2011
DOI: 10.1080/11263504.2011.633113
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High spots for diversity of soil and litter microfungi in Italy

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Cited by 16 publications
(3 citation statements)
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“…The first mycological investigations of soil in the north‐west Alps were reported in 1957, 1960, and 1974 . Subsequently, data are rare and scattered, with the most recent being on the microfungi living in soil hummocks in the Italian Rhaetian Alps . In the Lombardy region of the Italian Alps, where the present study was conducted, there is clear evidence that glaciers have retreated due to transient climate change and, during the latest glaciological campaign (2008–2009), this phenomenon was observed in 41 out of the 54 monitored sites .…”
Section: Introductionmentioning
confidence: 85%
“…The first mycological investigations of soil in the north‐west Alps were reported in 1957, 1960, and 1974 . Subsequently, data are rare and scattered, with the most recent being on the microfungi living in soil hummocks in the Italian Rhaetian Alps . In the Lombardy region of the Italian Alps, where the present study was conducted, there is clear evidence that glaciers have retreated due to transient climate change and, during the latest glaciological campaign (2008–2009), this phenomenon was observed in 41 out of the 54 monitored sites .…”
Section: Introductionmentioning
confidence: 85%
“…Complexes of bacteria, fungi (including saprobic micro fungi) and soil fauna play an important role in decomposing leaf litter (Persiani et al 2011). For the recycling of nutrients, the decomposition of living and logged trees along with fallen litter is critical and is primarily carried out by fungi, especially the members of basidiomycetes (Saitta et al 2011).…”
Section: Introductionmentioning
confidence: 99%
“…Arctic areas and glaciers of high-mountain complexes, such as Himalaya, Alps and Andes are glacial areas which also represent rich sources of psychrophiles and psychrotolerants (Thomas-Hall et al 2010;Turchetti et al 2011). The viability of microorganisms in cold environments has been the focus of interest for many years, and glacial ice is an excellent preservation matrix for microbial life (Newsham 2012); the longevity of microorganisms entrapped in ice (including those from alpine environments) has consequently become a subject of study (Catranis & Starmer 1991;Abyzov 1993;Persiani et al 2011;among others). Physiological mechanisms conferring cold tolerance on fungi are complex and not yet fully understood; they include increases in unsaturated membrane lipids (Russell 2008), the production of RNA chaperones to suppress the formation of undesired secondary RNA structures (Kwak et al 2011), the synthesis of antifreeze (García-Arribas et al 2007) and cold shock proteins (Horn et al 2007), as well as cold-active enzymes (Gatti-Lafranconi et al 2010).…”
Section: Introductionmentioning
confidence: 99%