.palwor.2023.03.009
Xiao-Jun Ye, Zuo-Yu Sun, Ming-Tao Yao

Bromalites (coprolites, regurgitalites and consumulites) are trace fossils that preserve valuable information on their producers’ diet and feeding behaviors. Here, we report a compact skeletal mass from the Middle Triassic Xingyi Fauna of Dingxiao, Xingyi City, Guizhou Province, South China through multiple analytical methods. Using micro-CT scans, we provide 3D reconstruction of two vertebral arches, four coracoids, three ribs of three kinds, four humeri including one male and three female ones, five scapulae including two right one and three left ones of different sizes, which are inferred to be from at least three individuals of Keichousaurus hui. Bone aggregates of multiple individuals, associated with less gastric etching on bone surfaces and the absence of a phosphatic and organic matrix surrounding the bones as revealed by microstructural and chemical analysis respectively, suggest that this bone mass is a regurgitalite rather than a coprolite. The vertebrate fossils reported from the regurgitalite-bearing strata suggest that the best candidate for the potential producer of the regurgitalite are the near-shore sauropterygians Nothosaurus or Lariosaurus. The discovery of a Keichousaurus-bearing regurgitalite shed new insights on the feeding behaviors of Middle Triassic marine reptiles and the paleoecology of the Xingyi Fauna.

溴石(桡足石、反刍石和纤毛石)是一种痕量化石,保存了有关其生产者饮食和摄食行为的宝贵信息。在这里,我们通过多种分析方法报告了来自中国南方贵州省兴义市顶效中三叠世兴义动物群的一个紧凑的骨骼块。利用显微CT扫描技术,我们提供了两个椎弓、四个齿冠、三种肋骨、四个肱骨(包括一个雄性和三个雌性)、五个肩胛骨(包括两个右肩胛骨和三个不同大小的左肩胛骨)的三维重建,推断这些骨骼至少来自三个个体的基周龙(Keichousaurus hui)。多个个体的骨骼聚集在一起,骨骼表面的胃蚀刻较少,而且骨骼周围没有磷化基质和有机基质(分别由显微结构和化学分析揭示),这表明这些骨块是反刍岩而不是共生岩。据报告,含雷吉拉特岩的地层中的脊椎动物化石表明,雷吉拉特岩的潜在生产者的最佳候选者是近岸的长尾龙类--诺特龙(Nothosaurus)或拉里龙(Lariosaurus)。含有基周龙的雷公石的发现为中三叠世海洋爬行动物的摄食行为和兴义动物群的古生态学提供了新的视角。
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引用次数: 0
An Ordovician (Whiterockian) marine community from Sonora, Mexico: Paleoecology and paleobiogeographic affinity with North America and Argentina 墨西哥索诺拉的奥陶纪(白垩纪)海洋群落:古生态学以及与北美和阿根廷的古生物地理亲缘关系
IF 1.7 3区 地球科学 Q2 PALEONTOLOGY Pub Date : 2024-03-29 DOI: 10.1016/j.palwor.2024.03.007
A Lower and Middle Ordovician sequence, containing an abundant biota of cyanobacteria, bryozoans, brachiopods, gastropods, cephalopods, trilobites, and echinoderms, is exposed at Rancho Las Norias in the central part of the state of Sonora, Mexico. This sequence that consists of wackestone, packstone, and grainstone is deposited in a shallow water marine environment within the photic zone, as indicated by the presence of cyanobacteria such as Nuia sibirica. A paleoecological study was performed on one fossiliferous level S1 at the middle part of the sequence in this study, where 113 individuals of 11 taxa were analyzed, which allows to reconstruct the paleocommunity structure of this calcareous layer. The paleocommunity consists mainly of brachiopods, gastropods, and trilobites. The applied paleoecological indices (Dominance and Evenness of Simpson, Diversity of Shannon-Weaver, Diversity of Menhinick, and Total Richness of Chao) indicate a benthic marine community constituted mainly by sessile-suspension feeders, and brachiopods (Orthidiella cf. O. longwelli) are the dominant forms. A Jaccard Similarity Index was also applied, where a similarity of ∼100% was obtained between Canada and Mexico, ∼80% between the USA and Mexico, and ∼50% between Argentina and Mexico, thus confirming the Ordovician paleogeographic affinity of these localities with Laurentia. The Ordovician of northwestern Mexico corresponds to the southernmost deposits of the North American craton and is an essential link in understanding the relationship between North and South America.
