Abstract
The distribution and state of subsea permafrost is largely unknown. Present maps, which rely heavily on model results, suggest that subsea permafrost is confined to the Beaufort, Siberian and Laptev seas. Here we show that discontinuous subsea permafrost exists along the Labrador coast (56 °N) under the influence of the Labrador Coastal Current. High-resolution bathymetric data reveal the presence of subsea thermokarst environments on the coastal seabed of Nain, Nunatsiavut, where an ice-rich sediment sample was recovered in July 2022 at a water depth of 27 m. Porewater analysis indicates that ground ice can persist in the sediments due to freshened submarine groundwater seepage that freezes at higher temperatures (0 °C) than seawater (−1.8 °C). The formation and preservation of subsea permafrost landforms is due to cold waters of the Labrador Coastal Current entering the coastal areas and remaining less than 0 °C for most of the year. Therefore, evidence of subsea permafrost landforms in coastal Labrador and the distribution of cold bottom water in the Northern Hemisphere suggests that subsea permafrost is likely to be preserved elsewhere in subarctic regions, especially where freshened submarine groundwater seepage elevates the freezing temperature. This highlights the potential underestimation of subsea permafrost in the world’s coastal oceans.
This is a preview of subscription content, access via your institution
Access options
Access Nature and 54 other Nature Portfolio journals
Get Nature+, our best-value online-access subscription
$29.99 / 30 days
cancel any time
Subscribe to this journal
Receive 12 print issues and online access
$259.00 per year
only $21.58 per issue
Buy this article
- Purchase on SpringerLink
- Instant access to full article PDF
Prices may be subject to local taxes which are calculated during checkout
Similar content being viewed by others
Data availability
All data are available from the Geological Survey of Canada Expedition Database and by contacting Natural Resources Canada (https://ed.marine-geo.canada.ca/cruises_e.php) under cruise 2021LudyPudluk, 2021Nuliajuk, 2022William-Kennedy and 2023002. The multi-beam bathymetry, the chloride content of porewater, the Ra isotopes of bottom waters and the CTD profiles from 2022, are available as source data with this manuscript. Bottom temperature maps (Fig. 6) were derived using EU Copernicus Marine Service Information (https://doi.org/10.48670/moi-00021). Source data are provided with this paper.
References
Harris, S. et al. Glossary of Permafrost and Related Ground-Ice Terms (National Research Council of Canada, 1988).
Zhang, T., Barry, R. G., Knowles, K., Heginbottom, J. A. & Brown, J. Statistics and characteristics of permafrost and ground-ice distribution in the Northern Hemisphere. Polar Geogr. 31, 47–68 (2008).
Wild, B. et al. Organic matter composition and greenhouse gas production of thawing subsea permafrost in the Laptev Sea. Nat. Commun. 13, 5057 (2022).
Angelopoulos, M., Overduin, P. P., Miesner, F., Grigoriev, M. N. & Vasiliev, A. A. Recent advances in the study of Arctic submarine permafrost. Permafr. Periglac. Process. 31, 442–453 (2020).
Rekant, P. et al. Evolution of subsea permafrost landscapes in Arctic Siberia since the Late Pleistocene: a synoptic insight from acoustic data of the Laptev Sea. arktos 1, 11 (2015).
Lindgren, A., Hugelius, G., Kuhry, P., Christensen, T. R. & Vandenberghe, J. GIS-based maps and area estimates of Northern Hemisphere permafrost extent during the Last Glacial Maximum. Permafr. Periglac. Process. 27, 6–16 (2016).
Overduin, P. P. et al. Submarine permafrost map in the Arctic modeled using 1‐D transient heat flux (supermap). J. Geophys. Res. Oceans 124, 3490–3507 (2019).
Sayedi, S. S. et al. Subsea permafrost carbon stocks and climate change sensitivity estimated by expert assessment. Environ. Res. Lett. 15, 124075 (2020).
Paull, C. K. et al. Rapid seafloor changes associated with the degradation of Arctic submarine permafrost. Proc. Natl Acad. Sci. USA 119, e2119105119 (2022).
Angelopoulos, M. et al. Heat and salt flow in subsea permafrost modeled with CryoGRID2. J. Geophys. Res. Earth Surf. 124, 920–937 (2019).
Miesner, F. et al. Subsea permafrost organic carbon stocks are large and of dominantly low reactivity. Sci. Rep. 13, 9425 (2023).
Natali, S. M. et al. Permafrost carbon feedbacks threaten global climate goals. Proc. Natl Acad. Sci. USA 118, e2100163118 (2021).
Duchesne, M. J., Fabien‐Ouellet, G. & Bustamante, J. Detecting subsea permafrost layers on marine seismic data: an appraisal from forward modelling. Near Surf. Geophys. 21, 3–20 (2023).
