New horizons in geomycology.
New horizons in geomycology.
复制标题
地球真菌学的新视野。
DOI:
10.1111/1758-2229.12480
复制
发表时间:
2017
影响因子:
3.3
通讯作者:
Gadd GM
中科院分区:
文献类型:
--
作者:
Gadd GM
Geomycology can be simply defined as the roles and significance of fungi in processes of relevance to geology, and as such is part of the more general area of geomicrobiology (Gadd, 2010). Rock and mineral bioweathering, metal transformations, mineral formation, and cycling of the elements, all of which are involved in mineral soil formation, are the most obvious geomicrobial processes under this heading. In the case of fungi, their additional significance as major decomposers of organic material underlines their important role in the cycling of major elements such as C, H, N, O, P, S, as well all other elements that may be associated with organic matter. The majority of stable elements can be found in living organisms, including metal pollutants, and the release of these in decomposition can result in further interaction with environmental components resulting in mineral formation for example. There are therefore clear connections between organic and inorganic components of geomicrobial processes, and between the aerobic and anaerobic domains of life. This is not always appreciated in geomicrobiology where to some the “geo” prefix is equated with chemolithotrophy and anaerobiosis in certain prokaryotes.While environmental microbiologists are generally aware of the global significance of fungi in organic matter decomposition, plant productivity, food spoilage and biodeterioration, there is rather less awareness of their significance in a geomycological context. The problem is exacerbated in geomicrobiology where the preponderant attention given to prokaryotes has lead to neglect of major eukaryotic groups such as fungi and algae. A recent example of such a narrow appreciation of microbial roles in major biosphere processes is found in a special edition of Elements dedicated to geomicrobiology where microbes were even defined as solely comprising bacteria and archaea (Druschel and Kappler, 2015), and with the entire perspective solely concentrating on these organisms. While some of this problem is undoubtedly due to the fragmentation and diversity of the different scientific communities that study prokaryotic and fungal processes, it is about time that geomycology received proper attention within geomicrobiology and Earth sciences as a vital and integral component. It is also clear that further integration is necessary between the different relevant disciplines. Geomicrobiology is by definition interdisciplinary requiring interaction between microbiologists, geologists, geochemists, mineralogists etc., yet there are still some obvious barriers that remain in some quarters. Witness the pejorative comments about Life Sciences in a section of the Elements editorial for example (“Microbiology (or biology) may not be your favourite subject. Or maybe you dreaded taking “life science” courses while at the university. Even if life science is not your preferred area of interest……”). Thankfully, there is a growing realisation in intelligent geological circles that microbes are important and this is bound to increase as knowledge and integration between disciplines develops. Another important point is that prokaryotes and eukaryotes are generally studied separately yet in the natural environment fungi rarely are found without bacteria, and vice versa in
影响因子:
3.3
作者:
P. Bonfante
通讯作者:
P. Bonfante
影响因子:
4.5
作者:
Druschel, Gregory K.;Kappler, Andreas
通讯作者:
Kappler, Andreas