Institut des Sciences de la Mer de Rimouski (ISMER), Université du Québec à Rimouski (UQAR), 310 Allée des Ursulines, Rimouski, Québec, G5L 3AL, Canada
Groupe de recherche Québec-Océan, Québec City, Canada
Département de Sciences Biologiques, Université de Montréal, 1375 Avenue Thérèse-Lavoie-Roux, Montréal, Québec, H2V 0B3, Canada
Groupe de Recherche Interuniversitaire en Limnologie (GRIL), Montréal, Canada
Jean-François Lapierre
Département de Sciences Biologiques, Université de Montréal, 1375 Avenue Thérèse-Lavoie-Roux, Montréal, Québec, H2V 0B3, Canada
Groupe de Recherche Interuniversitaire en Limnologie (GRIL), Montréal, Canada
Institut des Sciences de la Mer de Rimouski (ISMER), Université du Québec à Rimouski (UQAR), 310 Allée des Ursulines, Rimouski, Québec, G5L 3AL, Canada
Groupe de recherche Québec-Océan, Québec City, Canada
Publisher's note: On 31 August 2026, Figure 4 was corrected because it had been inadvertently published as a duplicate of Figure 6.
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Climate change is accelerating permafrost thaw and coastal erosion, increasing dissolved organic matter (DOM) inputs to the Arctic Ocean. We show that, beyond seawater dilution, DOM is transformed as it passes through Arctic beach subterranean estuaries, shifting from humic-rich to more microbially processed material. These coastal zones act as biogeochemical reactors, modifying DOM before its export to coastal waters.
Climate change is accelerating permafrost thaw and coastal erosion, increasing dissolved organic...