Angelopoulos, M. Mapping subsea permafrost with electrical resistivity surveys. Nat. Rev. Earth Environ. 3, 6 (2022).
Shakhova, N. et al. Current rates and mechanisms of subsea permafrost degradation in the East Siberian Arctic Shelf. Nat. Commun. 8, 15872 (2017).
French, H. & Shur, Y. The principles of cryostratigraphy. Earth Sci. Rev. 101, 190–206 (2010).
Way, R. G., Lewkowicz, A., Wang, Y. & McCarney, P. Permafrost Investigations below the Marine Limit at Nain, Nunatsiavut, Canada. In Permafrost 2021: Merging Permafrost Science and Cold Regions Engineering 38–48 (American Society of Civil Engineers, 2021).
Tarasov, L. & Peltier, W. R. A geophysically constrained large ensemble analysis of the deglacial history of the North American ice-sheet complex. Quat. Sci. Rev. 23, 359–388 (2004).
Vacchi, M. et al. Postglacial relative sea-level histories along the eastern Canadian coastline. Quat. Sci. Rev. 201, 124–146 (2018).
Clark, P. U. & Fitzhugh, W. W. Late deglaciation of the central Labrador coast and its implications for the age of glacial lakes Naskaupi and McLean and for prehistory. Quat. Res. 34, 296–305 (1990).
Hoffmann, J. J. L. et al. Complex eyed pockmarks and submarine groundwater discharge revealed by acoustic data and sediment cores in Eckernförde Bay, SW Baltic Sea. Geochem. Geophys. Geosyst. 21, e2019GC008825 (2020).
Garcia-Orellana, J. et al. Radium isotopes as submarine groundwater discharge (SGD) tracers: review and recommendations. Earth Sci. Rev. 220, 103681 (2021).
Paull, C. K. et al. Origin of pingo-like features on the Beaufort Sea shelf and their possible relationship to decomposing methane gas hydrates. Geophys. Res. Lett. https://doi.org/10.1029/2006GL027977 (2007).
Frederick, J. M. & Buffett, B. A. Effects of submarine groundwater discharge on the present-day extent of relict submarine permafrost and gas hydrate stability on the Beaufort Sea continental shelf. J. Geophys. Res. Earth Surf. 120, 417–432 (2015).
Gwiazda, R. et al. Freshwater seepage into sediments of the shelf, shelf edge, and continental slope of the Canadian Beaufort Sea. Geochem. Geophys. Geosyst. 19, 3039–3055 (2018).
Frederick, J. M. & Buffett, B. A. Submarine groundwater discharge as a possible formation mechanism for permafrost-associated gas hydrate on the circum-Arctic continental shelf. J. Geophys. Res. Solid Earth 121, 1383–1404 (2016).
Johnson, J. P. Jr. Deglaciation of the central Nain-Okak Bay section of Labrador. Arctic 22, 373–394 (1969).
Lévesque, Y., Walter, J. & Chesnaux, R. Transient electromagnetic (TEM) surveys as a first approach for characterizing a regional aquifer: the case of the Saint-Narcisse Moraine, Quebec, Canada. Geosciences 11, 415 (2021).
Petrie, B. The cold intermediate layer on the Labrador and northeast Newfoundland Shelves, 1978–1986. NAFO Sci. Counc. Stud. 12, 57–69 (1988).
Pickart, R. S. Water mass components of the North Atlantic deep western boundary current. Deep Sea Res. A 39, 1553–1572 (1992).
Riseborough, D., Shiklomanov, N., Etzelmüller, B., Gruber, S. & Marchenko, S. Recent advances in permafrost modelling. Permafr. Periglac. Process. 19, 137–156 (2008).
Riseborough, D. W. Soil latent heat as a filter of the climate signal in permafrost. In Proc. 5th Canadian Permafrost Conference 199–205 (Citeseer, 1990).
Burn, C. R. & Smith, Ca. S. Observations of the ‘thermal offset’ in near-surface mean annual ground temperatures at several sites near Mayo, Yukon territory. Can. Arctic 41, 99–104 (1988).
Galbraith, P. S., Larouche, P. & Caverhill, C. A sea-surface temperature homogenization blend for the northwest Atlantic. Can. J. Remote Sens. 47, 554–568 (2021).
Barrette, C. et al. Nunavik and Nunatsiavut regional climate information update, second iteration. In Nunavik and Nunatsiavut: From Science to Policy. An Integrated Regional Impact Study (IRIS) of climate change and modernization (eds Ropars, P. et al.) 1–66 (ArcticNet, 2020).
Wilkenskjeld, S., Miesner, F., Overduin, P. P., Puglini, M. & Brovkin, V. Strong increase in thawing of subsea permafrost in the 22nd century caused by anthropogenic climate change. Cryosphere 16, 1057–1069 (2022).