在墨西哥索诺拉州中部的 Rancho Las Norias,出露了一个中下奥陶统的岩层,其中含有丰富的生物群,包括蓝藻、双壳类、腕足类、腹足类、头足类、三叶虫和棘皮动物。该地层由瓦克石、包石和纹理石组成,沉积于光照区内的浅水海洋环境中,蓝藻(如 Nuia sibirica)的存在表明了这一点。本研究对该层序中段的一个化石层 S1 进行了古生态学研究,分析了 11 个类群的 113 个个体,从而重建了该钙质层的古群落结构。古群落主要由腕足动物、腹足类和三叶虫组成。应用的古生态指数(辛普森指数的优势度和均匀度、香农-韦弗指数的多样性、门希尼克指数的多样性和赵氏指数的总丰富度)表明,底栖海洋群落主要由无柄悬浮取食动物构成,腕足动物(Orthidiella cf. O. longwelli)是主要形式。此外,还应用了 Jaccard 相似性指数,加拿大与墨西哥之间的相似性为 100%,美国与墨西哥之间的相似性为 80%,阿根廷与墨西哥之间的相似性为 50%,从而证实了这些地方与劳伦西亚的奥陶纪古地理亲缘关系。墨西哥西北部的奥陶纪相当于北美克拉通最南端的沉积,是了解南北美洲关系的重要环节。
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引用次数: 0
Brachiopods from the Serpukhovian Tonka Formation of Carlin Canyon, Elko, Nevada (USA): Systematics and biostratigraphy 来自美国内华达州埃尔科卡林峡谷塞普霍维亚通卡地层的腕足类:系统学和生物地层学
IF 1.7 3区 地球科学 Q2 PALEONTOLOGY Pub Date : 2024-03-26 DOI: 10.1016/j.palwor.2024.03.006
Systematic study of a brachiopod assemblage from the Upper Mississippian Tonka Formation in Carlin Canyon, Elko, Nevada, USA, led to the recognition of 13 species, representing 12 genera and seven orders: ?Antiquatonia sp., Flexaria sp., ?Marginatia sp., Echinoconchus sp. of the Productida, ?Orthotetes sp. of the Orthotetida, Rhipidomella sp., Schizophoria sp. of the Orthida, Cleiothyridina cf. sublamellosa Hall, 1858, Composita sulcata Weller, 1914 of the Athyridida, Anthracospirifer shawi shawi Gordon, 1975, Anthracospirifer aff. A. shawi of the Spiriferida, Punctospirifer sp. of the Spiriferinida, and Girtyella indianensis Girty, 1909 of the Terebratulida, with the addition of one undetermined linoproductid and one genus and possibly two undetermined species of the Delthyridina. The assemblage shares affinities with upper Chesterian (middle Serpukhovian) Carlinia phillipsi and C. amsdeniana associations from western North American units, though the presence of Composita sulcata makes it also close to uppermost Chesterian faunas (Rhipidomella nevadensis and Composita popsiensis zones, upper Serpukhovian). The recorded faunal association, in terms of composition at the genus-level, is characteristic of brachiopod Unit 16 of Carter (1990a). Unit 16 spans the middle Chesterian (Gnathodus bilineatus conodont Zone) to upper Chesterian (Rachistognathus muricatus conodont Zone), corresponding to the upper Visean–Serpukhovian interval. A monospecific Vogegnathus postcampbelli conodont assemblage from the same locality confirms a late Chesterian (Serpukhovian) age of the fauna.
