Trace fossil assemblages from the Lower Devonian (Lochkovian-Emsian) of the Touat area (Reggane Basin, Algerian Sahara) and their palaeoenvironmental significance

IF 1.4 4区 地球科学 Q3 BIODIVERSITY CONSERVATION Palaeobiodiversity and Palaeoenvironments Pub Date : 2024-05-14 DOI:10.1007/s12549-024-00602-9
Abdelmalik Draoui, Mohamed Bendella, Bruno Ferré, Mostapha Benzina, Mansour Zaagane, Khaldia Ziouit, Abdelouafi Boutadaraa, Ahmed Boutadaraa, Abderraouf Salah
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Abstract

Mixed siliciclastic-carbonate deposits of Lower Devonian (Lochkovian-Emsian) age are exposed in the northeastern part of the Reggane Basin (Touat region). Based on lithological, sedimentological and palaeontological data, these deposits are subdivided into four distinct lithological units: Unit A characterises the Silurian-Devonian transitional zone; Unit B consists of a thick succession of Lochkovian-Pragian age, whereas Units C and D both document Emsian deposits. The studied section exhibits low to moderate ichnodiversity consisting of 14 ichnotaxa: Arenicolites isp., Chondrites isp., Curvolithus multiplex, Lockeia siliquaria, Monomorphichnus isp., Neonereites bisserialis, Neonereites uniserialis, Ophiomorpha isp., Palaeophycus isp., Planolites isp., Psilonichnus upsilon, Skolithos linearis, S. verticalis, and Thalassinoides isp. Both Curvolithus multiplex and Psilonichnus upsilon are documented for the first time from Palaeozoic deposits of the Saharan platform. These ichnofaunas are commonly ascribed to the Skolithos and Cruziana ichnofacies. Five distinct ichnoassemblages (Ichnoassemblages A to E) were defined, reflecting palaeoenvironmental changes from the foreshore to upper offshore zones, with frequent storm influence. Ichnofabric analysis of the section studied reveals six levels with different bioturbation intensities showing different palaeoecological conditions in various environmental settings (Monospecific Planolites, Lower combined Skolithos-Arenicolites, Combined Skolithos-Thalassinoides, Monospecific Skolithos, and Upper combined Skolithos-Arenicolites and Reburrowed Chondrites ichnofabrics). The vertical evolution of these deposits displays the successive deepening and shallowing trends recorded during the Lower Devonian in this area.

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图阿特地区(阿尔及利亚撒哈拉雷加内盆地)下泥盆统(洛科文-埃米西亚)的微量化石群及其古环境意义
雷加内盆地(图阿特地区)东北部出露了下泥盆纪(洛克维期-埃姆西期)硅质碎屑岩-碳酸盐混合沉积物。根据岩性、沉积学和古生物学数据,这些沉积物被细分为四个不同的岩性单元:A 单元是志留纪-德文纪过渡带的特征;B 单元包括厚厚的洛可可期-普拉格期演替,而 C 和 D 单元都记录了埃姆西亚沉积。所研究的剖面显示出低到中等程度的生物多样性,包括 14 个生物分类群:Arenicolites isp.、Chondrites isp.、Curvolithus multiplex、Lockeia siliquaria、Monomorphichnus isp.、Neonereites bisserialis、Neonereites uniserialis、Ophiomorpha isp.、Palaeophycus isp.、Planolites isp.、Psilonichnus upsilon、Skolithos linearis、S. verticalis 和 Thalassinoides isp.。Curvolithus multiplex 和 Psilonichnus upsilon 都是首次在撒哈拉平台的古生代沉积物中发现。这些蛭石通常归属于 Skolithos 和 Cruziana ichnofacies。该研究界定了五个不同的蛭石组合(蛭石组合 A 至 E),反映了从前缘到上近海区的古环境变化,以及频繁的风暴影响。对所研究断面的迭合结构分析表明,六个层级具有不同的生物扰动强度,显示了不同环境背景下的不同古生态条件(单特异性鳞片岩、下部组合鳞片岩-肾上腺鳞片岩、组合鳞片岩-Thalassinoides、单特异性鳞片岩以及上部组合鳞片岩-肾上腺鳞片岩和再碎屑软玉迭合结构)。这些沉积物的垂直演化显示了该地区下泥盆世期间所记录的连续加深和变浅趋势。
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来源期刊
Palaeobiodiversity and Palaeoenvironments
Palaeobiodiversity and Palaeoenvironments BIODIVERSITY CONSERVATIONPALEONTOLOGY -PALEONTOLOGY
CiteScore
3.90
自引率
14.30%
发文量
33
期刊介绍: Palaeobiodiversity and Palaeoenvironments is a peer-reviewed international journal for the publication of high-quality multidisciplinary studies in the fields of palaeobiodiversity, palaeoenvironments and palaeobiogeography. Key criteria for the acceptance of manuscripts are a global scope or implications of problems on a global scale significant not only for a single discipline, a focus on the diversity of fossil organisms and the causes and processes of change in Earth’s history. The topics covered include: Systematic studies of all fossil animal / plant groups with a special focus on palaeoenvironmental investigations, palaeoecosystems and climate changes in Earth’s history, environment-organism interaction, comparison of modern and ancient sedimentary environments, palaeoecology and palaeobiogeography.
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