A global estimate of terrestrial net secondary production of primary consumers

被引:6
|
作者
Street, Garrett M. [1 ,2 ]
McNickle, Gordon G. [3 ,4 ]
机构
[1] Mississippi State Univ, Dept Wildlife Fisheries & Aquaculture, Box 9690, Mississippi State, MS 39762 USA
[2] Mississippi State Univ, Quantitat Ecol & Spatial Technol Lab, Mississippi State, MS 39762 USA
[3] Purdue Univ, Dept Bot & Plant Pathol, W Lafayette, IN 47907 USA
[4] Purdue Univ, Purdue Ctr Plant Biol, W Lafayette, IN 47907 USA
来源
GLOBAL ECOLOGY AND BIOGEOGRAPHY | 2019年 / 28卷 / 12期
关键词
biome; carbon; climate; metabolic theory; modelling; MODIS; net primary production; production; POPULATION-CYCLES; FORAGING TIME; BODY-SIZE; HERBIVORES; EXTINCTION; UNGULATE; TEMPERATURE; ECOSYSTEMS; EVOLUTION; COMMUNITY;
D O I
10.1111/geb.12989
中图分类号
Q14 [生态学(生物生态学)];
学科分类号
071012 ; 0713 ;
摘要
Aim Net secondary production (NSP) emerges from the consumption of net primary production (NPP) by all heterotrophic organisms. There has been sporadic interest in the importance of NSP, but no global estimates have been produced. Here, we examine NSP and attempt a global estimate using contemporary NPP data combined with modern metabolic scaling theory for consumption rates. We distinguish between potential NSP, as the amount of secondary production that could be supported by NPP, and realized NSP, as the amount remaining after anthropogenic habitat disruption. Location Global. Time period 2000-2014. Methods We present a metabolic model of NSP, implementing a type II functional response for consumption rates, wherein search efficiency and handling time are calculated based on consumer mass and ambient temperature. We solve this model for each 0.05-decimal-degree pixel in the global terrestrial biosphere, using as data inputs NPP (MOD17A3) and land-surface temperature (MOD11C3). We aggregate estimates within global land-cover classifications (MCD12C1) to obtain cover-specific and global estimates of NSP. We also correct our estimates based on declines in consumer abundance reported in Living planet report 2014. Results We estimate that potential NSP is 4.74 Pg C/year globally (95% CI: 3.75-5.75). When we correct for global consumer population declines, realized NSP is estimated at 2.37 Pg C/year (95% CI: 1.86-2.89), a loss of 50% in the rate of carbon flux through secondary consumers. Main conclusions Our estimates should not be viewed as the last word on NSP but are sufficient to suggest that the flux of carbon through consumers is of a similar magnitude to many other fluxes crucial to the global carbon cycle. We view this as a hypothesis to be tested that suggests NSP deserves significantly more attention in Earth systems, macroecology and biogeochemical research.
引用
收藏
页码:1763 / 1773
页数:11
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