通过对美国内华达州埃尔科卡林峡谷上密西西比统通卡地层中的腕足类群进行系统研究,发现了 13 个物种,分别代表 12 个属和 7 个目:产品目中的 Antiquatonia sp.、Flexaria sp.、Marginatia sp.、Echinoconchus sp.、Orthetida 的 Orthotetes sp.、Rhipidomella sp.、Schizophoria sp、的 Echinoconchus sp.,直翅目的 Orthotetes sp.,直翅目的 Rhipidomella sp.、Schizophoria sp.,甲壳纲的 Cleiothyridina cf. sublamellosa Hall, 1858, Composita sulcata Weller, 1914,螺旋纲的 Anthracospirifer shawi shawi Gordon, 1975, Anthracospirifer aff.和 Terebratulida 的 Girtyella indianensis Girty, 1909,以及 Delthyridina 的一个未确定的线虫属和一个属,可能还有两个未确定的种。该动物群与北美西部的上切斯特期(Serpukhovian 中期)Carlinia phillipsi 和 C. amsdeniana 动物群有亲缘关系,但 Composita sulcata 的出现使其也接近于上切斯特期动物群(Rhipidomella nevadensis 和 Composita popsiensis 区,Serpukhovian 上期)。从属一级的组成来看,所记录的动物群关联是卡特(1990a)的腕足动物单元 16 的特征。第 16 单元横跨中切斯特期(Gnathodus bilineatus 锥齿轮区)至上切斯特期(Rachistognathus muricatus 锥齿轮区),相当于上维西期-上塞普霍夫期。同一地点出土的一个单特异性的 Vogegnathus postcampbelli 锥齿动物群证实了该动物群的晚切斯特期(Serpukhovian)时代。
{"title":"Brachiopods from the Serpukhovian Tonka Formation of Carlin Canyon, Elko, Nevada (USA): Systematics and biostratigraphy","authors":"","doi":"10.1016/j.palwor.2024.03.006","DOIUrl":"10.1016/j.palwor.2024.03.006","url":null,"abstract":"<div><div>Systematic study of a brachiopod assemblage from the Upper Mississippian Tonka Formation in Carlin Canyon, Elko, Nevada, USA, led to the recognition of 13 species, representing 12 genera and seven orders: ?<em>Antiquatonia</em> sp., <em>Flexaria</em> sp., ?<em>Marginatia</em> sp., <em>Echinoconchus</em> sp. of the Productida, ?<em>Orthotetes</em> sp. of the Orthotetida, <em>Rhipidomella</em> sp., <em>Schizophoria</em> sp. of the Orthida, <em>Cleiothyridina</em> cf. <em>sublamellosa</em> <span><span>Hall, 1858</span></span>, <em>Composita sulcata</em> <span><span>Weller, 1914</span></span> of the Athyridida, <em>Anthracospirifer shawi shawi</em> <span><span>Gordon, 1975</span></span>, <em>Anthracospirifer</em> aff. <em>A. shawi</em> of the Spiriferida, <em>Punctospirifer</em> sp. of the Spiriferinida, and <em>Girtyella indianensis</em> <span><span>Girty, 1909</span></span> of the Terebratulida, with the addition of one undetermined linoproductid and one genus and possibly two undetermined species of the Delthyridina. The assemblage shares affinities with upper Chesterian (middle Serpukhovian) <em>Carlinia phillipsi</em> and <em>C. amsdeniana</em> associations from western North American units, though the presence of <em>Composita sulcata</em> makes it also close to uppermost Chesterian faunas (<em>Rhipidomella nevadensis</em> and <em>Composita popsiensis</em> zones, upper Serpukhovian). The recorded faunal association, in terms of composition at the genus-level, is characteristic of brachiopod Unit 16 of <span><span>Carter (1990a)</span></span>. Unit 16 spans the middle Chesterian (<em>Gnathodus bilineatus</em> conodont Zone) to upper Chesterian (<em>Rachistognathus muricatus</em> conodont Zone), corresponding to the upper Visean–Serpukhovian interval. A monospecific <em>Vogegnathus postcampbelli</em> conodont assemblage from the same locality confirms a late Chesterian (Serpukhovian) age of the fauna.</div></div>","PeriodicalId":48708,"journal":{"name":"Palaeoworld","volume":null,"pages":null},"PeriodicalIF":1.7,"publicationDate":"2024-03-26","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"140399018","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":3,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"OA","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 0
