z-logo
Premium
Plant Species Mediate Changes in Soil Microbial N in Response to Elevated CO 2
Author(s) -
Hungate Bruce A.,
Canadell Josep,
Chapin F. Stuart
Publication year - 1996
Publication title -
ecology
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 2.144
H-Index - 294
eISSN - 1939-9170
pISSN - 0012-9658
DOI - 10.2307/2265749
Subject(s) - nutrient , forb , grassland , cycling , nitrogen , soil water , plant species , biology , botany , ecology , chemistry , archaeology , organic chemistry , history
The effect of elevated $\mathrm{CO}_2$ on plant—microbial interactions and nitrogen (N) cycling is critical to predicting plant growth responses to elevated $\mathrm{CO}_2$, because plant growth is often N—limited. We investigated whether the effects of elevated $\mathrm{CO}_2$ on plant—microbial N dynamics differed among six annual plant species; three European grasses that have invaded California grasslands, and one grass and two forbs native to California serpentine grassland. Elevated $\mathrm{CO}_2$ altered plant N pools and $ { 15}\mathrm{NH}_4 + $ uptake, but the direction and magnitude of the changes were species dependent. The introduced grasses showed increased plant N pools and $ { 15}\mathrm{NH}_4 + $ uptake, whereas the native species showed smaller increases or even decreases in plant N pools and $ 1 5{\mathrm{NH}_4 + $ uptake. Under nutrient enrichment, soil microbial N and 1 5\mathrm{NH}_4 + $ uptake differed among soils with different plant species, but they were not affected by elevated $\mathrm{CO}_2$. At low nutrients, elevated $\mathrm{CO}_2$ altered soil microbrial N and 1 5\mathrm{NH}_4 + $ uptake, but the direction and magnitude of the changes were species dependent. The changes in soil microbial N were positively correlated with changes in the plant N pool, suggesting that there was no trade—off in N uptake between plants and microbes. The results also suggest that plant species composition will partly determine the direction of changes in soil N cycling in response to elevated $\mathrm{CO}_2$.

This content is not available in your region!

Continue researching here.

Having issues? You can contact us here
Accelerating Research

Address

John Eccles House
Robert Robinson Avenue,
Oxford Science Park, Oxford
OX4 4GP, United Kingdom