Distribution of some species of fresh and brackish-water Ostracoda from the lower Pleistocene of SE Sicily

Q3 Environmental Science Biogeographia Pub Date : 2011-01-01 DOI:10.21426/B630110599
F. Sciuto
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引用次数: 3

Abstract

Biogeographia vol. XXX - 2011 (Pubblicato il 23 dicembre 2011) La Biogeografia della Sicilia Distribution of some species of fresh and brackish—water Ostracoda from the lower Pleistocene of SE Sicily FRANCESCO SCIUTO Dzpartimento di Scienze Biologic/ae, Geologic/Je eAmbz'entcz[z', Corso Itzzlzkz 55, 95129 Catania (Italy); e—mai/.-ficiuto @um'ct. it Key words: Ostracods, fresh and brackish water, Sicily, palaeobiogeography, biogeography. SUMMARY Lower Pleistocene marine sediments, evolving upwards to continental deposits, widely crop out along the south- western edge of the Hyblean Plateau in the Comiso-Vittoria area. This environmental transition is well recorded, along the right side of the Ippari river near “Cartiera Mulino” (Vittoria, Ragusa). Eight samples were collected in a geological section from this locality. The basal and middle layers contain abundant shallow—water marine ostracods whereas microfaunas from the top of the section only consist ofostracods which exclusively thrive in freshwater en- vironments. Three among the brackish and freshwater species are recorded (Aurilzz zzrborescem, Ilyocjypris gibba and Candomz neglecta) with remarks on their geographical and stratigraphical distribution. INTRODUCTION Ostracods are the most common extant arthropod group with abundant and continuous fossil record, due to their usually mineralised, easily preservable ex- oskeletons. They are able to thrive in all aquatic environments, mostly in marine settings from the sea level to oceanic depths, but also in continental waters: lakes, rivers and even humid ephemeral ponds. Consequently, ostracods represent an useful tool for palaeoenvironmental reconstructions and palaeobiogeographical analyses (Ducasse and Peypouquet, 1979; Babinot and Lethiers, 1984; Guernet and Lethiers, 1984; Carbonel, 1987; Passlovv, 1997; Martens et al., 2008). The present analysis is a contribution to the knowledge of the palaeobio— geographic distribution of/lurila czrborescem (Brady, 1865), Ilyocypris gibbzz (Ramdohr, 1808) and Ccmdomz neglecta Sars 1887, here first recorded from Lower Pleistocene sediments from SE Sicily.
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西西里岛东南部下更新世淡水和咸水介形类的分布
La Biogeografia della Sicilia西西里岛东南部下更新世部分淡水和咸水介形类的分布FRANCESCO SCIUTO Dzpartimento di Scienze Biologic/ae, geology /Je eAmbz'entcz ', Corso Itzzlzkz 55, 95129 Catania (Italy);来函/。-ficiuto @um 'ct。关键词:介形类,淡水和咸淡水,西西里岛,古生物地理,生物地理下更新世海相沉积物沿科米索-维多利亚地区海布良高原西南缘广泛生长,向上演化为陆相沉积。这种环境转变在伊帕里河右侧的“Cartiera Mulino”(维多利亚,拉古萨)附近得到了很好的记录。在该地区的一个地质剖面中采集了8个样品。基层和中间层含有丰富的浅水介形类,而顶部的微动物群仅由只在淡水环境中生长的介形类组成。记录了其中的3种(Aurilzz zzrborescem, Ilyocjypris gibba和Candomz忽视ta),并对其地理和地层分布进行了评述。介形类是现存最常见的节肢动物类群,由于它们的前骨骼通常是矿化的,易于保存,因此化石记录丰富且连续。它们能够在所有水生环境中茁壮成长,主要是在从海平面到海洋深处的海洋环境中,但也可以在大陆水域:湖泊、河流甚至潮湿的短暂池塘中茁壮成长。因此,介形类是古环境重建和古生物地理分析的有用工具(Ducasse和Peypouquet, 1979;Babinot and Lethiers, 1984;Guernet and Lethiers, 1984;Carbonel, 1987;Passlovv, 1997;Martens et al., 2008)。本文的分析有助于了解/lurila czrborescem (Brady, 1865)、Ilyocypris gibbzz (Ramdohr, 1808)和Ccmdomz ecta Sars(1887)的古地理分布,它们首次记录于西西里岛东南下更新世的沉积物中。
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来源期刊
Biogeographia
Biogeographia Environmental Science-Ecology
CiteScore
2.30
自引率
0.00%
发文量
18
审稿时长
28 weeks
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