FN Archimer Export Format
PT J
TI Assessment of C, N and Si isotopes as tracers of past ocean nutrient and carbon cycling
BT 
AF Farmer, Jesse
   Hertzberg, Jennifer
   Cardinal, Damien
   Fietz, Susanne
   Hendry, Katharine
   Jaccard, Sam
   Paytan, Adina
   Rafter, Patrick
   Ren, Haojia
   Somes, Christopher
   SUTTON, Jill
AS 1:1,2;2:3;3:4;4:5;5:6;6:7,8;7:9;8:10;9:11;10:12;11:13;12:;
FF 1:;2:;3:;4:;5:;6:;7:;8:;9:;10:;11:;12:;
C1 Department of Geosciences, Princeton University, Princeton, NJ, USA
   Max-Planck Institute for Chemistry, Mainz, Germany
   Department of Ocean, Earth & Atmospheric Sciences, Old Dominion University, Norfolk, VA, USA
   LOCEAN (UMR7159), Sorbonne Université, IRD, CNRS, MNHN, Paris, France
   Department of Earth Sciences, Stellenbosch University, Stellenbosch, South Africa
   School of Earth Sciences, University of Bristol, Bristol, UK
   Institute of Geological Sciences and Oeschger Center for Climate Change Research, University of Bern, Bern, Switzerland
   Institute of Earth Sciences, University of Lausanne, Lausanne, Switzerland
   Institute of Marine Sciences, University of California, Santa Cruz, Santa Cruz, CA, USA
   Department of Earth System Science, University of California, Irvine, CA, USA
   Department of Geosciences, National Taiwan University, Taipei, Taiwan
   GEOMAR Helmholtz Centre for Ocean Research Kiel, 24105 Kiel, Germany
   Univ Brest, CNRS, IRD, Ifremer, Institut Universitaire Européen de la Mer, LEMAR, Plouzané, France
C2 UNIV PRINCETON, USA
   MAX PLANCK INST CHEM, GERMANY
   UNIV OLD DOMINION, USA
   UNIV SORBONNE, FRANCE
   UNIV STELLENBOSCH, SOUTH AFRICA
   UNIV BRISTOL, UK
   UNIV BERN, SWITZERLAND
   UNIV LAUSANNE, SWITZERLAND
   UNIV CALIF SANTA CRUZ, USA
   UNIV CALIF IRVINE, USA
   UNIV NATL TAIWAN, TAIWAN
   IFM GEOMAR, GERMANY
   UBO, FRANCE
UM LEMAR
IN WOS Cotutelle UMR
   copubli-france
   copubli-europe
   copubli-univ-france
   copubli-int-hors-europe
   copubli-sud
IF 6.5
TC 7
UR https://archimer.ifremer.fr/doc/00649/76114/85186.pdf
LA English
DT Article
DE ;marine chemistry;carbon;nitrogen;silicon;paleoceanography;stable isotopes
AB Biological productivity in the ocean directly influences the partitioning of carbon between the atmosphere and ocean interior, thereby controlling the distributions of many elements and their isotopes in the ocean. Through this carbon cycle feedback, changing ocean productivity has long been hypothesized as a key pathway for modulating past atmospheric carbon dioxide levels and hence global climate. To reconstruct climate impacts from temporal changes in paleoproductivity, robust proxies are needed to test the connection between past ocean productivity, nutrient biogeochemistry, ocean circulation and climate. Here we compile water column carbon (C), nitrogen (N) and silicon (Si) stable isotopes from GEOTRACES-era data in four key ocean regions to review geochemical proxies of oceanic carbon and nutrient partitioning based on the C, N, and Si isotopic composition of marine sediments. Relationships between water column isotope distributions, ocean productivity, and nutrient utilization are discussed. The potential for isotope measurements in sedimentary archives to record aspects of past ocean productivity are evaluated, along with key uncertainties and limitations associated with each proxy. Constraints on past ocean productivity, nutrient cycling and utilization during late Quaternary glacial-interglacial cycles and over the Cenozoic are examined. This review highlights opportunities for future research using multielement proxy applications and emphasizes the importance of such applications to reconstructing Cenozoic climate evolution. 
PY 2021
PD JUN
SO Global Biogeochemical Cycles
SN 0886-6236
PU American Geophysical Union
VL 35
IS 7
UT 000677815700008
DI 10.1029/2020GB006775
ID 76114
ER

EF