Southern Ocean control of silicon stable isotope distribution in the deep Atlantic Ocean

• Published in: Global Biogeochemical Cycles
• Main Authors: de Souza, Gregory F., Reynolds, Ben C., Rickli, Joerg, Frank, Martin, Saito, Mak A., Gerringa, Loes J. A., Bourdon, Bernard
• Other Authors: Institute of Geochemistry and Petrology ETH Zürich, Department of Earth Sciences Swiss Federal Institute of Technology - ETH Zürich (D-ERDW), Eidgenössische Technische Hochschule - Swiss Federal Institute of Technology Zürich (ETH Zürich)- Eidgenössische Technische Hochschule - Swiss Federal Institute of Technology Zürich (ETH Zürich), Helmholtz Centre for Ocean Research Kiel (GEOMAR), Woods Hole Oceanographic Institution (WHOI), Royal Netherlands Institute for Sea Research (NIOZ), Laboratoire de Géologie de Lyon - Terre, Planètes, Environnement (LGL-TPE), École normale supérieure de Lyon (ENS de Lyon)-Université Claude Bernard Lyon 1 (UCBL), Université de Lyon-Université de Lyon-Institut national des sciences de l'Univers (INSU - CNRS)-Université Jean Monnet - Saint-Étienne (UJM)-Centre National de la Recherche Scientifique (CNRS), Swiss National Science Foundation (200021-116473, 200020-130361)
• Format: Article in Journal/Newspaper
• Language: English
• Published: HAL CCSD 2012
• Subjects: ANTARCTIC BOTTOM WATER; NORTH-ATLANTIC; NORDIC SEAS; OVERTURNING CIRCULATION; MEAN CIRCULATION; ATMOSPHERIC CO2; WEDDELL SEA; WORLD OCEAN; ICP-MS; SI; [SDU.STU]Sciences of the Universe [physics]/Earth Sciences; Antarctic; Drake Passage; Southern Ocean; Weddell; Weddell Sea; Antarc*; Denmark Strait; Nordic Seas; North Atlantic
• Online Access: https://hal.science/hal-00721135; https://hal.science/hal-00721135/document; https://hal.science/hal-00721135/file/2011GB004141.pdf; https://doi.org/10.1029/2011GB004141

International audience The fractionation of silicon (Si) stable isotopes by biological activity in the surface ocean makes the stable isotope composition of silicon (delta Si-30) dissolved in seawater a sensitive tracer of the oceanic biogeochemical Si cycle. We present a high-precision dataset that characterizes the delta Si-30 distribution in the deep Atlantic Ocean from Denmark Strait to Drake Passage, documenting strong meridional and smaller, but resolvable, vertical delta Si-30 gradients. We show that these gradients are related to the two sources of deep and bottom waters in the Atlantic Ocean: waters of North Atlantic and Nordic origin carry a high delta(30)Sisignature of >=+1.7 parts per thousand into the deep Atlantic, while Antarctic Bottom Water transports Si with a low delta Si-30 value of around +1.2 parts per thousand. The deep Atlantic delta Si-30 distribution is thus governed by the quasi-conservative mixing of Si from these two isotopically distinct sources. This disparity in Si isotope composition between the North Atlantic and Southern Ocean is in marked contrast to the homogeneity of the stable nitrogen isotope composition of deep ocean nitrate (delta N-15-NO3). We infer that the meridional delta Si-30 gradient derives from the transport of the high delta Si-30 signature of Southern Ocean intermediate/mode waters into the North Atlantic by the upper return path of the meridional overturning circulation (MOC). The basin-scale deep Atlantic delta Si-30 gradient thus owes its existence to the interaction of the physical circulation with biological nutrient uptake at high southern latitudes, which fractionates Si isotopes between the abyssal and intermediate/mode waters formed in the Southern Ocean.