Diversity and discrimination of large ornithopods revealed through their tracks (Lower Cretaceous, Spain): A phenetic correlation approach 通过足迹揭示大型鸟脚类动物的多样性和鉴别力(西班牙,下白垩统):表型关联方法
IF 1.7 3区 地球科学 Q2 PALEONTOLOGY Pub Date : 2024-03-24 DOI: 10.1016/j.palwor.2024.03.005
Large ornithopods were frequent in the alluvial-to-coastal sedimentary systems developed during the Barremian in the Iberian Peninsula. Here, several pes track casts of large ornithopods from the Barremian Camarillas Formation of the southwestern sector of the Maestrazgo Basin (Iberian Basin, Spain) are analyzed. Two morphotypes of tracks from three different size classes are differentiated based on some morphological features, such as length of digits, the width of the “heel” pad impression, and width of the proximal part of digit III. These casts are assigned to Caririchnium isp. Morphotype 1 is represented by small to large-sized tracks, whereas Morphotype 2 by medium-sized tracks. Morphological variation seen among tracks of Morphotype 1 is interpreted to be possibly an ontogenetic variation. On the contrary, the differences seen between Morphotype 1 and 2 cannot be explained only by extramorphological causes, so might represent different trackmakers, especially when taking into account the considerable Barremian ornithopod diversity. A modified phenetic correlation is carried out between several well-preserved casts and the identified feet of Barremian ornithopods from Iberia, in order to infer the putative trackmakers. Morphotype 1 fits with the foot skeletal structure of the large styracosternan Iguanodon, including small-sized tracks that are perfectly accommodated to that of perinates of I. galvensis. Morphotype 2 matches better to the pes skeletal structure of the medium-sized Mantellisaurus. Similar two morphotypes can be also identified in other areas of the Lower Cretaceous of Europe, so, they could be tentatively produced by the two sized groups of styracosternans typical in the Early Cretaceous of Europe. Therefore, the ichnological analysis may allow differentiation of the diversity known through the direct record. In addition, the paleoecological analysis indicates a spatial niche partitioning between two size groups of styracosternans, because large-sized tracks and bones of these dinosaurs are the most common in such sediments.
在伊比利亚半岛巴里米亚时期形成的冲积-海岸沉积系统中,经常出现大型兽脚类动物。本文分析了 Maestrazgo 盆地(西班牙伊比利亚盆地)西南部巴雷姆时期 Camarillas 地层中大型鸟脚类动物的几枚脚印。根据一些形态特征,如指骨长度、"脚跟 "垫印的宽度和第三指骨近端部分的宽度,对三个不同大小级别的两种形态的足迹进行了区分。这些石膏被归类为 Caririchnium isp。形态 1 代表小到大的足迹,而形态 2 代表中等大小的足迹。形态类型 1 的足迹之间的形态差异可能是一种个体发育差异。相反,形态 1 和形态 2 之间的差异不能仅用形态外的原因来解释,因此可能代表了不同的履带制作者,特别是考虑到巴里米亚节肢动物的多样性。为了推断可能的履带制作者,我们对伊比利亚地区几种保存完好的铸模和已鉴定的巴里米亚兽脚类足部进行了修正的表型相关性分析。形态 1 与大型伊瓜齿兽的足部骨骼结构相吻合,包括与伊瓜齿兽周足完全吻合的小尺寸足迹。形态 2 与中型曼特力龙的脚骨骼结构更为吻合。在欧洲下白垩世的其他地区也可以发现类似的两种形态,因此可以初步认为它们是由欧洲早白垩世典型的两种大小的styracosternans类群产生的。因此,通过手足学分析,可以对直接记录中已知的多样性进行区分。此外,古生态学分析表明,两种体型的styracosternans之间存在空间生态位分区,因为这些恐龙的大体型足迹和骨骼在此类沉积物中最为常见。
