| Literature DB >> 26140205 |
Santiago R Ramírez1, Carlos Hernández2, Andres Link3, Margarita M López-Uribe4.
Abstract
Neotropical rainforests sustain some of the most diverse terrestrial communities on Earth. Euglossine (or orchid) bees are a diverse lineage of insect pollinators distributed throughout the American tropics, where they provide pollination services to a staggering diversity of flowering plant taxa. Elucidating the seasonal patterns of phylogenetic assembly and functional trait diversity of bee communities can shed new light into the mechanisms that govern the assembly of bee pollinator communities and the potential effects of declining bee populations. Male euglossine bees collect, store, and accumulate odoriferous compounds (perfumes) to subsequently use during courtship display. Thus, synthetic chemical baits can be used to attract and monitor euglossine bee populations. We conducted monthly censuses of orchid bees in three sites in the Magdalena valley of Colombia - a region where Central and South American biotas converge - to investigate the structure, diversity, and assembly of euglossine bee communities through time in relation to seasonal climatic cycles. In particular, we tested the hypothesis that phylogenetic community structure and functional trait diversity changed in response to seasonal rainfall fluctuations. All communities exhibited strong to moderate phylogenetic clustering throughout the year, with few pronounced bursts of phylogenetic overdispersion that coincided with the transition from wet-to-dry seasons. Despite the heterogeneous distribution of functional traits (e.g., body size, body mass, and proboscis length) and the observed seasonal fluctuations in phylogenetic diversity, we found that functional trait diversity, evenness, and divergence remained constant during all seasons in all communities. However, similar to the pattern observed with phylogenetic diversity, functional trait richness fluctuated markedly with rainfall in all sites. These results emphasize the importance of considering seasonal fluctuations in community assembly and provide a glimpse to the potential effects that climatic alterations may have on both pollinator communities and the ecosystem services they provide.Entities:
Keywords: Biodiversity patterns; euglossini; orchid bees; pollinators
Year: 2015 PMID: 26140205 PMCID: PMC4485970 DOI: 10.1002/ece3.1466
Source DB: PubMed Journal: Ecol Evol ISSN: 2045-7758 Impact factor: 2.912
Figure 1Geographic location of the three sampling locations in the Magdalena valley between the Eastern and Central Cordilleras of Colombia.
Figure 2Nonmetric Multidimensional scaling (nMDS) plot demonstrating composition differences between three communities of euglossine bees sampled monthly (Guinea = guin; Rio Claro = rc; Reserva = res).
Figure 3Total raw abundance values (top panel), species richness (middle panel), and diversity (bottom panel) of euglossine bees in three communities in the Magdalena Valley over the course of 11 months of sampling.
Similarity percentage (SIMPER) analysis indicating the relative contribution and cumulative contribution species abundances to the differences between communities
| Community pairwise comparison | Species | Relative contribution (%) | Cumulative sum (%) |
|---|---|---|---|
| Reserva – Guinea | 5.66 | 11.16 | |
| 4.1 | 19.26 | ||
| 3.4 | 26.02 | ||
| 3.2 | 32.52 | ||
| 3.16 | 38.76 | ||
| 3.14 | 44.97 | ||
| 2.96 | 50.81 | ||
| Reserva – Rio Claro | 10.71 | 18.39 | |
| 4.64 | 26.36 | ||
| 4.53 | 34.15 | ||
| 4.19 | 41.36 | ||
| 3.54 | 47.45 | ||
| 2.61 | 51.94 | ||
| Guinea – Rio Claro | 13.1 | 21.95 | |
| 5.21 | 30.68 | ||
| 4.59 | 38.38 | ||
| 3.7 | 44.59 | ||
| 3.7 | 50.8 |
Figure 4Estimated standardized phylogenetic diversity (SES-MPD) in three communities of euglossine bees in the Magdalena Valley, Colombia, over the course of 1 year. Average monthly rainfall patterns are superimposed for comparison (dotted line).
Figure 5Linear regression models between standardized phylogenetic diversity and the rainfall differential (D). D is calculated as abs (Rt − Rt + 1), where Rt is the average rainfall at time interval t. Linear regressions were positive and significant for Guinea (P = 0.05) and Rio Claro (P = 0.038), but not for Reserva (P = 0.47).