Abstract

Most evidence of climate change impacts on food webs comes from modern studies and little is known about how ancient food webs have responded to climate changes in the past. Here, we integrate fossil evidence from 71 fossil sites, body-size relationships and actualism to reconstruct food webs for six large mammal communities that inhabited the Iberian Peninsula at different times during the Quaternary. We quantify the long-term dynamics of these food webs and study how their structure changed across the Quaternary, a period for which fossil data and climate changes are well known. Extinction, immigration and turnover rates were correlated with climate changes in the last 850 kyr. Yet, we find differences in the dynamics and structural properties of Pleistocene versus Holocene mammal communities that are not associated with glacial-interglacial cycles. Although all Quaternary mammal food webs were highly nested and robust to secondary extinctions, general food web properties changed in the Holocene. These results highlight the ability of communities to re-organize with the arrival of phylogenetically similar species without major structural changes, and the impact of climate change and super-generalist species (humans) on Iberian Holocene mammal communities.

Highlights

  • Climate change is one of the major drivers affecting the diversity, composition, structure and functioning of ecological communities

  • We address the following questions: (a) how have Quaternary mammal communities changed in terms of dynamics and food web structure?, and (b) are the changes in the structure and dynamics of these communities associated with Quaternary climate changes?

  • Pleistocene communities comprise 20–25 species .20 kg, a figure that falls within the range of values reported in comparative analyses of modern [49] and ancient food webs [20,21]

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Summary

Introduction

Climate change is one of the major drivers affecting the diversity, composition, structure and functioning of ecological communities. Changes in annual mean temperature inferred from oxygen isotopes range from an increase of 5uC during the warm scenarios to a decrease of 211uC in the extreme glacial periods [6]. This sequence of successive glacial and interglacial periods had direct and indirect effects on natural communities by forcing species to migrate [4], eliminating species [7], introducing new species, and shaping several broad diversity patterns that we observe today This sequence of successive glacial and interglacial periods had direct and indirect effects on natural communities by forcing species to migrate [4], eliminating species [7], introducing new species, and shaping several broad diversity patterns that we observe today (e.g. [8])

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