Premium
Nutrient cycling in the Atlantic basin: The evolution of nitrate isotope signatures in water masses
Author(s) -
Tuerena R. E.,
Ganeshram R. S.,
Geibert W.,
Fallick A. E.,
Dougans J.,
Tait A.,
Henley S. F.,
Woodward E. M. S.
Publication year - 2015
Publication title -
global biogeochemical cycles
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 2.512
H-Index - 187
eISSN - 1944-9224
pISSN - 0886-6236
DOI - 10.1002/2015gb005164
Subject(s) - geotraces , oceanography , north atlantic deep water , water mass , water column , phytoplankton , nitrate , thermohaline circulation , denitrification , environmental science , transect , geology , nutrient , chemistry , ecology , nitrogen , biology , organic chemistry
A basin‐wide transect of nitrate isotopes ( δ 15 N NO3 , δ 18 O NO3 ), across the UK GEOTRACES 40°S transect in the South Atlantic is presented. This data set is used to investigate Atlantic nutrient cycling and the communication pathways of nitrogen cycling processes in the global ocean. Intermediate waters formed in the subantarctic are enriched in δ 15 N NO3 and δ 18 O NO3 from partial utilization of nitrate by phytoplankton and distant denitrification processes, transporting heavy isotope signatures to the subtropical Atlantic. Water mass modification through the Atlantic is investigated by comparing data from 40°S (South Atlantic) and 30°N (North Atlantic). This reveals that nitrate in the upper intermediate waters is regenerated as it transits through the subtropical Atlantic, as evidenced by decreases in δ 18 O NO3. We document diazotrophy‐producing high N:P particle ratios (18–21:1) for remineralization, which is further confirmed by a decrease in δ 15 N NO3 through the subtropical Atlantic. These modifications influence the isotopic signatures of the North Atlantic Deep Water (NADW) which is subsequently exported from the Atlantic to the Southern Ocean. This study reveals the dominance of recycling processes and diazotrophy on nitrate cycling in the Atlantic. These processes provide a source of low δ 15 N NO3 to the Southern Ocean via the NADW, to counteract enrichment in δ 15 N NO3 from water column denitrification in the Indo/Pacific basins. We hence identify the Southern Ocean as a key hub through which denitrification and N 2 fixation communicate in the ocean through deepwater masses. Therefore, the balancing of the oceanic N budget and isotopic signatures require time scales of oceanic mixing.