Gulyás Sándor, Sümegi Pál
Department of Geology and Paleontology, University of Szeged, Szeged, Hungary.
Sci Rep. 2024 Apr 24;14(1):9419. doi: 10.1038/s41598-024-60185-5.
The thermal spring-fed Lake Pețea located in NW Romania southeast of the city of Oradea harbors a unique endemic warm water biota. It is the only location in Europe where thermal water endemic melanopsid Microcolpia parreyssii (Philippi, 1847) lived along with the highly endangered warm-water relict neritid Theodoxus prevostianus. Lake Petea's evolution was mainly controlled by major climate-driven hydrological changes also seen in regional records. The hydrological changes were mainly controlled by varying input of thermal water due to recurring increased/decreased recharge of the underground karst water system. The driving factor was warming connected to the interstadial GI 1 increasing recharge by melting of regional ice sheets in the Late Glacial. Conversely, during the Younger Dryas (H0) and the Holocene increasing/decreasing moisture availability was in control. Low stands created multiple bottlenecks reducing genetic variability seen in the appearance of extreme morphologies during next rapid climate melioration. The studied gastropods responded mostly similarly to changes controlling the availability of elements in shell construction and habitat reduction leading to changes in shape, density, size. Periods of lower lake levels and reduced warm water input are characterized by the emergence of elongated tightly coiled shells while globular, compressed loosely coiled shells develop at times of warmer water provision and increased Mg availability. In size there is a contrasting trend. Namely globose Th. prevostianus shells are larger than the elongated ones. Conversely globose, compressed Microcolpia are generally smaller than their elongated spindle-shaped counterparts. In this sense the development of dwarf morphotypes in warmer water habitats is characteristic of Lake Pețea melanopsids. This type of dwarfism i.e. the reduction of shell size is lacking though in Lake Pețea neritids. Our findings also confirm the presence of various ecophenotypes of Microcolpia in the pond degrading our endemic species Mi. parreyssii to a variety of Mi. daudebartii.
位于罗马尼亚西北部奥拉迪亚市东南部的佩泰亚温泉湖拥有独特的地方性温水生物群。它是欧洲唯一一处温水地方性软体动物微小拟黑螺(Microcolpia parreyssii,菲利普,1847年)与极度濒危的温水残遗类蜒螺普雷沃蜓螺(Theodoxus prevostianus)共同生存的地方。佩泰亚湖的演化主要受重大气候驱动的水文变化控制,这些变化在区域记录中也有体现。水文变化主要受地下岩溶水系统补给量反复增减导致的温泉水输入变化的控制。驱动因素是与间冰阶GI 1相关的变暖,在晚冰期区域冰盖融化增加了补给量。相反,在新仙女木期(H0)和全新世,水分供应的增减起了控制作用。低水位造成了多个瓶颈,减少了遗传变异性,这在接下来快速的气候改善过程中极端形态的出现中可见一斑。所研究的腹足类动物对控制壳结构中元素可用性和栖息地减少的变化反应大多相似,这些变化导致了形状、密度和大小的改变。湖泊水位较低和温水输入减少的时期,其特征是出现细长紧密盘绕的壳,而球状、压缩的松散盘绕的壳则在水温较高和镁可用性增加时形成。在大小方面存在相反的趋势。即球状的普雷沃蜓螺壳比细长的壳大。相反,球状、压缩的微小拟黑螺通常比其细长纺锤形的同类小。从这个意义上说,温水栖息地中侏儒形态型的发育是佩泰亚湖拟黑螺的特征。不过,佩泰亚湖蜒螺中不存在这种侏儒症,即壳大小的减小。我们还证实了在池塘中存在微小拟黑螺的各种生态表型,这将我们的特有物种微小拟黑螺退化到了多种道氏拟黑螺。