Blue carbon gains from glacial retreat along Antarctic fjords: what should we expect?

Allbwn ymchwil: Cyfraniad at gyfnodolynErthygladolygiad gan gymheiriaid

Fersiynau electronig

Dogfennau

Dangosydd eitem ddigidol (DOI)

  • David Barnes
    British Antarctic Survey, Natural Environment Research Council (NERC)
  • Chester Sands
    British Antarctic Survey, Natural Environment Research Council (NERC)
  • Alison Cook
    Durham University
  • Floyd Howard
  • Alejandro Román González
    College of Life and Environmental Sciences, University of Exeter, Penryn Campus, Penryn, 9 TR10 9EZ, UK.
  • Carlos Muñoz-Ramirez
    Universidad Católica de la Santísima Concepción
  • Kate Retallick
  • James Scourse
    College of Life and Environmental Sciences, University of Exeter, Penryn Campus, Penryn, 9 TR10 9EZ, UK.
  • Katrien Van Landeghem
  • Nadescha Zwerschke
    British Antarctic Survey, Natural Environment Research Council (NERC)

Rising atmospheric CO 2 is intensifying climate change but it is also driving global and particularly polar greening. However, most blue carbon sinks (that held by marine organisms) are shrinking, which is important as these are hotspots of genuine carbon sequestration. Polar blue carbon increases with losses of marine ice over high latitude continental shelf areas. Marine ice (sea ice, ice shelf and glacier retreat) losses generate a valuable negative feedback on climate change. Blue carbon change with sea ice and ice shelf losses has been estimated, but not how blue carbon responds to glacier retreat along fjords. We derive a testable estimate of glacier retreat driven blue carbon gains by investigating three fjords in the West Antarctic Peninsula (WAP). We started by multiplying ~40 year mean glacier retreat rates by the number of retreating WAP fjords and their time of exposure. We multiplied this area by regional zoobenthic carbon means from existing datasets to suggest that WAP fjords generate 3,130 tonnes of new zoobenthic carbon per year (t zC/year) and sequester >780 t zC/year. We tested this by capture and analysis of 204 high resolution seabed images along emerging WAP fjords. Biota within these images were identified to density per 13 functional groups. Mean stored carbon per individual was assigned from literature values to give a stored zoobenthic Carbon per area, which was multiplied up by area of fjord exposed over time, which increased the estimate to 4,536 t zC/year. The purpose of this study was to establish a testable estimate of blue carbon change caused by glacier retreat along Antarctic fjords and thus to establish its relative importance compared to polar and other carbon sinks.

Allweddeiriau

Iaith wreiddiolSaesneg
Tudalennau (o-i)2750-2755
Nifer y tudalennau6
CyfnodolynGlobal Change Biology
Cyfrol26
Rhif y cyfnodolyn5
Dyddiad ar-lein cynnar23 Maw 2020
Dynodwyr Gwrthrych Digidol (DOIs)
StatwsCyhoeddwyd - Mai 2020

Cyfanswm lawlrlwytho

Nid oes data ar gael
Gweld graff cysylltiadau