degradation at the land ocean interface
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Permafrost carbon release and degradation at the land-ocean interface George Tanski, Michael Fritz, Justine Ramage, Christian Knoblauch, Nicole Couture, and Hugues Lantuit Herschel Island, Yukon, Canada Background of northern landmass of


  1. Permafrost carbon release and degradation at the land-ocean interface George Tanski, Michael Fritz, Justine Ramage, Christian Knoblauch, Nicole Couture, and Hugues Lantuit Herschel Island, Yukon, Canada

  2. Background of northern landmass of global coasts km of coastline (Gt C org. ) Global carbon storage in soils TARNOCAI et al. 2009 George Tanski 1

  3. Background of the coast are unlithified Erosion rates up to Herschel Island, Yukon Coast, Canada George Tanski 2

  4. Background of the coast are unlithified Erosion rates up to Komakuk Beach, Yukon Coast, Canada George Tanski 3

  5. Background of the coast are unlithified Erosion rates up to Herschel Island, Yukon, Canada Photo: J. WOLTER George Tanski 4

  6. Topic I release... Dissolved organic carbon (DOC) OC ≤ 0.45 µm Particulate organic carbon (POC) Sediments George Tanski 5

  7. Topic I: Release of DOC from ground ice Herschel Island Roland Bay Canada Study sites Kay Point Beaufort Sea (Arctic Ocean) Unglaciated Glaciated George Tanski 6

  8. Topic I: Release of DOC from ground ice River discharge ** DOC: 1.3 Gg yr -1 POC: 2.1 Gg yr -1 Sediment: 127.0 Gg yr -1 Coastal erosion * DOC: ? SOC: 0.04 Gg yr -1 Sediment: 2.66 Gg yr -1 * MACDONALD et al. 1998 1 Gg = 10 12 g = 10 9 kg = 10 6 t ** COUTURE 2010 George Tanski 7

  9. Topic I: Release of DOC from ground ice Ground ice content and types along the Yukon Coastal Plain • 37% ground ice C: 26% A+B: 11% After COUTURE 2010 A) Ice wedges B) Massive ice beds C) Pore/Non-massive intrasedimental ice George Tanski 8

  10. Topic I: Release of DOC from ground ice Ground ice content and types along the Yukon Coastal Plain • 37% ground ice C: 26% A+B: 11% After COUTURE 2010 A) Ice wedges B) Massive ice beds A) B) C) C) Pore/Non-massive intrasedimental ice George Tanski 9

  11. Topic I: Release of DOC from ground ice Calculation of DOC flux • n DOC storage = θj ∗ ρ ∗ DOCconc.j j=1 n DOC flux = lj ∗ hj ∗ Rj ∗ DOC storage j j=1 Modified, after COUTURE 2010 George Tanski 10

  12. Topic I: Release of DOC from ground ice River discharge * DOC: 1.3 Gg yr -1 POC: 2.1 Gg yr -1 Sediment: 127.0 Gg yr -1 Coastal erosion ** DOC: 0.09 -3 Gg yr -1 SOC: 0.04 Gg yr -1 Sediment: 2.66 Gg yr -1 * MACDONALD et al. 1998 1 Gg = 10 12 g = 10 9 kg = 10 6 t ** COUTURE 2010 George Tanski 11

  13. Topic I: Conclusion Low dissolved organic carbon fluxes from eroding permafrost coasts • Western part and Herschel Island are hotspots • Mostly fluxes from ice thrust moraine ridges and lacustrine deposits • Mostly as POC  DOC/POC ratio of ~1:1000 • OC input from the Mackenzie dominates the Beaufort Sea • But: High bioavailabilty of DOC assumed • Recent studies show high bioavailabilty • e.g. VONK et al. 2013  DOC loss > 34.0 ± 0.8% within two weeks • e.g. HOOD et al. 2009  45% of DOC terr. bioavailable • George Tanski 12

  14. Topic II release... Dissolved organic carbon (DOC) OC ≤ 0.45 µm Particulate organic carbon (POC) Nutrients (NH 4 , NO 2 , NO 3 ) Sediments George Tanski 13

  15. Topic II: Degradation of organic matter Herschel Island Slump D Canada Study site Beaufort Sea (Arctic Ocean) Unglaciated Glaciated George Tanski 14

  16. Topic II: Degradation of organic matter Retrogressive thaw slump: „Slump D“ George Tanski 15

  17. Topic II: Degradation of organic matter Evolution of „Slump D“ George Tanski 16

  18. Topic II: Degradation of organic matter Vegetation classification of „Slump D“ based on NDVI George Tanski 17

  19. Topic II: Degradation of organic matter DOC Surface/10cm depth 30cm depth George Tanski 18

  20. Topic II: Degradation of organic matter DON Surface/10cm depth 30cm depth George Tanski 19

  21. Topic II: Degradation of organic matter NH 4 Surface/10cm depth 30cm depth George Tanski 20

  22. Topic II: Conclusion DOC conc. gradient from permafrost headwall to slump deposits •  Degradation of DOC right after thawing High ammonium conc. directly after thawing •  Indicator for quick depletion of organic material Strong degradtion of organic material at the land-ocean interface • George Tanski 21

  23. Outlook and open questions What are the degradation mechanisms? What are the degradation patterns of POC ? What happens with permafrost carbon after transport into the ocean? What are possible impacts on nearshore marine nearshore ecosystem ? How is OC incorporated into local food webs ? George Tanski 22

  24. PYRN PYRN celebratesf its 10 th anniversary • Just released its long-term strategy until 2018 • Is seeking to increase the network • More involvement of east asian partners planned • @ICOP 2016 big young researcher workshop planned • ICOP 2016 chance to be part of the new Executive Committee • You can apply for travel funding! • George Tanski 23

  25. PYRN Improvement of the network • Census preparation in progress • Meet us at the poster session ! • Find us online or on facebook! • George Tanski 24

  26. Thank you very much for the attention! Herschel Island, Yukon, Canada

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