High Lithogenic and Micro‐Nutrient Fluxes From the West Greenland Margin Traced by Thorium in Seawater and Sediments

Abstract The flux of nutrients from continents to the oceans sustains oceanic primary productivity and is a fundamental component of the carbon cycle. In most regions of the world's oceans primary productivity is limited by the supply of nutrients. In particular, iron can become limiting in the open‐ocean due to its low solubility. Glaciated continents have been suggested as an underappreciated source of iron to the high‐latitude oceans. Yet, uncertainty remains regarding the magnitude and spatial variability of glacially derived nutrient fluxes, and the extent to which these nutrients impact open‐ocean ecosystems. To quantify lithogenic fluxes at the West Greenland margin, we measured 232 Th and 230 Th in seawater and core‐top sediments across the shelf and slope. Our results highlight a negative correlation between low‐salinity waters and dissolved and particulate 232 Th, suggesting a glacial source for this lithogenic isotope. We calculated dissolved 232 Th fluxes 5–24 μg m −2 yr −1 (100–500 m depth), and sedimentary 232 Th fluxes 105–711 μg m −2 yr −1 , higher than typical open‐ocean settings and similar to margin sites influenced by large inputs from aeolian dust and rivers. A sampling transect shows that dissolved 232 Th fluxes increase toward Greenland, confirming that lithogenic inputs are sourced laterally from the margin. Using our 232 Th fluxes, we estimate an elevated supply of dissolved Fe which extends over the continental slope toward the open ocean. This Fe flux is large enough to support much of the local primary productivity, highlighting the importance of lithogenic fluxes in supporting the marine ecosystem in high‐latitude oceans.