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      Paleoenvironments shaped the exchange of terrestrial vertebrates across Wallace’s Line

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          Abstract

          Faunal turnover in Indo-Australia across Wallace’s Line is one of the most recognizable patterns in biogeography and has catalyzed debate about the role of evolutionary and geoclimatic history in biotic interchanges. Here, analysis of more than 20,000 vertebrate species with a model of geoclimate and biological diversification shows that broad precipitation tolerance and dispersal ability were key for exchange across the deep-time precipitation gradient spanning the region. Sundanian (Southeast Asian) lineages evolved in a climate similar to the humid “stepping stones” of Wallacea, facilitating colonization of the Sahulian (Australian) continental shelf. By contrast, Sahulian lineages predominantly evolved in drier conditions, hampering establishment in Sunda and shaping faunal distinctiveness. We demonstrate how the history of adaptation to past environmental conditions shapes asymmetrical colonization and global biogeographic structure.

          Editor’s summary

          The movement of species across newly connected continents millions of years ago still shapes flora and fauna today. Skeels et al . showed that species’ dispersal ability, climate tolerances, and the climate in which they evolved help to explain why biotic exchanges are typically unequal, with more species spreading from one continent than the other. Using a model simulating species ranges and diversification paired with paleoenvironmental reconstructions, the authors found that precipitation tolerance influenced vertebrate species movements across Wallace’s Line, which separates the distinct biota of Australia and New Guinea from that of Southeast Asia. Species that evolved in dry Australia were less able to cross to Asia, whereas the swath of tropical forest across the region allowed more species to move in the other direction through New Guinea. —BEL

          Abstract

          Environmental adaptation and dispersal ability explain which vertebrate species spread between newly connected continents.

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          WorldClim 2: new 1-km spatial resolution climate surfaces for global land areas

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            Terrestrial Ecoregions of the World: A New Map of Life on Earth

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              Is Open Access

              Present and future Köppen-Geiger climate classification maps at 1-km resolution

              We present new global maps of the Köppen-Geiger climate classification at an unprecedented 1-km resolution for the present-day (1980–2016) and for projected future conditions (2071–2100) under climate change. The present-day map is derived from an ensemble of four high-resolution, topographically-corrected climatic maps. The future map is derived from an ensemble of 32 climate model projections (scenario RCP8.5), by superimposing the projected climate change anomaly on the baseline high-resolution climatic maps. For both time periods we calculate confidence levels from the ensemble spread, providing valuable indications of the reliability of the classifications. The new maps exhibit a higher classification accuracy and substantially more detail than previous maps, particularly in regions with sharp spatial or elevation gradients. We anticipate the new maps will be useful for numerous applications, including species and vegetation distribution modeling. The new maps including the associated confidence maps are freely available via www.gloh2o.org/koppen.
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                Author and article information

                Contributors
                Journal
                Science
                Science
                American Association for the Advancement of Science (AAAS)
                0036-8075
                1095-9203
                July 07 2023
                July 07 2023
                : 381
                : 6653
                : 86-92
                Affiliations
                [1 ]Department of Environmental Systems Science, Ecosystems and Landscape Evolution, Institute of Terrestrial Ecosystems, ETH Zurich, 8092 Zurich, Switzerland.
                [2 ]Swiss Federal Institute for Forest, Snow and Landscape Research WSL, 8903 Birmensdorf, Switzerland.
                [3 ]Research School of Biology, Australian National University, Canberra 0200, Australia.
                [4 ]Department of Earth Sciences, Utrecht University, 3584 CB Utrecht, Netherlands.
                [5 ]Institute for Biodiversity and Ecosystem Dynamics, University of Amsterdam, 1090 GE Amsterdam, Netherlands.
                [6 ]Systematics, Biodiversity and Evolution of Plants, Ludwig Maximilian University of Munich, 80331 Munich, Germany.
                [7 ]German Centre for Integrative Biodiversity Research (iDiv) Halle-Jena-Leipzig, 04103 Leipzig, Germany.
                [8 ]Institute of Biology, École Normale Supérieure, 75005 Paris, France.
                [9 ]Department of Ecology and Evolutionary Biology, Yale University, New Haven, CT 06520, USA.
                [10 ]Center for Biodiversity and Global Change, Yale University, New Haven, CT 06520, USA.
                Article
                10.1126/science.adf7122
                37410831
                17ac7961-8e9a-4bb2-a539-b29d7369f56d
                © 2023

                Free to read

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