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Quaternary non-marine ostracods of Runtuyoc lake, northern Argentina: New taxonomic descriptions and the implication for Holocene paleoenvironment

机译:阿根廷北部Runtuyoc湖第四纪非海洋类成龙类:新的分类学描述及其对全新世古环境的启示

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摘要

We performed an ostracod taxonomic analysis on samples from a shallow lake (Runtuyoc Lake) in north-western Argentina in order to contribute to the understanding of the evolution of this water body through the last 5000 years. The ostracod assemblages consist of 15 species, two species exclusively from modern samples (Herpetocypris helenae and Chlamydotheca incisa), 8 exclusively from Quaternary samples (Limnocythere jujunensis sp. nov., L. titicaca, L. alexanderi, L. aff. staplini, Cyprideis salebrosa, Penthesilenula incae, Cypridopsis vidua, Sarscypridopsis aculeata) and 5 from both, modern and Quaternary samples (Ilyocypris natural, Potamocypris smaragdina, Heterocypris incongruens, Heterocypris similis, Candona sp.). The lake is located in the Miraflores river course and is characterized nowadays by freshwater conditions, but a saline past is evident as it went through different periods of desiccation. From 5500 to 3000 cal a BP, the lake was absent, probably related to extreme dry conditions. Then, water inputs into the lake produced a saline shallow lake until to reach modern setting as a freshwater body basin. Runtuyoc lake records, supports the regional environmental trending change for the Argentinian northwest, with wetter conditions in the early and late Holocene, and arid for the middle Holocene at least from 5500 to 3000/2500 cal a BP.
机译:我们对阿根廷西北部一个浅湖(Runtuyoc湖)的样品进行了异种分类研究,以帮助人们了解过去5000年中该水体的演变。虫类群由15种组成,其中两种仅来自现代样品(Herpetocypris helenae和Chlamydotheca incisa),八种仅来自第四纪样品(Limnocythere jujunensis sp。nov。,L。titicaca,L。alexanderi,L。aff。staplini,Cyprideis)。 salebrosa,Penthesilenula incae,Cypridopsis vidua,Sarscypridopsis aculeata)和来自现代和第四纪样品(天然的Ilyocypris,Potamocypris smaragdina,Heterocypris incongruens,Heterocypris similis,Candona sp。)的5个。该湖位于米拉弗洛雷斯河道上,如今以淡水条件为特征,但由于经历了不同的干燥期,因此盐分明显。从5500到3000 cal BP,该湖不存在,可能与极端干燥的条件有关。然后,向湖中的水输入产生了一个盐碱的浅湖,直到达到现代设置为淡水体盆。 Runtuyoc湖的记录支持阿根廷西北地区的区域环境趋势变化,全新世早期和晚期条件较为湿润,中全新世干旱条件至少在5500至3000/2500 cal a BP。

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