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Evidence of Predation on Early Pleistocene Freshwater Ostracods (Umbria, Central Italy)

机译:早期优质水淡水滴答量(翁布里亚,意大利翁布里亚)的捕食证据

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Although drillholes in modern and ancient ostracods are known, the record is relatively scarce when compared to other taxa, and mainly exist with reference to the marine environment. Moreover, less is known about perforated ostracods, and more generally, about bioerosion in freshwater environments. Traces of predation on freshwater ostracods are reported for the first time in deep-lake deposits belonging to the early Pleistocene Fosso Bianco Unit, and outcropping in the Cava Nuova section (Umbria, central Italy). Deposits are mainly clay to silty clay and sand; the fossil record is sparse, and is mainly comprised of very rare gastropods and bivalves, ostracods and plant remains (leaves, seeds and wood’s fragments). The association of ostracods consists of Candona (Neglecandona) neglecta , Caspiocypris basilicii, Caspiocypris tiberina, Caspiocypris perusia, Caspiocypris tuderis , Caspiocypris posteroacuta , and Cyprideis torosa . The Caspiocypris group, considered to be endemic to the grey clays of the Fosso Bianco Unit, present the majority of specimens affected by predation, with a prevalence of predated female valves and a comparable number of right and left predated valves, while only a few of Candona (N.) neglecta (adult and juvenile) valves are perforated. Traces of predation for nourishment, represented by microborings of different types, were abscribed to the ichnospecies Oichnus paraboloides Bromley 1981, Oichnus simplex Bromley 1981, Oichnus gradatus Nielsen and Nielsen 2001, Oichnus ovalis Bromley 1993, and Dipatulichnus rotundus Nielsen and Nielsen 2001. Microboring affected both adult and juvenile specimens, evidencing prey–predator coexistence in the same environment over a long period of time. This report makes a fundamental contribution to the knowledge of predation in this peculiar confined environment, also suggesting prey–predator relations over a relatively short time interval (80–160 ka).
机译:虽然众所周知,探测器在现代和古代奥斯特拉科克,但与其他分类群相比,记录相对稀缺,并主要存在于海洋环境。此外,较少是关于穿孔的滴答物,更通常是关于淡水环境中的生物渗透的。在属于早期更新世福索比亚科单位的深湖矿床中首次报告了淡水滴答物的痕量,并在Cava Nuova部分(意大利翁布里亚)露出露出。存款主要是粘土和沙子;化石纪录稀疏,主要由非常罕见的胃胃和纤维植物,蛇斑和植物留下(叶子,种子和木材的碎片)。奥斯特拉科德的协会由坎迪纳(Degrescandona)疏忽,caspiocypris basilicii,Caspiocypris tiberina,caspiocypris perusia,caspiocypris tuderis,caspiocypris posteroacuta和caspiocypris posteroacuta和caspiocypris posteroacuta。 Caspiocypris组被认为是流体福索银币单元的灰色粘土的流行,呈现了捕食影响的大部分标本,捕获的雌性阀门的患病率和相当数量的右左右阀门,而只有几个Candona(N.)疏忽(成人和少年)阀门是穿孔的。由不同类型的微生物捕获的营养痕迹,不同类型的微生物,Ochnospstex Bromley 1981,Oichnus Simplex Bromley和Nielsen 2001,Oichnus ovalis Bromley 1993,以及Dipatulichnus rotundus nielsen和Nielsen 2001.微生物影响成人和少年标本都在很长一段时间内在同一环境中证明了猎物捕食者共存。本报告对该特殊狭窄环境中的捕食知识进行了根本贡献,也提出了在相对较短的时间间隔(80-160 kA)上的牺牲品 - 捕食者关系。

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