Response of Boreal Plant Communities and Forest Floor Carbon Fluxes to Experimental Nutrient Additions
High-latitude warming is increasing soil temperatures and driving permafrost thaw, potentially altering soil nutrient conditions by enhancing microbial mineralization and making nutrients from previously frozen soils accessible for plant and microbial use. Increases in soil nutrient concentrations m...
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Published in | Ecosystems (New York) Vol. 27; no. 3; pp. 462 - 478 |
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Main Authors | , , , , |
Format | Journal Article |
Language | English |
Published |
New York
Springer US
01.04.2024
Springer Springer Nature B.V |
Subjects | |
Online Access | Get full text |
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