Different nitrogen saturation thresholds for above‐, below‐, and total net primary productivity in a temperate steppe

Identifying the thresholds for the positive responses of total net primary productivity (NPP) to nitrogen (N) enrichment is an essential prerequisite for predicting the benefits of N deposition on ecosystem carbon sequestration. However, the responses of below‐ground NPP (BNPP) to N enrichment are u...

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Bibliographic Details
Published inGlobal change biology Vol. 29; no. 16; pp. 4586 - 4594
Main Authors Yang, Guo‐Jiao, Stevens, Carly, Zhang, Zi‐Jia, Lü, Xiao‐Tao, Han, Xing‐Guo
Format Journal Article
LanguageEnglish
Published England Blackwell Publishing Ltd 01.08.2023
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Summary:Identifying the thresholds for the positive responses of total net primary productivity (NPP) to nitrogen (N) enrichment is an essential prerequisite for predicting the benefits of N deposition on ecosystem carbon sequestration. However, the responses of below‐ground NPP (BNPP) to N enrichment are unknown in many ecosystems, which limits our ability to understand the carbon cycling under the scenario of increasing N availability. We examined the changes in above‐ground NPP (ANPP), BNPP, and NPP of a temperate meadow steppe across a wide‐ranging N addition gradient (0, 2, 5, 10, 20, and 50 g N m−2 year−1) during 5 years. Both ANPP and NPP increased nonlinearly with N addition rates. The N saturation threshold for ANPP (TA) and NPP (TN) was at the rate of 13.11 and 6.70 g N m−2 year−1, respectively. BNPP decreased with increasing N addition when N addition rates ˃5 g N m−2 year−1, resulting in much lower TN than TA. Soil N enrichment played a key role in driving the negative impacts of high N addition rates on BNPP, and consequently on the earlier occurrence of N saturation threshold for NPP. Our results highlight the negative effects of soil N enrichment on NPP in natural grasslands super‐saturated with N. Furthermore, by considering ANPP and BNPP simultaneously, our results indicate that previous findings from above‐ground might have over‐estimated the positive effects of N deposition on primary productivity. Based on a field experiment with six nitrogen (N) addition rates in a temperate steppe, we found that the N saturation threshold for ANPP (TA) and NPP (TN) was 13.11 and 6.70 g N m−2 year−1, respectively. Soil N enrichment played a key role in driving the negative impacts of high N addition rates on BNPP, resulting in much lower TN than TA. Our results indicate that previous findings from above‐ground might have over‐estimated the positive effects of N deposition on primary productivity.
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ISSN:1354-1013
1365-2486
DOI:10.1111/gcb.16803