The "White Ocean" hypothesis: A late Pleistocene Southern Ocean governed by coccolithophores and driven by phosphorus

Frontiers in Microbiology

Volumn 3, Issue JUL, 2012, Pages

  Flores, José Abel ^a   Filippelli, Gabriel M ^b   Sierro, Francisco J ^a   Latimer, Jennifer ^c  

^a UNIVERSITY OF SALAMANCA   (Spain)

^b INDIANA UNIVERSITY   (United States)

^c INDIANA STATE UNIVERSITY   (United States)

Author keywords

Coccolithophores; Geochemistry; Ocean drilling program; Paleoecology; Paleoproductivity; Phosphorus; Pleistocene; Southern ocean

Indexed keywords

EID: 84875770667     PISSN: None     EISSN: 1664302X     Source Type: Journal    
DOI: 10.3389/fmicb.2012.00233     Document Type: Article

References (89)

1. Ahagon, N., Tanaka, Y., and Ujiié, H. (1993). Florisphaera profunda,a possible nannoplankton indicator of late quaternary changes in sea-water turbidity at the northwestern margin of the Pacific. Mar. Micropaleontol. 22, 255-273.
2. Arrigo, K., Worthon, D., Schnell, V., and Lizotte, M. P. (1998). Primary production in Southern Ocean waters. J. Geophys. Res. 103, 15587-15600.
3. Asmus, T., Frank, M., Koschmieder, C., Frank, H., Gersonde, R., Kuhn, G., and Mangini, A. (1999). Variations of biogenic particle flux in the SouthernAtlantic section of the Subantarctic Zone during the late quaternary: evidence from sedimentary Pa-231(ex) and Th-230(ex). Mar. Geol. 159, 63-78.
4. Averyt, K. B., and Paytan, A. (2004). A comparison of multiple proxies for export production in the Equatorial Pacific. Paleoceanography 19, 4003-4016.
5. Balch, W. M. (2004). "Re-evaluation of the physiological ecology of coccolithophores,"Coccolithophores - From Molecular Processes to Global Impact, eds H. Thierstein and J. Young (Berlin: Springer), 165-190.
6. Baumann,K.-H.,Cepek,M.,and Kinkel, H. (1999). "Coccolithophores as indicators of ocean water masses, surface-water temperature, and paleoproductivity - examples from the South Atlantic," in Use of Proxies in Paleoceanography: Examples from the South Atlantic, eds G. Fischer and G. Wefer (Berlin: Springer), 117-144.
7. Baumann, K. H., and Freitag, T. (2004). Pleistocene fluctuations in the northern Benguela Current system as revealed by coccolith assemblages. Mar. Micropaloentol. 52, 195-215.
8. Beaufort, L., de Garidel-Thoron, A., Mix, N., and Pisias, G. (2001). ENSO-like forcing on oceanic primary production during the late Pleistocene. Science 293, 2440-2444.
9. Beaufort, L., Lancelot, Y., Camberlin, P., Cayre, O., Vincent, E., Bassinot, F., and Labeyrie, L. (1997). Insolation cycles as major control of Equatorial Indian Ocean primary production. Science 278, 1451-1454.
10. Becquey, S., and Gersonde, R. (2002). Past hydrographic and climatic changes in the Subantarctic Zone of the South Atlantic - the Pleistocene record from ODP Site 1090. Palaeogeogr. Palaeoclimatol. Palaeoecol. 182, 221-239.
11. Bollmann, J. (1997). Morphology and biogeography of the genus Gephyrocapsa coccoliths, in Holocene sediments. Mar. Micropaleontol. 29, 319-350.
12. Boyle, E. A. (1990). Quaternary deep water paleoceanography. Science 249, 863-887.
13. Broecker, W. S. (1982). Glacial to interglacial changes in ocean chemistry. Prog. Oceanogr. 11, 151-197.
14. Burckle, L. H. (1993). Late Quaternary interglacial stages warmer than present. Quat. Sci. Rev. 12, 825-831.
15. Charles, C. D., Froelich, P. N., Zibello, M. A., Mortlock, R. A., and Morley, J. J. (1991). Biogenic opal in Southern Ocean sediments over the last 450,000 years: implications for surface water chemistry and circulation. Paleoceanography 6, 697-728.
16. Coale,K. H., Johnson,K. S.,Fitzwater,S. E.,Gordon,R. M.,Tanner,S.,Chavez, F. P.,Ferioli,L.,Sakamoto,C.,Rogers, P., Millero, F., Steinberg, P., Nightingale, P., Cooper, D., Cochlan, W. P., Landry, M. R., Constantinou, J., Rollwagen, G., Trasvina, A., Kudela, R. (1996). A massive phytoplankton bloom induced by an ecosystemscale iron fertilization experiment in the equatorial Pacific. Nature 383, 495-501.
