Past rapid spread of introduced livestock coincided with vegetation clearance on Madagascar
Abstract
Abstract Debates persist around the past and present effects of introduced livestock on the native biodiversity of Madagascar. Indeed, the variable habitat and past rate of spread of livestock across the island’s distinct ecoregions are poorly known. Sets of 14C and stable isotope data from bovid bone collagen give a direct approach to estimating past introduction events and animal diet. We sampled more than 100 bovid bones collected at 23 sites across the island and present a compiled dataset of stable carbon and nitrogen isotope data from 126 specimens (94 of which are directly 14C-dated) belonging to Bos (cattle), Ovis (sheep) and Capra (goat). The earliest documented presence of bovids in the island's interior approximately 1200 years ago probably reflects a rapid spread of livestock across the island before the start of the past millennium. Isotopic data suggest that, since cattle introduction, these livestock have come to rely more on plants in increasingly wet habitat and approximately 10% more on carbon from some combination of C4 grasses or succulents that use crassulacean acid metabolism (CAM). We argue that a potential variety of causal mechanisms connect past changes in livestock diet with changes in climate, vegetation and endemic large herbivore abundance, and we highlight productive areas for future research.
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Authors: Sean Hixon, Leanne Phelps, Lucien Rakotozafy, Zoë Crossland, Mary E. Prendergast, Chantal Radimilahy, Henry Wright, Noel Amano, Nicole Boivin, Alison Crowther, Kristina Douglass, Andrius Garbaras, Richard J. George, Sophia W. Hüsges, Anneke Janzen, Douglas J. Kennett, Heritiana Randrianatoandro, Stefanie Schirmer, Axel Steinhof, Ricardo Fernandes
Institutions: University of California, Santa Barbara, The University of Queensland, Columbia University, University of Antananarivo, University of Michigan, University of Warsaw, Oregon State University, University of Tennessee at Knoxville, Knoxville College, Griffith University, Pennsylvania State University, Princeton University, Rice University, Climate Central, Center for Physical Sciences and Technology, Department of Archaeology, Santa Fe Institute, Max Planck Institute for Biogeochemistry, Max Planck Institute for the Science of Human History