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Palaeobiodiversity and Palaeoenvironments最新文献

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Global palaeobiogeographic distribution patterns of the Cenozoic pleurotomariid gastropods (Family: Pleurotomariidae Swainson, 1840) 新生代胸腹足类全球古地理分布格局(科:胸腹足科,1840)
4区 地球科学 Q1 Earth and Planetary Sciences Pub Date : 2023-10-11 DOI: 10.1007/s12549-023-00589-9
Kanishka Bose, Shiladri S. Das, Subhronil Mondal
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引用次数: 0
Organic carbon isotope stratigraphy of Devonian-Carboniferous boundary sections in the Rhenish Mountains 莱茵山脉泥盆系—石炭系界线剖面有机碳同位素地层学研究
4区 地球科学 Q1 Earth and Planetary Sciences Pub Date : 2023-09-26 DOI: 10.1007/s12549-023-00584-0
Dieter Korn, Franziska E. Schmid, Ulrich Struck
Abstract The boundary between the Devonian and the Carboniferous has been drawn using ammonoids, conodonts and miospores, while geochemical data have only rarely been used. The sampling of eight sections (Aprath, Apricke, Effenberg, Wocklum, Stockum, Drewer WJ, Drewer WA, Marsberg) at the northern margin of the Rhenish Mountains demonstrates the potential of the isotope ratio of organic carbon to regionally correlate sections in different facies areas. With the help of the carbon isotopes, a distinct stratigraphic succession is documented, which is characterised by several positive and negative excursions; this succession was recorded in all examined sections. The carbon isotopes can therefore make a significant contribution to the stratigraphic subdivision of sections and complement the biostratigraphic methods.
泥盆纪与石炭系界线的划分主要是利用菊石、牙形刺和微孢子进行的,而地球化学资料的应用却很少。通过对莱因尼山脉北缘8个剖面(Aprath、Apricke、Effenberg、Wocklum、Stockum、Drewer WJ、Drewer WA、Marsberg)的采样,揭示了有机碳同位素比值在不同相区区域对应剖面上的潜力。在碳同位素的帮助下,记录了一个明显的地层演替,其特征是多次正偏移和负偏移;这种演替在所有被检查的切片中都有记录。因此,碳同位素可以对剖面的地层细分做出重要贡献,并补充生物地层方法。
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引用次数: 0
Lithofacies variability and facies analysis of a Givetian reef in the southwestern Lahn Syncline (Rhenish Massif, Germany) 德国莱茵地块Lahn向斜西南部吉文田礁岩相变异性及相分析
4区 地球科学 Q1 Earth and Planetary Sciences Pub Date : 2023-09-19 DOI: 10.1007/s12549-023-00585-z
Peter Königshof, Steffen Loos, Julia Rutkowski
Abstract A 200 m thick drill core penetrating the Givetian Hahnstätten Reef in the southwestern Lahn Syncline (Rhenish Massif) was investigated. A range of different depositional environments is described based on lithofacies and microfacies analysis. All in all, nine lithofacies types (FTs) are distinguished, which can include subfacies types. The majority of lithofacies of these ultrapure carbonates is represented by lime mudstone and fenestral microbialites, all pointing to shallow subtidal, intertidal to even supratidal low-energy palaeoenvironments. In contrast, more high-energy parts of the reef were dominated by bioclastic rubble deposits (e.g. rudstone). Autochthonous, reef-building carbonates are represented by bafflestone and framestone. Diversity of reef building organisms (stromatoporoids and corals) is low and is dominated by Stachyodes , Actinostroma , Stromatopora , and Thamnopora and alveolitids, respectively. Other bioclasts are brachiopods, gastropods, ostracods, foraminifera, echinoderms, trilobites, and conodonts in descending order. Development of the Hahnstätten Reef is interpreted as having been controlled mainly by synsedimentary tectonics and volcanism with contributions from eustasy. The occurrence of Stringocephalus burtini in the entire section and conodont findings, which provide more precise biostratigraphic data confirm an early to middle Givetian age ( Polygnathus rhenanus/varcus Zone to Polygnathus ansatus Zone) of the succession. The average quality of the ultrapure carbonates lies at 97.68% CaO (excl. loss of ignition), with 70% of the core ranging between 98% and 99% CaO. This extremely high purity makes it difficult to identify correlations between lithofacies and geochemical data.