17. Coale, K. H., Kenneth, J. S., Chavez, F. P., Buesseler, K. O., Barber, Ri. T., Brzezinski, M. A., Cochlan, W. P., Millero, F. J., Falkowski, P. G., Bauer, J. E., Wanninkhof, R. H., Kudela, R. M.,Altabet, M. A., Hales, B. E., Takahashi, T., Landry, M. R., Bidigare, R. R., Wang, X., Chase, Z., Strutton, P. G., Friederich, G. E., Gorbunov, M. Y., Lance, V. P., Hilting, A. K., Hiscock, M. R., Demarest, M., Hiscock, W. T., Sullivan, K. F., Tanner, S. J., Gordon, R. M., Hunter, C. N., Elrod, V. A., Fitzwater, S. E., Jones, J. L., Tozzi, S., Koblizek, M., Roberts, A. E., Herndon, J., Brewster, J., Ladizinsky, N., Smith, G., Cooper, D., Timothy, D., Brown, S. L., Selph, K. E., Sheridan, C. C., Twining, B. S., and Johnson, Z. I. (2004). Southern Ocean iron enrichment experiment: carbon cycling in high- and low-Si waters. Science 304, 408-414.
18. Colman, A. S., and Holland, H. D. (2000). The global diagenetic flux of phosphorus from marine sediments to the oceans; redox sensitivity and the control of atmospheric oxygen levels: special publication. J. Sediment. Res. A Sediment. Petrol. Process 66, 53-75.
19. Cortese, J., and Abelmann, A. (2002). Radiolarian-based paleotemperatures during the last 160 kyrs at ODP Site 1089 (Southern Ocean, Atlantic Sector). Palaeogeogr. Palaeoclimatol. Palaeoecol. 182, 259-286.
20. Droxler, A. W., and Farrell, J. W. (2000). Marine Isotope Stage 11 (MIS 11): new insights for a warm future. Glob. Planet. Change 24, 1-5.
21. Droxler, A. W., Poore, P. Z., and Burckle, L. H. (2003). Earths Climate and Orbital Eccentricity: The Marine Isotope Stage 11 Question. Washington, DC: Geophysical Monograph, American Geophysical Union, 240.
22. Dymond,J.,Collier,R.,and McManus,J. (1997). Can the aluminum and titaniumcontentsof oceansedimentsbe used to determine the paleoproductivity of the oceans? Paleoceanography 12, 586-593.
23. Eagle, M., Paytan, A., Arrigo, K. R., van Dijken,G.,andMurray,R.W.(2003). A comparison between excess barium and barite as indicators of carbon export. Paleoceanography 18, 1021.
24. Elderfield, H., and Rickaby, R. E. M. (2000). Oceanic Cd/P ratio and nutrient utilization in the glacial Southern Ocean. Nature 405, 305-310.
25. Filippelli, G. M. (1997). Controls on phosphorus concentration and accumulation in oceanic sediments. Mar. Geol. 139, 231-240.
26. Filippelli, G. M., and Delaney, M. L. (1996). Phosphorus geochemistry of equatorial Pacific sediments. Geochim. Cosmochim. Acta 60, 1479-1495.
27. Filippelli, G. M., Latimer, J. C., Murray, R. W., and Flores, J. A. (2007). Productivity records from the Southern Ocean and the equatorial Pacific Ocean: testing the glacial shelfnutrient hypothesis. Deep Sea Res. Part IITop. Stud. Oceanogr. 54/21-22, 2443-2452.
28. Flores, J. A., Gersonde, R., and Sierro, F. J. (1999). Pleistocene fluctuations in the Agulhas Current Retroflection based on the calcareous plankton record. Mar. Micropaleontol. 37, 1-22.
29. Flores, J. A., Sierro, F. J., and Raffi, I. (1995). Evolution of the calcareous nannofossil assemblage as a response to the paleoceanographic changes in the Eastern equatorial Pacific from 4 to 2 Ma (Leg 138, Sites 849 and 852). Proc. ODP Init. Rep. 138, 163-176.
30. Flores, J.-A., Marino, M., Sierro, F. J., Hodell, D. A., and Charles, C. D. (2003). Calcareous plankton dissolution pattern and coccolithophore assemblages during the last 600 kyr at ODP Site 1089 (Cape Basin, South Atlantic): paleoceanographic implications. Palaeogeogr. Palaeoclimatol. Palaeoecol. 196, 409-426.
31. Flores, J. A., and Sierro, F. J. (1997). Revised technique for calculation of calcareous nannofossil accumulation rates. Micropaleontology 43, 321-324.