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引用次数: 0
Review and update on the applications of inertinite macerals in coal geology, paleoclimatology, and paleoecology 惰性矿物在煤炭地质学、古气候学和古生态学中的应用回顾与更新
IF 1.7 3区 地球科学 Q2 PALEONTOLOGY Pub Date : 2024-03-18 DOI: 10.1016/j.palwor.2024.03.003
Inertinite is a coal component group recognized under microscope. The origin, formation, and applications of inertinite continue to be debated. Many important achievements have been reported in the recent years. The most important advance is that the presence of inertinite macerals has been used as the most critical evidence of paleowildfires. However, the origin of some micrinite has been recognized as liptinitic/huminitic or as kaolinite, and even as voids. Some secretinite and funginite can be formed by microbial and fungal oxidation. Some researchers questioned the validity of using the maceral (including inertinite) ratios to indicate the depositional environment and appealed to stop using maceral parameters (including inertinite) to explain peat-forming environments and vegetation. Because the proven inertinite macerals formed by organic matter degradation comprised only a small part of all inertinite groups, most inertinite macerals can be used as evidence of paleowildfires, and the inertinite macerals may be used to estimate the wildfire type. The inertinite reflectance values may be used to estimate the wildfire temperature, and the oxygen level can be estimated by the inertinite contents. Furthermore, the relationship between inertinite and other wildfire evidences, e.g., char, charcoal, soot, and fusain, has also been clarified.
惰性石英是一种在显微镜下可以识别的煤成分。关于惰性石英的起源、形成和应用仍有争议。近年来,已有许多重要成果被报道。最重要的进展是,惰性微晶的存在已被作为古野火的最关键证据。然而,一些微晶石的来源已被确认为锂辉石/光辉石或高岭石,甚至是空隙。一些秘长岩和风成岩可能是由微生物和真菌氧化形成的。一些研究人员对使用大理石(包括惰性石)比率来表示沉积环境的有效性提出质疑,并呼吁停止使用大理石参数(包括惰性石)来解释泥炭形成环境和植被。由于已证实的有机质降解形成的惰性大分子只占所有惰性大分子组的一小部分,因此大部分惰性大分子可用作古野火的证据,惰性大分子可用于估计野火类型。惰性无机物的反射率值可用来估计野火的温度,氧气含量可通过惰性无机物的含量来估计。此外,惰性石墨与其他野火证据(如炭、木炭、烟尘和燧石)之间的关系也得到了澄清。
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引用次数: 0
Earliest upper Barremian (Lower Cretaceous) record of bivalve Pinna (Pinnidae) from the Kopet-Dagh Basin, northeastern Iran and its possible predators 伊朗东北部 Kopet-Dagh 盆地最早的上白垩世(下白垩世)双壳类动物 Pinna (Pinnidae) 记录及其可能的捕食者
IF 1.7 3区 地球科学 Q2 PALEONTOLOGY Pub Date : 2024-03-18 DOI: 10.1016/j.palwor.2024.03.004
The bivalves Pinna sp. cf. cretacea (Schlotheim, 1813) and Pinna cretacea cretacea (Schlotheim, 1813) are systematically described for the first time from the ammonite-constrained upper Barremian (Lower Cretaceous) strata of the Kopet-Dagh Basin, northeastern Iran. This is also, the first record of the Family Pinnidae from the Kopet-Dagh Basin. The specimens were collected from the basal part of the Sarcheshmeh Formation, exposed in the Bojnurd city, North Khorasan province. Additionally, this study includes observations on predation scars (such as scalloped, embayed, and cleft scars), and encrustations by orbitolinids on the Pinna samples. Insights into the contemporary paleoenvironment, characterized by quiet and shallow waters with a soft, muddy substrate, are also discussed.
