Glacial‐interglacial variations in sediment organic carbon accumulation and benthic foraminiferal assemblages on the Bermuda Rise (ODP Site 1063) during MIS 13 to 10

Peer Reviewed http://deepblue.lib.umich.edu/bitstream/2027.42/94866/1/palo1807.pdf

Bibliographic Details
Published in:Paleoceanography
Main Authors: Poli, Maria Serena, Meyers, Philip A., Thunell, Robert C., Capodivacca, Marco
Other Authors: Department of Earth and Environmental Sciences, University of Michigan, Ann Arbor, Michigan, USA, Now at TetraTech Geo, Ann Arbor, Michigan, USA, Department of Earth and Ocean Sciences, University of South Carolina, Columbia, South Carolina, USA, Department of Geography and Geology, Eastern Michigan University, Ypsilanti, Michigan, USA
Format: Article in Journal/Newspaper
Language:unknown
Published: Wiley 2012
Subjects:
Organic Carbon Isotopes
Benthic Foraminifera
TOC/TN Ratio
TOC MAR
Atmospheric and Oceanic Sciences
Science
Arctic
Online Access:https://hdl.handle.net/2027.42/94866
https://doi.org/10.1029/2012PA002314
id ftumdeepblue:oai:deepblue.lib.umich.edu:2027.42/94866
record_format openpolar
institution Open Polar
collection University of Michigan: Deep Blue
op_collection_id ftumdeepblue
language unknown
topic Organic Carbon Isotopes
Benthic Foraminifera
TOC/TN Ratio
TOC MAR
Atmospheric and Oceanic Sciences
Science
spellingShingle Organic Carbon Isotopes
Benthic Foraminifera
TOC/TN Ratio
TOC MAR
Atmospheric and Oceanic Sciences
Science
Poli, Maria Serena
Meyers, Philip A.
Thunell, Robert C.
Capodivacca, Marco
Glacial‐interglacial variations in sediment organic carbon accumulation and benthic foraminiferal assemblages on the Bermuda Rise (ODP Site 1063) during MIS 13 to 10
topic_facet Organic Carbon Isotopes
Benthic Foraminifera
TOC/TN Ratio
TOC MAR
Atmospheric and Oceanic Sciences
Science
description Peer Reviewed http://deepblue.lib.umich.edu/bitstream/2027.42/94866/1/palo1807.pdf
author2 Department of Earth and Environmental Sciences, University of Michigan, Ann Arbor, Michigan, USA
Now at TetraTech Geo, Ann Arbor, Michigan, USA
Department of Earth and Ocean Sciences, University of South Carolina, Columbia, South Carolina, USA
Department of Geography and Geology, Eastern Michigan University, Ypsilanti, Michigan, USA
format Article in Journal/Newspaper
author Poli, Maria Serena
Meyers, Philip A.
Thunell, Robert C.
Capodivacca, Marco
author_facet Poli, Maria Serena
Meyers, Philip A.
Thunell, Robert C.
Capodivacca, Marco
author_sort Poli, Maria Serena
title Glacial‐interglacial variations in sediment organic carbon accumulation and benthic foraminiferal assemblages on the Bermuda Rise (ODP Site 1063) during MIS 13 to 10
title_short Glacial‐interglacial variations in sediment organic carbon accumulation and benthic foraminiferal assemblages on the Bermuda Rise (ODP Site 1063) during MIS 13 to 10
title_full Glacial‐interglacial variations in sediment organic carbon accumulation and benthic foraminiferal assemblages on the Bermuda Rise (ODP Site 1063) during MIS 13 to 10
title_fullStr Glacial‐interglacial variations in sediment organic carbon accumulation and benthic foraminiferal assemblages on the Bermuda Rise (ODP Site 1063) during MIS 13 to 10
title_full_unstemmed Glacial‐interglacial variations in sediment organic carbon accumulation and benthic foraminiferal assemblages on the Bermuda Rise (ODP Site 1063) during MIS 13 to 10
title_sort glacial‐interglacial variations in sediment organic carbon accumulation and benthic foraminiferal assemblages on the bermuda rise (odp site 1063) during mis 13 to 10
publisher Wiley
publishDate 2012
url https://hdl.handle.net/2027.42/94866
https://doi.org/10.1029/2012PA002314
genre Arctic
genre_facet Arctic
op_relation Poli, Maria Serena; Meyers, Philip A.; Thunell, Robert C.; Capodivacca, Marco (2012). "Glacial‐interglacial variations in sediment organic carbon accumulation and benthic foraminiferal assemblages on the Bermuda Rise (ODP Site 1063) during MIS 13 to 10." Paleoceanography 27(3): n/a-n/a. <http://hdl.handle.net/2027.42/94866>
0883-8305
1944-9186
https://hdl.handle.net/2027.42/94866
doi:10.1029/2012PA002314
Paleoceanography
Raymo, M. E., W. F. Ruddiman, N. J. Shackleton, and D. W. Oppo ( 1990 ), Evolution of Atlantic‐Pacific δ 13 C gradients over the last 2.5 m.y, Earth Planet. Sci. Lett., 97, 353 – 368, doi:10.1016/0012‐821X(90)90051‐X.
