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洞穴温度变化及其对地下生态系统的意义。

Temperature variation in caves and its significance for subterranean ecosystems.

机构信息

Departamento de Biologia Animal, and Centre for Ecology, Evolution and Environmental Changes (cE3c) & CHANGE-Institute for Global Change and Sustainability, Faculdade de Ciências, Universidade de Lisboa, Campo Grande, 1749-016, Lisbon, Portugal.

Faculty of Biology, Institute of Zoology, University of Belgrade, Studentski Trg 16, 11 000, Belgrade, Serbia.

出版信息

Sci Rep. 2023 Nov 25;13(1):20735. doi: 10.1038/s41598-023-48014-7.

Abstract

Climate change affects all ecosystems, but subterranean ecosystems are repeatedly neglected from political and public agendas. Cave habitats are home to unknown and endangered species, with low trait variability and intrinsic vulnerability to recover from human-induced disturbances. We studied the annual variability and cyclicity of temperatures in caves vis-à-vis surface in different climatic areas. We hypothesize that cave temperatures follow the average temperature pattern at the surface for each location with a slight delay in the signal, but we found three different thermal patterns occurring in caves: (1) high positive correlation and a similar thermal pattern to the surface, (2) low correlation and a slight thermal delay of the signal from the surface, and (3) high negative correlation with an extreme delay from the surface. We found daily thermal cycles in some caves, which may potentially control the circadian rhythms of cave organisms. Our results show that caves had lower thermal amplitude than the surface, and that thermal averages within caves approximately correspond to the to the annual average of surface temperature. Caves buffer external temperature and act as refugia for biota in extreme climatic events. Likewise, temperature increases at surface will lead to increment in caves, threatening subterranean biota and ecosystem services.

摘要

气候变化影响着所有的生态系统,但地下生态系统却一再被政治和公众议程所忽视。洞穴生境是未知和濒危物种的家园,它们的特征变异率低,内在脆弱性使其难以从人类引起的干扰中恢复。我们研究了不同气候区洞穴与地表温度的年际变化和周期性。我们假设洞穴温度会随当地地表温度的平均模式而变化,只是信号会稍有延迟,但我们发现洞穴中存在三种不同的热模式:(1)与地表呈高度正相关且热模式相似;(2)与地表相关性低且信号稍有延迟;(3)与地表呈高度负相关且信号延迟极大。我们在一些洞穴中发现了每日的热循环,这可能会控制洞穴生物的昼夜节律。我们的结果表明,洞穴的温度振幅比地表低,洞穴内的温度平均值大致与地表温度的年平均值相对应。洞穴可以缓冲外部温度,为生物群落在极端气候事件中提供避难所。同样,地表温度的升高也会导致洞穴温度升高,从而威胁地下生物群和生态系统服务。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/9b86/10676404/0fcbcf9ff626/41598_2023_48014_Fig1_HTML.jpg

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