| Literature DB >> 28356409 |
Kristy J Kroeker1, Rebecca L Kordas2, Christopher D G Harley3.
Abstract
Changes in the Earth's environment are now sufficiently complex that our ability to forecast the emergent ecological consequences of ocean acidification (OA) is limited. Such projections are challenging because the effects of OA may be enhanced, reduced or even reversed by other environmental stressors or interactions among species. Despite an increasing emphasis on multifactor and multispecies studies in global change biology, our ability to forecast outcomes at higher levels of organization remains low. Much of our failure lies in a poor mechanistic understanding of nonlinear responses, a lack of specificity regarding the levels of organization at which interactions can arise, and an incomplete appreciation for linkages across these levels. To move forward, we need to fully embrace interactions. Mechanistic studies on physiological processes and individual performance in response to OA must be complemented by work on population and community dynamics. We must also increase our understanding of how linkages and feedback among multiple environmental stressors and levels of organization can generate nonlinear responses to OA. This will not be a simple undertaking, but advances are of the utmost importance as we attempt to mitigate the effects of ongoing global change.Entities:
Keywords: climate change; cumulative impacts; ocean acidification; thresholds
Mesh:
Substances:
Year: 2017 PMID: 28356409 PMCID: PMC5377028 DOI: 10.1098/rsbl.2016.0802
Source DB: PubMed Journal: Biol Lett ISSN: 1744-9561 Impact factor: 3.703
Figure 1.Conceptual figure highlighting how non-additive effects of environmental change drivers can arise within an organism, population or community despite a lack of non-additivity at lower levels of organization. For a single species exposed to two drivers (e.g. warming × high CO2 or low O2), the coloured symbols represent (a) changes in individual-level performance (circles), (b) intraspecific population responses at a static point in time (bars), (c) intraspecific population growth trajectories (lines) based on the scenarios presented in panel (b), and (d) alterations to one such set of growth trajectories (panel c, centre) when influenced by negative (left) or positive species interactions (right). For all graphs, blue represents the current ‘control’ conditions, green represents acidification (or low oxygen), orange represents warming, and red represents the simultaneous application of both stressors. The dotted line in panel (b) represents zero population growth (λ = 1). In these examples, a change in thermal performance with exposure to low oxygen or high CO2 can create antagonistic, additive or synergistic effects [12] (a). Species physiological responses can result in population persistence or extinction if growth rates are pushed past a demographic threshold (b,c). Interactions among species can also push populations past demographic thresholds (d), as when negative species interactions reduce population growth rates (shifting the orange trajectory from growth (in panel (c), centre) to decline (in panel (d), left)) or when positive interactions enhance population growth rates (shifting the green trajectory from decline (in panel (c), centre) to growth (in panel (d), right)). In such cases, indirect effects can override the direct effects at lower levels of organization.