Schmiedl, G., and A. Mackensen ( 1997 ), Late quaternary paleoproductivity and deep water circulation in the eastern South Atlantic Ocean: Evidence from benthic foraminifera, Palaeogeogr. Palaeoclimatol. Palaeoecol., 130 ( 1–4 ), 43 – 80, doi:10.1016/S0031‐0182(96)00137‐X.
Schmittner, A. ( 2005 ), Decline of the marine ecosystem caused by a reduction in the Atlantic overturning circulation, Nature, 434, 628 – 633, doi:10.1038/nature03476.
Schmittner, A., A. Oschlies, H. D. Matthews, and E. D. Galbraith ( 2008 ), Future changes in climate, ocean circulation, ecosystems, and biogeochemical cycling simulated for a business‐as‐usual CO 2 emission scenario until year 4000 AD, Global Biogeochem. Cycles, 22, GB1013, doi:10.1029/2007GB002953.
Schnitker, D. ( 1974 ), West Atlantic abyssal circulation during the past 120,000 years, Nature, 248, 385 – 387, doi:10.1038/248385a0.
Schnitker, D. ( 1979 ), The deep waters of the western North Atlantic during the past 24,000 years, and the re‐initiation of the Western Boundary Undercurrent, Mar. Micropaleontol., 4, 265 – 280, doi:10.1016/0377‐8398(79)90020‐3.
Schnitker, D. ( 1980 ), Quaternary deep‐sea benthic foraminifers and bottom water masses, Annu. Rev. Earth Planet. Sci., 8, 343 – 370, doi:10.1146/annurev.ea.08.050180.002015.
Schwarz, J. N., and M. P. Schodlok ( 2009 ), Impact of drifting icebergs on surface phytoplankton biomass in the Southern Ocean: Ocean colour remote sensing and in situ iceberg tracking, Deep Sea Res., Part I, 56, 1727 – 1741, doi:10.1016/j.dsr.2009.05.003.
Shackleton, N. J., M. A. Hall, J. Line, and C. Shuxi ( 1983 ), Carbon isotope data in core V19–30 confirm reduced carbon dioxide concentration in the ice age atmosphere, Nature, 306 ( 5941 ), 319 – 322, doi:10.1038/306319a0.
Smart, C. W. ( 2008 ), Abyssal NE Atlantic benthic foraminifera during the last 15 kyr: Relation to variations in seasonality of productivity, Mar. Micropaleontol., 69, 193 – 211, doi:10.1016/j.marmicro.2008.07.007.
Smart, C. W., and A. J. Gooday ( 1997 ), Recent benthic foraminifera in the abyssal northeast Atlantic Ocean: Relation to phytodetrital inputs, J. Foraminiferal Res., 27 ( 2 ), 85 – 92, doi:10.2113/gsjfr.27.2.85.
Smart, C. W., S. C. King, A. J. Gooday, J. W. Murray, and E. Thomas ( 1994 ), A benthic foraminiferal proxy of pulsed organic matter paleofluxes, Mar. Micropaleontol., 23, 89 – 99, doi:10.1016/0377‐8398(94)90002‐7.
Smart, C. W., C. Waelbroeck, E. Michel, and A. Mazaud ( 2010 ), Benthic foraminiferal abundance and stable isotope changes in the Indian Ocean sector of the Southern Ocean during the last 20 kyr: Paleoceanographic implications, Palaeogeogr. Palaeoclimatol. Palaeoecol., 297, 537 – 548, doi:10.1016/j.palaeo.2010.08.011.
