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The future of the northeast Atlantic benthic flora in a high CO2 world

  • Juliet Brodie*
  • , Christopher J. Williamson
  • , Dan A. Smale
  • , Nicholas A. Kamenos
  • , Nova Mieszkowska
  • , Rui Santos
  • , Michael Cunliffe
  • , Michael Steinke
  • , Christopher Yesson
  • , Kathryn M. Anderson
  • , Valentina Asnaghi
  • , Colin Brownlee
  • , Heidi L. Burdett
  • , Michael T. Burrows
  • , Sinead Collins
  • , Penelope J.C. Donohue
  • , Ben Harvey
  • , Andrew Foggo
  • , Fanny Noisette
  • , Joana Nunes
  • Federica Ragazzola, John A. Raven, Daniela N. Schmidt, David Suggett, Mirta Teichberg, Jason M. Hall-Spencer
*Corresponding author for this work
  • The Natural History Museum, London
  • Cardiff University
  • Marine Biological Association
  • University of Southampton
  • University of Glasgow
  • University of Algarve
  • University of Essex
  • Zoological Society of London Institute of Zoology
  • University of British Columbia
  • University of Genoa
  • University of St Andrews
  • Scottish Marine Institute
  • University of Edinburgh
  • Aberystwyth University
  • Sorbonne Université
  • Station Biologique de Roscoff
  • Plymouth Marine Laboratory
  • University of Bristol
  • The James Hutton Institute
  • University of Technology Sydney
  • Leibniz Center for Tropical Marine Research

Research output: Contribution to journalArticlepeer-review

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Abstract

Seaweed and seagrass communities in the northeast Atlantic have been profoundly impacted by humans, and the rate of change is accelerating rapidly due to runaway CO2 emissions and mounting pressures on coastlines associated with human population growth and increased consumption of finite resources. Here, we predict how rapid warming and acidification are likely to affect benthic flora and coastal ecosystems of the northeast Atlantic in this century, based on global evidence from the literature as interpreted by the collective knowledge of the authorship. We predict that warming will kill off kelp forests in the south and that ocean acidification will remove maerl habitat in the north. Seagrasses will proliferate, and associated epiphytes switch from calcified algae to diatoms and filamentous species. Invasive species will thrive in niches liberated by loss of native species and spread via exponential development of artificial marine structures. Combined impacts of seawater warming, ocean acidification, and increased storminess may replace structurally diverse seaweed canopies, with associated calcified and noncalcified flora, with simple habitats dominated by noncalcified, turf-forming seaweeds
Original languageEnglish
Pages (from-to)2787-2798
Number of pages0
JournalEcology and Evolution
Volume4
Issue number13
DOIs
Publication statusPublished - 18 Jun 2014

UN SDGs

This output contributes to the following UN Sustainable Development Goals (SDGs)

  1. SDG 13 - Climate Action
    SDG 13 Climate Action
  2. SDG 14 - Life Below Water
    SDG 14 Life Below Water
  3. SDG 15 - Life on Land
    SDG 15 Life on Land

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