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Societal importance of Antarctic negative feedbacks on climate change: blue carbon gains from sea ice, ice shelf and glacier losses

  • D. K.A. Barnes
    ,
  • C. J. Sands
    ,
  • M. L. Paulsen
    ,
  • ,
  • C. Moreau
    ,
  • C. Held
  • British Antarctic Survey
    ,
  • Australian Antarctic Division
    ,
  • Aarhus Universitet
    ,
  • ,
  • Universidad Científica del Sur
    ,
  • Université Libre de Bruxelles
Research Output:
Contribution to journal
Review article
Peer-review

Open access

Publication Information

Output type

Research Output:
Contribution to journal
Review article
Peer-review

Original language

English

Article number

43

Journal (Volume, Issue Number)

Science of Nature (Volume 108, Issue 5)

Publication milestones

  • Published - 10/2021

Publication status

Published - 10/2021

ISSN

0028-1042

Publication IDs

  • Scopus: 85114390821

Abstract

Diminishing prospects for environmental preservation under climate change are intensifying efforts to boost capture, storage and sequestration (long-term burial) of carbon. However, as Earth’s biological carbon sinks also shrink, remediation has become a key part of the narrative for terrestrial ecosystems. In contrast, blue carbon on polar continental shelves have stronger pathways to sequestration and have increased with climate-forced marine ice losses—becoming the largest known natural negative feedback on climate change. Here we explore the size and complex dynamics of blue carbon gains with spatiotemporal changes in sea ice (60–100 MtCyear−1), ice shelves (4–40 MtCyear−1 = giant iceberg generation) and glacier retreat (< 1 MtCyear−1). Estimates suggest that, amongst these, reduced duration of seasonal sea ice is most important. Decreasing sea ice extent drives longer (not necessarily larger biomass) smaller cell-sized phytoplankton blooms, increasing growth of many primary consumers and benthic carbon storage—where sequestration chances are maximal. However, sea ice losses also create positive feedbacks in shallow waters through increased iceberg movement and scouring of benthos. Unlike loss of sea ice, which enhances existing sinks, ice shelf losses generate brand new carbon sinks both where giant icebergs were, and in their wake. These also generate small positive feedbacks from scouring, minimised by repeat scouring at biodiversity hotspots. Blue carbon change from glacier retreat has been least well quantified, and although emerging fjords are small areas, they have high storage-sequestration conversion efficiencies, whilst blue carbon in polar waters faces many diverse and complex stressors. The identity of these are known (e.g. fishing, warming, ocean acidification, non-indigenous species and plastic pollution) but not their magnitude of impact. In order to mediate multiple stressors, research should focus on wider verification of blue carbon gains, projecting future change, and the broader environmental and economic benefits to safeguard blue carbon ecosystems through law.

Funding Details

FundersFunding numbers
H2020
800371

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Sustainable Development Goals

  • SDG 13 - Climate Action
    SDG 13 Climate Action
  • SDG 14 - Life Below Water
    SDG 14 Life Below Water
  • SDG 15 - Life on Land
    SDG 15 Life on Land