Smith, K., B. H. Robison, J. J. Helly, R. S. Kaufmann, H. A. Ruhl, T. J. Shaw, B. S. Twining, and M. Vernet ( 2007 ), Free‐drifting icebergs: Hot spots of chemical and biological enrichment in the Weddell Sea, Science, 317, 478 – 482, doi:10.1126/science.1142834.
Stein, R., J. Hefter, J. Grutzner, A. Voelker, and B. D. A. Naafs ( 2009 ), Variability of surface water characteristics and Heinrich‐like events in the Pleistocene midlatitude North Atlantic Ocean: Biomarker and XRD records from IODP Site U1313(MIS 16–9), Paleoceanography, 24, PA2203, doi:10.1029/2008PA001639.
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Thierstein, H. R., B. Molfino, K. Geitzenauer, and N. J. Shackleton ( 1977 ), Global synchroneity of late Quaternary coccolith datum levels; validation by oxygen isotopes, Geology, 5, 400 – 404, doi:10.1130/0091‐7613(1977)5<400:GSOLQC>2.0.CO;2.
Thomas, E., and A. J. Gooday ( 1996 ), Cenozoic deep‐sea benthic foraminifers: Tracers for changes in oceanic productivity?, Geology, 24 ( 4 ), 355 – 358, doi:10.1130/0091‐7613(1996)024<0355:CDSBFT>2.3.CO;2.
Thomas, E., L. Booth, M. Maslin, and N. Shackleton ( 1995 ), Northeastern Atlantic benthic foraminifera during the last 45,000 years: Changes in productivity seen from the bottom up, Paleoceanography, 10 ( 3 ), 545 – 562, doi:10.1029/94PA03056.
Verardo, D. J., and A. McIntyre ( 1994 ), Production and destruction: Control of biogenous sedimentation in the tropical Atlantic 0–300 000 years BP, Paleoceanography, 9, 63 – 86, doi:10.1029/93PA02901.
Villanueva, J., E. Calvo, C. Pelejero, J. O. Grimalt, A. Boelaert, and L. D. Labeyrie ( 2001 ), A latitudinal productivity band in the central North Atlantic over the past 20 kyr: An alkenone perspective, Paleoceanography, 16, 617 – 626, doi:10.1029/2000PA000543.
Yoder, J. A., L. P. Atkinson, T. N. Lee, H. H. Kim, and C. R. McClain ( 1981 ), Role of the Gulf Stream frontal eddies in forming phytoplankton patches on the outer southeastern shelf, Limnol. Oceanogr., 26, 1103 – 1110, doi:10.4319/lo.1981.26.6.1103.
Yoder, J. A., S. G. Ackleson, R. T. Barber, P. Flament, and W. M. Balch ( 1994 ), A line in the sea, Nature, 371, 689 – 692, doi:10.1038/371689a0.
Alonso‐Garcia, M., F. J. Sierro, and J. A. Flores ( 2011 ), Arctic front shifts in the subpolar North Atlantic during the Mid‐Pleistocene (800–400 ka) and their implications for ocean circulation, Palaeogeogr. Palaeoclimatol. Palaeoecol., 311 ( 3–4 ), 268 – 280, doi:10.1016/j.palaeo.2011.09.004.
Altenbach, A. V., and M. Sarnthein ( 1989 ), Productivity record in benthic foraminifera, in Productivity of the Ocean: Present and Past, edited by W. H. Berger, V. S. Smetaceck, and G. Wefer, pp. 255 – 269, Wiley, Chichester, U. K.
Altenbach, A. V., U. Pflauman, R. Schiebel, A. Thies, S. Timm, and M. Trauth ( 1999 ), Scaling percentages and distributional patterns of benthic foraminifera with flux rates of organic carbon, J. Foraminiferal Res., 29 ( 3 ), 173 – 185.
Alve, E. ( 2010 ), Benthic foraminiferal responses to absence of fresh phytodetritus: A two year experiment, Mar. Micropaleontol., 76, 67 – 75, doi:10.1016/j.marmicro.2010.05.003.
