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Microbial colonization and its effects on mineral weathering (CCES-Big Link)
Colonization and initial soil formation after glacier retrieval in alpine regions is surprisingly fast. A key factor of the relevant weathering processes most probably arises from microbial exudates. Systematic studies will show the potential abundance of weathering-active microorganisms and the role of their exudates on mineral dissolution and nutrient mobilization. We focus on the interactions between biota and mineral surfaces and the subsequent mineral dissolution. Aims
Methods
Added valueThe resulting insights are crucial for the entire BigLink project, where weathering of bare rock material is a critical step of initial soil formation and the subsequent establishment of a new ecosystem that is able to prevent rock material from continuous erosion. This information will be fundamental for the understanding of isotope fractionation (Subproject 4) and carbon turnover (Subproject 1). Projectpartners
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