《自然地球科学》的研究显示，由于气候变暖，热喀斯特地区土壤二氧化碳排放量比非热喀斯特地区增加了 5.5 倍。 Study in Nature Geoscience reveals thermokarst regions' soil CO2 emissions increase 5.5 times more than non-thermokarst areas due to climate warming.

《自然地球科学》的一项研究表明，永久冻土塌陷区或热喀斯特地区的土壤二氧化碳（CO2）排放对气候变暖的敏感度比非塌陷区更高。 A study in Nature Geoscience shows soil carbon dioxide (CO2) emissions in permafrost-collapsed areas, or thermokarst, are more sensitive to climate warming than in non-collapsed areas. 由于土壤质量较差，以及与有机碳分解相关的微生物基因较多，热喀斯特地区的排放量比非热喀斯特地区增加了5.5倍。 Emissions from thermokarst regions increase 5.5 times more than non-thermokarst areas due to lower soil quality and higher microbial genes related to organic carbon decomposition. 这种增强的敏感性可能会显著增加土壤二氧化碳排放量并加剧气候变化的影响。 This heightened sensitivity could significantly increase soil CO2 emissions and exacerbate climate change effects.