Antoine, D., J.‐M. Andre, and A. Morel ( 1996 ), Oceanic primary production. Estimation at global scale from satellite (coastal zone color scanner) chlorophyll, Global Biogeochem. Cycles, 10, 57 – 69, doi:10.1029/95GB02832.
Bassinot, F. C., L. D. Labeyrie, E. Vincent, X. Quidelleur, N. J. Shackleton, and Y. Lancelot ( 1994 ), The astronomical theory of climate and the age of the Brunhes‐Matuyama magnetic reversal, Earth Planet. Sci. Lett., 126, 91 – 108, doi:10.1016/0012‐821X(94)90244‐5.
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Berger, W. H., and J. C. Herguera ( 1992 ), Reading the sedimentary record of the ocean's productivity, in Primary Productivity and Biogeochemical Cycles in the Sea, edited by P. G. Falkowski and A. D. Woodhead, pp. 455 – 486, Plenum, New York.
Berger, W. H., T. Bickert, M. K. Yasuda, and G. Wefer ( 1996 ), Reconstruction of atmospheric CO 2 levels from ice‐core data and the deep‐sea record of Ontong Java plateau: The Milankovitch Chron, Geol. Rundsch., 85, 466 – 495, doi:10.1007/BF02369003.
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spelling ftumdeepblue:oai:deepblue.lib.umich.edu:2027.42/94866 2023-08-20T04:03:12+02:00 Glacial‐interglacial variations in sediment organic carbon accumulation and benthic foraminiferal assemblages on the Bermuda Rise (ODP Site 1063) during MIS 13 to 10 Poli, Maria Serena Meyers, Philip A. Thunell, Robert C. Capodivacca, Marco Department of Earth and Environmental Sciences, University of Michigan, Ann Arbor, Michigan, USA Now at TetraTech Geo, Ann Arbor, Michigan, USA Department of Earth and Ocean Sciences, University of South Carolina, Columbia, South Carolina, USA Department of Geography and Geology, Eastern Michigan University, Ypsilanti, Michigan, USA 2012-09 application/pdf https://hdl.handle.net/2027.42/94866 https://doi.org/10.1029/2012PA002314 unknown Wiley Poli, Maria Serena; Meyers, Philip A.; Thunell, Robert C.; Capodivacca, Marco (2012). "Glacial‐interglacial variations in sediment organic carbon accumulation and benthic foraminiferal assemblages on the Bermuda Rise (ODP Site 1063) during MIS 13 to 10." Paleoceanography 27(3): n/a-n/a. <http://hdl.handle.net/2027.42/94866> 0883-8305 1944-9186 https://hdl.handle.net/2027.42/94866 doi:10.1029/2012PA002314 Paleoceanography Raymo, M. E., W. F. Ruddiman, N. J. Shackleton, and D. W. Oppo ( 1990 ), Evolution of Atlantic‐Pacific δ 13 C gradients over the last 2.5 m.y, Earth Planet. Sci. Lett., 97, 353 – 368, doi:10.1016/0012‐821X(90)90051‐X. Schmiedl, G., and A. Mackensen ( 1997 ), Late quaternary paleoproductivity and deep water circulation in the eastern South Atlantic Ocean: Evidence from benthic foraminifera, Palaeogeogr. Palaeoclimatol. Palaeoecol., 130 ( 1–4 ), 43 – 80, doi:10.1016/S0031‐0182(96)00137‐X. Schmittner, A. ( 2005 ), Decline of the marine ecosystem caused by a reduction in the Atlantic overturning circulation, Nature, 434, 628 – 633, doi:10.1038/nature03476. Schmittner, A., A. Oschlies, H. D. Matthews, and E. D. Galbraith ( 2008 ), Future changes in climate, ocean circulation, ecosystems, and biogeochemical cycling simulated for a business‐as‐usual CO 2 emission scenario until year 4000 AD, Global Biogeochem. Cycles, 22, GB1013, doi:10.1029/2007GB002953. Schnitker, D. ( 1974 ), West Atlantic abyssal circulation during the past 120,000 years, Nature, 248, 385 – 387, doi:10.1038/248385a0. Schnitker, D. ( 