Angelopoulos, M. et al. Thermokarst lake to lagoon transitions in eastern Siberia: do submerged taliks refreeze? J. Geophys. Res. Earth Surf. 125, e2019JF005424 (2020).
Cyr, F. & Galbraith, P. S. A climate index for the Newfoundland and Labrador shelf. Earth Syst. Sci. Data 13, 1807–1828 (2021).
Cyr, F. et al. Physical Oceanographic Conditions on the Newfoundland and Labrador Shelf During 2017 (Canadian Science Advisory Secretariat, 2019); https://waves-vagues.dfo-mpo.gc.ca/library-bibliotheque/40855430.pdf
Fraser, C. L’évolution Morphologique et le Développement Stratigraphique des Dépôts Littoraux en Milieu de Régression Forcée à Umiujaq, Baie d’Hudson. MSc thesis, Université du Québec à Rimouski (2001).
Hay, A. Remote acoustic imaging of the plume from a submarine spring in an Arctic fjord. Science 225, 1154–1156 (1984).
Micallef, A. et al. Offshore freshened groundwater in continental margins. Rev. Geophys. 59, e2020RG000706 (2021).
Heginbottom, J. A., Brown, J., Melnikov, E. S. & Ferrians, O. J. Jr. Circumarctic map of permafrost and ground ice conditions. In Proc. 6th International Conference on Permafrost 1132–1136 (South China Univ. Technology Press, 1993).
Wang, Y. et al. Significant underestimation of peatland permafrost along the Labrador Sea coastline in northern Canada. Cryosphere 17, 63–78 (2023).
Gilbert, R., Naldrett, D. L. & Horvath, V. V. Holocene sedimentary environment of Cambridge Fjord, Baffin Island, Northwest Territories. Can. J. Earth Sci. 27, 271–280 (1990).
Acknowledgements
This project was funded by the Marine Geoscience for Marine Spatial Planning of the Geological Survey of Canada (Natural Resources Canada), and the Natural Science and Engineering Research Council of Canada Ship-time allocation grant. We thank Kirk Regular and Adam Templeton for surveys on the RV Ludy-Pudluk (partly funded by a Canada Research Chair in Ocean Mapping at the Marine Institute of Memorial University) and RV Nuliajuk as well as all the scientific participants of the 2022 and 2023 RV William-Kennedy cruises. Work on the RV William-Kennedy was supported in part by the Churchill Marine Observatory, a Canada Foundation for Innovation grant led by the University of Manitoba in collaboration with other partners, including the Arctic Research Foundation. We also acknowledge the Nunatsiavut Government, the Nunatsiavut Research Centre and the Labrador Inuit of Nain for their guidance on research conducted on traditional Inuit lands. This work was completed with Nunatsiavut government Research Advisory Committee approval nos 18034796 and 11666556.
Author information
Authors and Affiliations
Contributions
A.N., A.L. and K.R. secured funding for the different cruises. A.N. and K.R. designed the 2021 mapping cruise. A.N., J.B.R.E. and A.L. designed the sampling cruises. A.N., A.L. and M.S. managed the research programme. A.N., J.B.R.E., R.G.W., E.J.H., F.C., J.L.E., H.D.G., N.V.N., J.H., L.P., G.P., J.T., A.L., C.K.A., B.L.K., M.S. and H.D.G. collected, processed and/or analysed the data. All authors contributed to the writing and review of the manuscript.
Corresponding author
Ethics declarations
Competing interests
The authors declare no competing interests.
Peer review
Peer review information
Nature Geoscience thanks Pier Overduin and the other, anonymous, reviewer(s) for their contribution to the peer review of this work. Primary Handling Editor: Tom Richardson, in collaboration with the Nature Geoscience team.
Additional information
Publisher’s note Springer Nature remains neutral with regard to jurisdictional claims in published maps and institutional affiliations.
Supplementary information
Supplementary Information
Supplementary Sections 1 and 2.
Supplementary Data 1
Radium data.
Source data
Source Data Fig. 1
Multi-beam data of Webb’s Bay.
Source Data Fig. 3
Porewater data.
Source Data Fig. 5
CTD data presented in the paper. Zip files include cnv files (July 2022) and xlsx files (September 2022).
Source Data Fig. 2
Subbottom profiles shown in Fig. 2, in JP2000 format.
Rights and permissions
About this article
Cite this article
Normandeau, A., Eamer, J.B.R., Way, R.G. et al. Evidence for subsea permafrost in subarctic Canada linked to submarine groundwater discharge. Nat. Geosci. (2024). https://doi.org/10.1038/s41561-024-01497-z
Received:
Accepted:
Published:
DOI: https://doi.org/10.1038/s41561-024-01497-z