Multiple Dimensions of Climate Change and Their Implications for Biodiversity

By R. A. Garcia, M. Cabeza, C. Rahbek, Miguel B. Araújo. Science, 2014

712 citations recorded by the source corpus.

Subfields: Ecological Modeling, Ecology, Evolution, Behavior and Systematics, Nature and Landscape Conservation

View Paper: https://www.semanticscholar.org/paper/bcc060582d0a86730257d2d3d8a3cc62e7d76753

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Citations in the corpus

Climate change, species range shifts and dispersal corridors: an evaluation of spatial conservation models (2016, background): “Climate change poses major challenges to conservation plan- ning because species distributions are affected in complex and seemingly idiosyncratic ways (Thomas et al. 2004; Hof et al. 2011; Garcia et al. 2014).”
Protected areas network is not adequate to protect a critically endangered East Africa Chelonian: Modelling distribution of pancake tortoise, Malacochersus tornieri under current and future climates (2020, positive): “As MaxEnt is used to address increasingly complex problems (and not simple exploratory analyses), it is important to ensure that modeling decisions are biologically motivated by specific hypotheses, study goals, and species-specific considerations and reflect the intended a priori assumptions (Peter”
Massive Mortality of a Planktivorous Seabird in Response to a Marine Heatwave (2018, background): “Although many studies have focused on the long-term ecological implications of climate change (Bellard et al., 2012; Garcia et al., 2014), our understanding of extreme temperature events and their impact on ecosystems is less well understood (Wernberg et al., 2012).”
Modeling Species and Community Responses to Past, Present, and Future Episodes of Climatic and Ecological Change (2015, background): “F or p er so na l u se o nl y. ES46CH16-Blois ARI 4 November 2015 8:32 Williams et al. 2007, Garcia et al. 2014) and, when coupled with land-use change and other human impacts such as invasive species, are likely to lead to even more no-analog communities (Lugo 2009, Ordonez et al. 2014).”
The macroecology of animal versus wind pollination: ecological factors are more important than historical climate stability (2016, positive): “As different climate change metrics may capture different effects of climate change (Garcia et al. 2014), we considered two measures of historical climate stability: (1) the velocity of mean annual temperature (MAT velocity) and that of mean annual precipitation (MAP velocity) between the Last…”
Climate change vulnerability assessment of species (2018, background): “…approaches may include the outputs of correlative and mechanistic approaches (e.g., Küster, Bierman, Klotz, & Kühn, 2011; Pompe, Hanspach, & Badeck, 2014; Young et al., 2012) or be included in other approaches (e.g., Garcia et al., 2014); we discuss these further under the ‘ combined approach ’ .”
Vulnerability of global biodiversity hotspots to climate change (2021, background): “Additionally, the appearance of novel climates and the disappearance of existing ones is projected primarily in the tropics and subtropics, where many of the biodiversity hotspots of the world are located (Garcia et al., 2014; Williams et al., 2007).”
Origins of global mountain plant biodiversity: Testing the ‘mountain‐geobiodiversity hypothesis’ (2019, neutral): “…need to shift the geo‐ graphical range) due to climatic fluctuations potentially results in higher rates of local extirpation and/or extinction (Garcia, Cabeza, Rahbek, & Araújo, 2014), especially in species with narrow climatic (and geographic) ranges, leading to an overall reduced species…”
Connectivity for species on the move: supporting climate‐driven range shifts (2019, background): “Capturing the variations inherent in climate change remains a major challenge for connectivity modeling and for ecological response modeling in general (Garcia et al. 2014; van de Pol et al. 2017).”
Biodiversity redistribution under climate change: Impacts on ecosystems and human well-being (2017, neutral): “However, future projections in the tropics are uncertain because of a lack of close climatic analogs from which to extrapolate (71).”