1979 ), The deep waters of the western North Atlantic during the past 24,000 years, and the re‐initiation of the Western Boundary Undercurrent, Mar. Micropaleontol., 4, 265 – 280, doi:10.1016/0377‐8398(79)90020‐3. Schnitker, D. ( 1980 ), Quaternary deep‐sea benthic foraminifers and bottom water masses, Annu. Rev. Earth Planet. Sci., 8, 343 – 370, doi:10.1146/annurev.ea.08.050180.002015. Schwarz, J. N., and M. P. Schodlok ( 2009 ), Impact of drifting icebergs on surface phytoplankton biomass in the Southern Ocean: Ocean colour remote sensing and in situ iceberg tracking, Deep Sea Res., Part I, 56, 1727 – 1741, doi:10.1016/j.dsr.2009.05.003. Shackleton, N. J., M. A. Hall, J. Line, and C. Shuxi ( 1983 ), Carbon isotope data in core V19–30 confirm reduced carbon dioxide concentration in the ice age atmosphere, Nature, 306 ( 5941 ), 319 – 322, doi:10.1038/306319a0. Smart, C. W. ( 2008 ), Abyssal NE Atlantic benthic foraminifera during the last 15 kyr: Relation to variations in seasonality of productivity, Mar. Micropaleontol., 69, 193 – 211, doi:10.1016/j.marmicro.2008.07.007. Smart, C. W., and A. J. Gooday ( 1997 ), Recent benthic foraminifera in the abyssal northeast Atlantic Ocean: Relation to phytodetrital inputs, J. Foraminiferal Res., 27 ( 2 ), 85 – 92, doi:10.2113/gsjfr.27.2.85. Smart, C. W., S. C. King, A. J. Gooday, J. W. Murray, and E. Thomas ( 1994 ), A benthic foraminiferal proxy of pulsed organic matter paleofluxes, Mar. Micropaleontol., 23, 89 – 99, doi:10.1016/0377‐8398(94)90002‐7. Smart, C. W., C. Waelbroeck, E. Michel, and A. Mazaud ( 2010 ), Benthic foraminiferal abundance and stable isotope changes in the Indian Ocean sector of the Southern Ocean during the last 20 kyr: Paleoceanographic implications, Palaeogeogr. Palaeoclimatol. Palaeoecol., 297, 537 – 548, doi:10.1016/j.palaeo.2010.08.011. Smith, K., B. H. Robison, J. J. Helly, R. S. Kaufmann, H. A. Ruhl, T. J. Shaw, B. S. Twining, and M. Vernet ( 2007 ), Free‐drifting icebergs: Hot spots of chemical and biological enrichment in the Weddell Sea, Science, 317, 478 – 482, doi:10.1126/science.1142834. Stein, R., J. Hefter, J. Grutzner, A. Voelker, and B. D. A. Naafs ( 2009 ), Variability of surface water characteristics and Heinrich‐like events in the Pleistocene midlatitude North Atlantic Ocean: Biomarker and XRD records from IODP Site U1313(MIS 16–9), Paleoceanography, 24, PA2203, doi:10.1029/2008PA001639. Steinacher, M., et al. ( 2010 ), Projected 21st century decrease in marine productivity: A multi‐model analysis, Biogeosciences, 7 ( 3 ), 979 – 1005, doi:10.5194/bg‐7‐979‐2010. Suess, E., and P. J. Müller ( 1980 ), Productivity, sedimentation rate and sedimentary organic matter in the oceans II.‐ Elemental fractionation, Colloq. Int. C. N. R. S., 293, 17 – 26. Sun, X., B. H. Corliss, C. W. Brown, and W. J. Showers ( 2006 ), The effect of primary productivity and seasonality on the distribution of deep‐sea benthic foraminifera in the North Atlantic, Deep Sea Res., Part I, 53, 28 – 47, doi:10.1016/j.dsr.2005.07.003. Thierstein, H. R., B. Molfino, K. Geitzenauer, and N. J. Shackleton ( 1977 ), Global synchroneity of late Quaternary coccolith datum levels; validation by oxygen isotopes, Geology, 5, 400 – 404, doi:10.1130/0091‐7613(1977)5<400:GSOLQC>2.0.CO;2. Thomas, E., and A. J. Gooday ( 1996 ), Cenozoic deep‐sea benthic foraminifers: Tracers for changes in