Carbon and phosphorus exchange rates in arbuscular mycorrhizas depend on environmental context and differ among co‐occurring plants

Author:

Lekberg Ylva12ORCID,Jansa Jan3ORCID,McLeod Morgan1ORCID,DuPre Mary Ellyn1ORCID,Holben William E.4ORCID,Johnson David5ORCID,Koide Roger T.6ORCID,Shaw Alanna2ORCID,Zabinski Catherine7ORCID,Aldrich‐Wolfe Laura8ORCID

Affiliation:

1. MPG Ranch Missoula MT 59801 USA

2. Department of Ecosystem and Conservation Sciences, W.A. Franke College of Forestry and Conservation University of Montana Missoula MT 59812 USA

3. Institute of Microbiology of the Czech Academy of Sciences Prague 14220 Czech Republic

4. Cellular, Molecular and Microbial Biology University of Montana Missoula MT 59812 USA

5. Department of Earth and Environmental Sciences University of Manchester Manchester M13 9PT UK

6. Department of Biology Brigham Young University Provo UT 84602 USA

7. Department of Land Resources and Environmental Sciences Montana State University Bozeman MT 59717 USA

8. Department of Biological Sciences North Dakota State University Fargo ND 58108 USA

Abstract

Summary Phosphorus (P) for carbon (C) exchange is the pivotal function of arbuscular mycorrhiza (AM), but how this exchange varies with soil P availability and among co‐occurring plants in complex communities is still largely unknown. We collected intact plant communities in two regions differing c. 10‐fold in labile inorganic P. After a 2‐month glasshouse incubation, we measured 32P transfer from AM fungi (AMF) to shoots and 13C transfer from shoots to AMF using an AMF‐specific fatty acid. AMF communities were assessed using molecular methods. AMF delivered a larger proportion of total shoot P in communities from high‐P soils despite similar 13C allocation to AMF in roots and soil. Within communities, 13C concentration in AMF was consistently higher in grass than in blanketflower (Gaillardia aristata Pursh) roots, that is P appeared more costly for grasses. This coincided with differences in AMF taxa composition and a trend of more vesicles (storage structures) but fewer arbuscules (exchange structures) in grass roots. Additionally, 32P‐for‐13C exchange ratios increased with soil P for blanketflower but not grasses. Contrary to predictions, AMF transferred proportionally more P to plants in communities from high‐P soils. However, the 32P‐for‐13C exchange differed among co‐occurring plants, suggesting differential regulation of the AM symbiosis.

Publisher

Wiley

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