32. Föllmi, K. B. (1996). The phosphorus cycle, phosphogenesis and marine phosphate-rich deposits. Earth Sci. Rev. 40, 55-124.
33. Francois, R., Altabet, M. A., Yu, E. F., Sigman, D. M., Bacon, M. P., Frank, M., Bohrmann, G., Bareille, G., and Labeyrie, L. (1997). Contribution of Southern Ocean surfacewater stratification to low atmospheric CO2 concentrations during the last glacial period. Nature 389, 929-935.
34. Frank, M., Eisenhauer, A., Bonn, W. J., Walter, P., Grobe, H., Kubik, P. W., Dittrich-Hannen, B., and Mangini, A. (1995). Sediment redistribution versus paleoproductivity change: Weddell Sea margin sediment stratigraphy for the last 250,000 years deduced from 230Thex, 10Be and biogenic barium profiles. Earth Planet. Sci. Lett. 136, 559-573.
35. Giraudeau, J., and Bailey, G. W. (1995). Spatial dynamics of coccolithophore communities during an upwelling event in the Southern Benguela system. Cont. Shelf Res. 15, 1825-1852.
36. Gordon, R. M., Coale, K. H., and Johnson, K. S. (1997). Iron distributions in the equatorial Pacific: implications for new production. Limnol. Oceanogr. 42, 419-431.
37. Guidry, M. W., and Mackenzie, F. T. (2003). Experimental study of igneous and sedimentary apatite dissolution: control of pH, distance from equilibrium, and temperature on dissolution rates. Geochim. Cosmochim. Acta 67, 2949-2963.
38. Hernández-Almeida, I., Bárcena, M. A., Flores, J. A., Sierro, F. J., Sánchez-Vidal, A., and Calafat, A. (2011). Microplankton response to environmental conditions in the Alboran Sea (Western Mediterranean): one year sediment trap record. Mar. Micropaleontol. 78, 14-24.
39. Hodell, D., Kanfoush, S. L., Venz, K. A., Charles, C. D., and Sierro, F. J. (2003). "The mid-brunhestransition in ODP sites 1089 and 1090 (Subantarctic South Atlantic)," in: Marine Isotope Stage 11: An Extreme Interglacial? edsA.W. Droxler, R. Z. Poore, L. D. Burckle, and L. E. Osterman, 113-129. [American geophysical union geophysical monograph 137].
40. Hodell, D. A. (1993). Late Pleistocene paleoceanography of the South Atlantic sector of the Southern Ocean: ocean drilling program hole 704A. Paleoceanography 8, 47-67.
41. Hodell, D. A., Charles, C. D., Curtis, J. H., Mortyn, P. G., Ninnemann, U., and Venz, K. A. (2002)."Data report: oxygen isotope stratigraphy of ODP Leg 177 Sites 1088, 1089, 1090, 1093, and 1094,"in Proc. Ocean Drill. Prog. Sci. Results (College Station: Texas A&M), 177.
42. Hodell, D. A., Charles, C. D., and Ninnemann,U. (2000). Comparison of interglacial stages in the South Atlantic sector of the southern ocean for the past 450 kyr: implications for MarineIsotopeStage (MIS) 11. Glob. Planet. Change 24, 7-26.
43. Hodell, D. A., Charles, C. D., and Sierro, F. J. (2001). Late Pleistocene evolution of the oceans carbonate system. Earth Planet. Sci. Lett. 192, 109-124.
44. Howard, W. R., and Prell, W. L. (1992). Late quaternary surface circulation of the Southern Indian Ocean and its relationship to orbital variations. Paleoceanography 7, 79-117.
45. Ikehara, M., Kawamura, K., Ohkouchi, N., Murayama, M., Nakamura, T., and Taira, A. (2000). Variations of terrestrial input and marine productivity in the Southern Ocean (48°S) during the last two deglaciations. Paleoceanography 15, 170-180.
46. Imbrie, J., Hays, J. D., Martinson, D. G., McIntyre, A., Mix, A., Morley, J. J., Pisias, N. G., Prell, W. L., and Shackleton, N. J. (1984). "The orbital theory of Pleistocene climate: Support from a revised chronology of the marine δ18O record," in Milankovitch and Climate, Part I, eds A. Berger, J. Imbrie, J. Hays, G. Kukla, and B. Saltzman (Dordrecht: D. Reidel Publishing), 269-305.
47. Jansen, J. H. F., Kuijpers, A., and Troelstra, S. R. (1986). A Mid-Brunhes climatic event: long-term changes in Global Atmosphere and Ocean circulation. Science 233, 619-622.