oceanic productivity?, Geology, 24 ( 4 ), 355 – 358, doi:10.1130/0091‐7613(1996)024<0355:CDSBFT>2.3.CO;2. Thomas, E., L. Booth, M. Maslin, and N. Shackleton ( 1995 ), Northeastern Atlantic benthic foraminifera during the last 45,000 years: Changes in productivity seen from the bottom up, Paleoceanography, 10 ( 3 ), 545 – 562, doi:10.1029/94PA03056. Verardo, D. J., and A. McIntyre ( 1994 ), Production and destruction: Control of biogenous sedimentation in the tropical Atlantic 0–300 000 years BP, Paleoceanography, 9, 63 – 86, doi:10.1029/93PA02901. Villanueva, J., E. Calvo, C. Pelejero, J. O. Grimalt, A. Boelaert, and L. D. Labeyrie ( 2001 ), A latitudinal productivity band in the central North Atlantic over the past 20 kyr: An alkenone perspective, Paleoceanography, 16, 617 – 626, doi:10.1029/2000PA000543. Yoder, J. A., L. P. Atkinson, T. N. Lee, H. H. Kim, and C. R. McClain ( 1981 ), Role of the Gulf Stream frontal eddies in forming phytoplankton patches on the outer southeastern shelf, Limnol. Oceanogr., 26, 1103 – 1110, doi:10.4319/lo.1981.26.6.1103. Yoder, J. A., S. G. Ackleson, R. T. Barber, P. Flament, and W. M. Balch ( 1994 ), A line in the sea, Nature, 371, 689 – 692, doi:10.1038/371689a0. Alonso‐Garcia, M., F. J. Sierro, and J. A. Flores ( 2011 ), Arctic front shifts in the subpolar North Atlantic during the Mid‐Pleistocene (800–400 ka) and their implications for ocean circulation, Palaeogeogr. Palaeoclimatol. Palaeoecol., 311 ( 3–4 ), 268 – 280, doi:10.1016/j.palaeo.2011.09.004. Altenbach, A. V., and M. Sarnthein ( 1989 ), Productivity record in benthic foraminifera, in Productivity of the Ocean: Present and Past, edited by W. H. Berger, V. S. Smetaceck, and G. Wefer, pp. 255 – 269, Wiley, Chichester, U. K. Altenbach, A. V., U. Pflauman, R. Schiebel, A. Thies, S. Timm, and M. Trauth ( 1999 ), Scaling percentages and distributional patterns of benthic foraminifera with flux rates of organic carbon, J. Foraminiferal Res., 29 ( 3 ), 173 – 185. Alve, E. ( 2010 ), Benthic foraminiferal responses to absence of fresh phytodetritus: A two year experiment, Mar. Micropaleontol., 76, 67 – 75, doi:10.1016/j.marmicro.2010.05.003. Antoine, D., J.‐M. Andre, and A. Morel ( 1996 ), Oceanic primary production. Estimation at global scale from satellite (coastal zone color scanner) chlorophyll, Global Biogeochem. Cycles, 10, 57 – 69, doi:10.1029/95GB02832. Bassinot, F. C., L. D. Labeyrie, E. Vincent, X. Quidelleur, N. J. Shackleton, and Y. 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Hall ( 2005 ), Ocean climate variability in the eastern North Atlantic during interglacial marine isotope stage 11: A partial analogue to the Holocene?, Paleoceanography, 20, PA3009, doi:10.1029/2004PA001091. IndexNoFollow Organic Carbon Isotopes Benthic Foraminifera TOC/TN Ratio TOC MAR Atmospheric and Oceanic Sciences Science Article 2012 ftumdeepblue https://doi.org/10.1029/2012PA00231410.1016/0012‐821X(90)90051‐X10.1016/S0031‐0182(96)00137‐X10.1038/nature0347610.1029/2007GB00295310.1038/248385a010.1016/0377‐8398(79)90020‐310.1146/annurev.ea.08.050180.00201510.1016/j.dsr.2009.05.00310.1038/306319a010. 2023-07-31T20:45:13Z Peer Reviewed http://deepblue.lib.umich.edu/bitstream/2027.42/94866/1/palo1807.pdf Article in Journal/Newspaper Arctic University of Michigan: Deep Blue Paleoceanography 27 3 n/a n/a

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