SALINITY-RELATED PRESERVATION OF MOLLUSKS IN SHALLOW LAKES: IMPLICATIONS FOR THE UNDERSTANDING OF THE LACUSTRINE PAMPEAN FOSSIL RECORD

IF 1.5 4区 地球科学 Q2 GEOLOGY Palaios Pub Date : 2023-03-31 DOI:10.2110/palo.2021.048
Claudio G. De Francesco, G. Hassan
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引用次数: 1

Abstract

ABSTRACT: Premortem and postmortem processes significantly influence the formation of the molluscan fossil record in freshwater environments. Despite their importance for paleoenvironmental studies, they remain poorly understood. In Pampean shallow lakes, Holocene shell deposits of the euryhaline snail Heleobia parchappii show a relation with salinity, as preservation seems to be favored by brackish-saline water conditions. To explore if this pattern may respond to ecological (i.e., differential survival and reproduction) or taphonomic processes acting differently in freshwater and brackish-saline environments, we conducted a field-based study comparing premortem (abundance, length, width/length ratio, and crushing resistance in living and dead shells) and postmortem (fragmentation, fine-scale surface alteration, and loss of periostracum of dead shells) attributes along a modern lacustrine salinity gradient (0.5–40 ppt) in the Pampa plain of Argentina. Snails from saline lakes were smaller and more rotund than those from freshwater lakes, exhibiting higher abundances and resistances in death assemblages. They showed the highest fidelity in shell length and the best states of preservation, which were similar to values recorded in fossil shells. We concluded that shells deposited in saline lakes are better preserved than those deposited in freshwater lakes, giving rise to highly abundant shell concentrations, analogues to those shell-rich fossil levels recorded in Pampean lakes. Such abundance does not reflect the natural abundances of living snails, but rather is the result of the combined influence that less destructive environments and better shell intrinsic properties have on preservation.
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浅水湖泊软体动物与盐度相关的保存:对理解湖泊潘潘化石记录的启示
摘要:在淡水环境中,尸检和死后处理对软体动物化石记录的形成有重要影响。尽管它们对古环境研究很重要,但人们对它们的了解仍然很少。在潘潘浅水湖,广盐蜗牛Heleobia parchappii的全新世外壳沉积物显示出与盐度的关系,因为微咸水条件似乎有利于保存。为了探索这种模式是否会对淡水和微咸水环境中不同作用的生态(即不同的生存和繁殖)或物质过程做出反应,我们进行了一项基于实地的研究,比较了阿根廷潘帕平原现代湖泊盐度梯度(0.5-40ppt)的死壳和活壳的前壳(丰度、长度、宽长比和抗压性)和死壳(碎裂、细尺度表面蚀变和死壳周介壳的损失)属性。盐湖中的蜗牛比淡水湖中的蜗牛更小、更圆,在死亡组合中表现出更高的丰度和抗性。它们在外壳长度上表现出最高的保真度和最佳的保存状态,这与化石外壳中记录的值相似。我们得出的结论是,沉积在盐湖中的贝壳比沉积在淡水湖中的贝壳保存得更好,从而产生了高度丰富的贝壳浓度,类似于潘潘湖中记录的富含贝壳的化石水平。这种丰度并不能反映活蜗牛的自然丰度,而是破坏性较小的环境和较好的外壳固有特性对保存的综合影响的结果。
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来源期刊
Palaios
Palaios 地学-地质学
CiteScore
2.80
自引率
12.50%
发文量
40
审稿时长
6 months
期刊介绍: PALAIOS is a monthly journal, founded in 1986, dedicated to emphasizing the impact of life on Earth''s history as recorded in the paleontological and sedimentological records. PALAIOS disseminates information to an international spectrum of geologists and biologists interested in a broad range of topics, including, but not limited to, biogeochemistry, ichnology, paleoclimatology, paleoecology, paleoceanography, sedimentology, stratigraphy, geomicrobiology, paleobiogeochemistry, and astrobiology. PALAIOS publishes original papers that emphasize using paleontology to answer important geological and biological questions that further our understanding of Earth history. Accordingly, manuscripts whose subject matter and conclusions have broader geologic implications are much more likely to be selected for publication. Given that the purpose of PALAIOS is to generate enthusiasm for paleontology among a broad spectrum of readers, the editors request the following: titles that generate immediate interest; abstracts that emphasize important conclusions; illustrations of professional caliber used in place of words; and lively, yet scholarly, text.
期刊最新文献
NEW QUANTITATIVE DESCRIPTORS (SHAPE AND MACROBORING) OF BIOGENIC NODULES: EXAMPLES FROM THE LESSER ANTILLES AND NEW ZEALAND LOCOMOTION TRACES EMPLACED BY MODERN STALKLESS COMATULID CRINOIDS (FEATHERSTARS) A FOSSIL FOREST FROM ITALY REVEALS THAT WETLAND CONIFERS THRIVED IN EARLY PERMIAN PERI-TETHYAN PANGEA TAPHONOMY OF TINY TETRAPOD TRACKS IN AN EXAMPLE FROM THE LOWER PERMIAN (CISURALIAN) SŁUPIEC FORMATION (SW POLAND) PLANT COMMUNITY CHANGE ACROSS THE PALEOCENE–EOCENE BOUNDARY IN THE GULF COASTAL PLAIN, CENTRAL TEXAS
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