(Schlotheim, 1813) 和 (Schlotheim, 1813) 首次在伊朗东北部 Kopet-Dagh 盆地受氨蛋白约束的上巴里米统(下白垩统)地层中系统地描述了双壳类。这也是科佩特-达赫盆地凤蝶科的首次记录。标本采集自北呼罗珊省布伊诺德市出露的萨尔切什梅赫层基底部分。此外,这项研究还包括对捕食疤痕(如扇形疤痕、凹陷疤痕和裂缝疤痕)以及眶鞘类动物在样本上结壳情况的观察。本研究还讨论了对当代古环境的见解,该环境的特点是水域安静、浅,底质松软、泥泞。
{"title":"Earliest upper Barremian (Lower Cretaceous) record of bivalve Pinna (Pinnidae) from the Kopet-Dagh Basin, northeastern Iran and its possible predators","authors":"","doi":"10.1016/j.palwor.2024.03.004","DOIUrl":"10.1016/j.palwor.2024.03.004","url":null,"abstract":"<div><div>The bivalves <em>Pinna</em> sp. cf. <em>cretacea</em> (<span><span>Schlotheim, 1813</span></span>) and <em>Pinna cretacea cretacea</em> (<span><span>Schlotheim, 1813</span></span><span><span>) are systematically described for the first time from the ammonite-constrained upper Barremian (Lower Cretaceous) strata of the Kopet-Dagh Basin, northeastern Iran. This is also, the first record of the Family Pinnidae from the Kopet-Dagh Basin. The specimens were collected from the basal part of the Sarcheshmeh Formation, exposed in the Bojnurd city, North Khorasan province. Additionally, this study includes observations on predation scars (such as scalloped, embayed, and cleft scars), and </span>encrustations by orbitolinids on the </span><em>Pinna</em><span> samples. Insights into the contemporary paleoenvironment, characterized by quiet and shallow waters with a soft, muddy substrate, are also discussed.</span></div></div>","PeriodicalId":48708,"journal":{"name":"Palaeoworld","volume":null,"pages":null},"PeriodicalIF":1.7,"publicationDate":"2024-03-18","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"140168873","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":3,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 0
First Dapingian linguliform microbrachiopods from the Argentine Precordillera (Cuyania terrane): Taxonomy and faunal relationships 阿根廷前山地带(Cuyania terrane)的第一批Dapingian舌状微腕足动物:分类和动物关系
IF 1.7 3区 地球科学 Q2 PALEONTOLOGY Pub Date : 2024-03-18 DOI: 10.1016/j.palwor.2024.03.002
New records of linguliform brachiopods from the Middle Ordovician of Argentina, coming from the base of the Gualcamayo Formation, are described and illustrated. The sampled levels correspond to the first 3 m at the Potrerillos Creek section, Argentine Precordillera of San Juan, assigned to the lower part of the Baltoniodus navis Zone (middle Dapingian). The fauna consists of the lingulids Palaeoglossa? sp., Elliptoglossa vulgaris Hansen and Holmer and Paterula sp., together with the acrotretids Conotreta andina Lavié, Serra and Feltes, Scaphelasma zharykensis Popov, Torynelasma? sp., Numericoma simplex?, and Eoconulus sp. This relatively diverse association is the first of Dapingian age in the Cuyania terrane with a mixed fauna, which shows affinities with the regions of Baltica, Bohemia, Avalonia, South China, and Laurentia.