摘要:对Lahn向斜(莱茵地块)西南部Givetian Hahnstätten礁的200 m厚岩心进行了研究。根据岩相和微相分析,描述了一系列不同的沉积环境。总的来说,划分出9种岩相类型,其中包括亚相类型。这些超纯碳酸盐岩的岩相以灰岩泥岩和窗缘微生物岩为代表,均指向浅层潮下、潮间甚至潮上低能古环境。相比之下,珊瑚礁的高能量部分主要由生物碎屑碎屑沉积物(如rudstone)组成。原生造礁碳酸盐以挡板岩和框架岩为代表。造礁生物(叠层孔虫和珊瑚)多样性较低,分别以Stachyodes、Actinostroma、Stromatopora、Thamnopora和alveolitids为主。其他生物碎屑依次为腕足动物、腹足动物、介形虫、有孔虫、棘皮动物、三叶虫和牙形刺。Hahnstätten礁的发育被解释为主要受同沉积构造和火山作用的控制,并有海游带的贡献。整个剖面中burtini链头虫的出现和牙形刺的发现提供了更精确的生物地层资料,证实了早至中期(Polygnathus rhenanus/varcus带至Polygnathus ansatus带)的演替。超纯碳酸盐的平均质量为97.68%(不含燃失),其中70%的岩心在98% ~ 99%之间。这种极高的纯度使得很难确定岩相和地球化学数据之间的相关性。
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引用次数: 0
Where’s dinner? Variation in carnivoran distributional responses to the mid-Vallesian faunal turnover 晚餐在哪里?中瓦利西亚区动物群更替中肉食动物分布响应的变异
4区 地球科学 Q1 Earth and Planetary Sciences Pub Date : 2023-09-13 DOI: 10.1007/s12549-023-00588-w
Paulina A. Madern, Yanell Braumuller, Aslı Ceren Mavikurt, Serdar Mayda, Leonie Bergwerff, Naomi Janssen, Juan Cantalapiedra, Josep Maria Robles, Isaac Casanovas-Vilar, Peter C. van Welzen, Lars W. van den Hoek Ostende
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引用次数: 0
Early Paleogene precipitation patterns over East Asia: Was there a monsoon after all? 东亚古近纪早期的降水模式:到底有季风吗?
IF 1.4 4区 地球科学 Q1 Earth and Planetary Sciences Pub Date : 2023-09-08 DOI: 10.1007/s12549-023-00586-y
O. Bondarenko, Torsten Utescher
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引用次数: 0
The identity of the Silurian retiolitine genera Paraplectograptus and Sagenograptoides (Graptoloidea, Retiolitinae)
IF 1.4 4区 地球科学 Q1 Earth and Planetary Sciences Pub Date : 2023-08-28 DOI: 10.1007/s12549-023-00587-x
J. Maletz
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引用次数: 0
Late Early to late Middle Pleistocene medium-sized deer from the Italian Peninsula: implications for taxonomy and biochronology 意大利半岛中更新世晚期早期至晚期中型鹿:分类学和生物年代学意义
IF 1.4 4区 地球科学 Q1 Earth and Planetary Sciences Pub Date : 2023-08-09 DOI: 10.1007/s12549-023-00583-1
B. Mecozzi, R. Sardella, M. Breda
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引用次数: 1
The shark and ray teeth of the Lower Miocene (Upper Marine Molasse) from Ballendorf, Baden-Württemberg, Southern Germany 来自德国南部巴登-符腾堡州巴伦多夫的下中新世(上海洋Molasse)的鲨鱼和鳐鱼牙齿
IF 1.4 4区 地球科学 Q1 Earth and Planetary Sciences Pub Date : 2023-08-03 DOI: 10.1007/s12549-023-00582-2
Olaf Höltke, E. Maxwell, Helmut Bracher, M. Rasser
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引用次数: 0
Eocene sediments and a fresh to brackish water biota from the early rifting stage of the Upper Rhine Graben (west of oil field Landau, southwest Germany): implications for biostratigraphy, palaeoecology and source rock potential 上莱茵地堑早期裂谷阶段的始新世沉积物和淡水-微咸水生物群(德国西南部兰道油田西部):对生物地层学、古生态学和烃源岩潜力的影响
IF 1.4 4区 地球科学 Q1 Earth and Planetary Sciences Pub Date : 2023-07-21 DOI: 10.1007/s12549-023-00577-z
C. Hartkopf-Fröder, E. Martini, C. Heilmann-Clausen, F. Neumann, P. Schäfer, H. Wilkes, Johannes Böcker, M. Hottenrott
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引用次数: 0
Convergent evolution of defensive appendages – a lithobiomorph-like centipede with a scolopendromorph-type ultimate leg from about 100 million-year-old amber 防御附肢的聚合进化——一种类似石生物形态的蜈蚣,其最终腿来自约1亿年前的琥珀
IF 1.4 4区 地球科学 Q1 Earth and Planetary Sciences Pub Date : 2023-07-05 DOI: 10.1007/s12549-023-00581-3
G. T. Haug, J. Haug, C. Haug
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引用次数: 0
期刊
Palaeobiodiversity and Palaeoenvironments
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