| Literature DB >> 29321850 |
Chenxia Liang1, Gang Feng1, Xingfeng Si2,3, Lingfeng Mao4, Guisheng Yang5, Jens-Christian Svenning6, Jie Yang1.
Abstract
Bird species richness is mediated by local, regional, and historical factors, for example, competition, environmental heterogeneity, contemporary, and historical climate. Here, we related bird species richness with phylogenetic relatedness of bird assemblages, plant species richness, topography, contemporary climate, and glacial-interglacial climate change to investigate the relative importance of these factors. This study was conducted in Inner Mongolia, an arid and semiarid region with diverse vegetation types and strong species richness gradients. The following associated variables were included as follows: phylogenetic relatedness of bird assemblages (Net Relatedness Index, NRI), plant species richness, altitudinal range, contemporary climate (mean annual temperature and precipitation, MAT and MAP), and contemporary-Last Glacial Maximum (LGM) change in climate (change in MAT and change in MAP). Ordinary least squares linear, simultaneous autoregressive linear, and Random Forest models were used to assess the associations between these variables and bird species richness across this region. We found that bird species richness was correlated negatively with NRI and positively with plant species richness and altitudinal range, with no significant correlations with contemporary climate and glacial-interglacial climate change. The six best combinations of variables ranked by Random Forest models consistently included NRI, plant species richness, and contemporary-LGM change in MAT. Our results suggest important roles of local ecological factors in shaping the distribution of bird species richness across this semiarid region. Our findings highlight the potential importance of these local ecological factors, for example, environmental heterogeneity, habitat filtering, and biotic interactions, in biodiversity maintenance.Entities:
Keywords: biotic interaction; bird species richness; contemporary climate; environmental heterogeneity; glacial–interglacial climate change
Year: 2017 PMID: 29321850 PMCID: PMC5756892 DOI: 10.1002/ece3.3606
Source DB: PubMed Journal: Ecol Evol ISSN: 2045-7758 Impact factor: 2.912
Results of single‐variable analysis by ordinary least squares (OLS) and simultaneous autoregressive (SAR) models. MAT and MAP are mean annual temperature and precipitation. ChangeMAT and ChangeMAP are the contemporary‐Last Glacial Maximum change in MAT and MAP. SRplant is species richness of plants. ALTrange is altitudinal range. NRI is phylogenetic relatedness of bird assemblages. Coefficients (coef) and adjusted r 2 were given. All statistically significant p‐values were less than .01 and are indicated as *
| CoefOLS |
| CoefSAR |
| |
|---|---|---|---|---|
| Area | 0.06 | −.01 | 0.09 | .08 |
| MAT | −0.05 | −.01 | 0.02 | .08 |
| MAP | 0.08 | −.01 | 0.07 | .08 |
| ChangeMAT | −0.18 | .02 | −0.22 | .10 |
| ChangeMAP | 0.20 | .03 | 0.17 | .09 |
| SRplant | 0.52 | .26* | 0.49 | .30* |
| ALTrange | 0.37 | .13* | 0.34 | .17* |
| NRI | −0.68 | .45* | −0.67 | .48* |
Figure 1Relationships between bird species richness (log transformed) and the three most associated variables: phylogenetic relatedness of bird assemblages (Net Relatedness Index, NRI), plant species richness (SR plant, log transformed), and altitudinal range (ALT range). Single‐variable OLS linear fits (standardized) are shown, and their r 2 is given. All statistically significant p‐values were less than .01 and are indicated as *
The six combinations of variables most associated with bird species richness, ranked by the correlations between observed and predicted species richness, from the Random Forest models (CorRF). Each column is a different variable (NRI, phylogenetic relatedness of bird assemblages; ChangeMAT, contemporary‐Last Glacial Maximum change in temperature; SRplant, species richness of plant; MAP, mean annual precipitation; ALTrange, altitudinal range; MAT, mean annual temperature; ChangeMAP, contemporary‐Last Glacial Maximum change in precipitation). White cell indicates that the variable was not included in the particular combination (each row). AIC weights (AICw) and adjusted r 2 from simultaneous autoregressive (SAR) models of each combination of variables were also listed
| NRI | ChangeMAT | SRplant | ALTrange | MAP | MAT | ChangeMAP | CorRF | AICw_SAR |
|
|---|---|---|---|---|---|---|---|---|---|
| 0.620 | 0.100 | .544 | |||||||
| 0.614 | 0.049 | .547 | |||||||
| 0.610 | 0.074 | .551 | |||||||
| 0.605 | 0.049 | .557 | |||||||
| 0.604 | 0.045 | .546 | |||||||
| 0.604 | 0.020 | .548 |