本文描述并说明了阿根廷中奥陶纪瓜尔卡马约地层底部的鳞状腕足类新记录。取样层位于阿根廷圣胡安前缘山脉 Potrerillos 溪地段的前 3 米处,属于中奥陶纪(中达平纪)下段。该动物群包括矛形目(Lingulids)、汉森(Hansen)、霍尔默(Holmer)和sp.,以及针形目(acrotretids)的拉维(Lavié)、塞拉(Serra)和费尔特斯(Feltes)、波波夫(Popov)、sp.、sp.和 sp.。这个相对多样化的群落是库亚尼亚地层中第一个达平夏时代的混合动物群落,显示出与波罗的海、波希米亚、阿瓦鲁尼亚、华南和劳伦西亚地区的亲缘关系。
{"title":"First Dapingian linguliform microbrachiopods from the Argentine Precordillera (Cuyania terrane): Taxonomy and faunal relationships","authors":"","doi":"10.1016/j.palwor.2024.03.002","DOIUrl":"10.1016/j.palwor.2024.03.002","url":null,"abstract":"<div><div><span>New records of linguliform brachiopods from the Middle Ordovician of Argentina, coming from the base of the Gualcamayo Formation, are described and illustrated. The sampled levels correspond to the first 3 m at the Potrerillos Creek section, Argentine Precordillera of San Juan, assigned to the lower part of the </span><em>Baltoniodus navis</em> Zone (middle Dapingian). The fauna consists of the lingulids <em>Palaeoglossa</em>? sp., <em>Elliptoglossa vulgaris</em> Hansen and Holmer and <em>Paterula</em> sp., together with the acrotretids <em>Conotreta andina</em> Lavié, Serra and Feltes, <em>Scaphelasma zharykensis</em> Popov, <em>Torynelasma</em>? sp., <em>Numericoma simplex</em>?, and <em>Eoconulus</em><span><span> sp. This relatively diverse association is the first of Dapingian age in the Cuyania terrane with a mixed fauna, which shows affinities with the regions of Baltica, Bohemia, </span>Avalonia, South China, and Laurentia.</span></div></div>","PeriodicalId":48708,"journal":{"name":"Palaeoworld","volume":null,"pages":null},"PeriodicalIF":1.7,"publicationDate":"2024-03-18","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"140168827","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":3,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 0
Palynological assemblages from Hongguleleng Formation of Western Junggar, Northwest China and their correlation with conodont zonation 中国西北准噶尔西部红古楞地层的古生物组合及其与锥齿动物分带的相关性
IF 1.7 3区 地球科学 Q2 PALEONTOLOGY Pub Date : 2024-03-18 DOI: 10.1016/j.palwor.2024.03.001
The Upper Devonian Hongguleleng Formation is a significant stratigraphic unit near the Frasnian/Famennian and Devonian/Carboniferous boundaries of the Kazakhstan Paleoplate. However, its age is still under debate. A new palynostratigraphic analysis was conducted at the Gennaren section to provide a more accurate biostratigraphic assignment. In this study, we identified 43 species belonging to 26 spore genera, including those in open nomenclature. Despite the poor preservation of the palynofloras, the spore taxa were categorized into two assemblages. Assemblage I is established at the lower part of the lower member of the Hongguleleng Formation, containing Cornispora varicornata, cf. Auroraspora pseudocrista, and Cyrtospora cristifera. Assemblage II is from the upper part of the lower member of the Hongguleleng Formation, including Grandispora cornuta, Grandispora famennensis var. famennensis, Grandispora cf. famennensis var. minutus, Grandispora microseta, and Rugospora radiata. These assemblages are compared with the Western European DV Oppel Zone (lower-middle Famennian), and the GF to VCo Oppel zones. The assemblages are equivalent to the conodont crepidarhomboidea and marginifera to Lower trachytera zones (middle-upper Famennian).
泥盆纪上统红古楞地层是哈萨克斯坦古地层中靠近弗拉斯年/法门年和泥盆纪/石炭纪边界的一个重要地层单元。然而,其年龄仍存在争议。为了提供更准确的生物地层划分,我们在 Gennaren 剖面进行了新的古地层分析。在这项研究中,我们确定了属于 26 个孢粉属的 43 个物种,其中包括那些开放命名的物种。尽管古植物保存较差,但我们还是将孢子类群分为两个集合体。组合 I 位于红古楞地层下部,包含 、 、 和 。组合 II 位于红古楞地层下统的上部,包括Ⅴ变种、Ⅴ变种、Ⅴ变种和Ⅴ变种。这些组合与西欧 DV 奥佩尔带(法门年中下期)以及 GF 至 VCo 奥佩尔带进行了比较。这些化石群与同牙- 和下区(法门纪中上叶)相当。
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Palaeoworld
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