48. Kleijne, A., Kroon, D., and Zevenboom, W. (1989). Phytoplankton and foraminiferal frequencies in Northern Indian Ocean and Red Sea surface waters. J. Sea Res. 24, 531-539.
49. Kuhn, G., and Diekmann, B. (2002). Late quaternary variability of ocean circulation in the southeastern South Atlantic inferred from the terrigenous sediment record of a drift deposit in the southern Cape Basin (ODP Site 1089). Palaeogeogr. Palaeoclimatol. Palaeoecol. 182, 287-303.
50. Kukla, G., McManus, J. F., Rousseau, D. D., and Chuine, I. (1998). How long and how stable was the last interglacial? Quat. Sci. Rev. 16, 605-612.
51. Kumar, N., Anderson, R. F., Mortlock, R. A., Froelich, P. N., Kubik, P., Dittrich-Hannen, B., and Suter, M. (1995). Increased biological productivity and export production in the glacial Southern Ocean. Nature 378, 675-680.
52. Latimer, J. C., and Filippelli, G. M. (2001). Terrigenous input and paleoproductivity in the Southern Ocean. Paleoceanography 16, 627-693.
53. Latimer, J. C., and Filippelli, G. M. (2003). Data report: sediment geochemical results from ODP Leg 189, Site 1171 - eocene to present. Proc. Ocean Drill. Prog. Sci. Results 189, 1-16.
54. Latimer, J. C., Filippelli, G. M., Hendy, I., Gleason, J. D., and Blum, J. D. (2006). Glacial-interglacial terrigenous provenance in the southeastern Atlantic Ocean: the importance of deep water sources and surface currents. Geology 34, 545-548.
55. Lea, D. W., and Boyle, E. A. (1990). Foraminiferal reconstructions of barium distributions in water masses of the glacial oceans. Paleoceanography 5, 719.
56. Lutjeharms, J. R. E. (1981). Spatial scales and intensities of circulation in the ocean areas adjacent to South Africa. Deep Sea Res. Part II Top. Stud. Oceanogr. 28, 1289-1302.
57. Lutjeharms, J. R. E. (1996). "The exchange of water between the South Indian and South Atlantic Oceans" in The South Atlantic: Present and Past Circulation, eds G. Wefer, W. H. Berger, G. Siedler, and D. J. Webb (Berlin: Springer), 125-162.
58. Lutjeharms, J. R. E., and Valentine, H. R. (1984). Southern Ocean thermal fronts along South Africa. Deep Sea Res. Part II Top. Stud. Oceanogr. 31, 1461-1475.
59. Mantyla, A. W., and Reid, J. L. (1983). Abyssal characteristics of the World Ocean waters. Deep Sea Res. Part II Top. Stud. Oceanogr. 30, 805-833.
60. Marcantonio, F., Kumar, N., Stute, M., Anderson, R. F., Seidl, M. A., Schlosser, P., and Mix, A. (1995). Comparative study of accumulation rates derived by He and Th isotopic analysis of marine sediments. Earth Planet. Sci. Lett. 133, 549-555.
61. Margalef, R. (1978). Life-forms of phytoplankton as survival alternatives in an unstable environment. Oceanol. Acta 1, 493-509.
62. Martinson, D. O., Pisias, N. G., Hayes, J. D., Imbrie, J., Moore, T. C. J., and Shackleton, N. J. (1987). Age dating and the orbital theory of the ice ages: development of a high resolution 0 to 300,000 year chronostratigraphy. Quaternary Res. 27, 1-29.
63. Mayer, L., Pisias, N., Janecek, T., Mix, A. C., Lyle, M. W., Arason, P., and Mosher, D. (1992). "Explanatory notes," in Proceedings of the Ocean Drilling Program, Scientific Results (College Station: Ocean Drilling Program), 13-42.
64. Molfino, B., and McIntyre, A. (1990). Nutricline variations in the Equatorial Atlantic coincident with theYounger-Dryas. Paleoceanography 5, 997-1008.
65. Moreno, A., Cacho, I., Canals, M., Grimalt, J. O., Sánchez-Goñi, M. F., Shackleton, N., and Sierro, F. J. (2005). Links between oscillation at the millennial time-scale. A multiproxy study of the last 50,000 from the Alboran Sea (Western Mediterranean Sea). Quat. Sci. Rev. 24, 1623-1636.
66. Moreno, A., Cacho, I., Canals, M., Prins, M. A., Sánchez-Goñi, M. F., Grimalt, J. O., and Weltje, G. J. (2002). Saharan dust transport and highlatitude glacial climatic variability: theAlboran Sea record. Quat. Int. 58, 318-328.
67. Mortlock, R. A., Charles, C. D., Froelich, P. N., Zibello, M. A., Saltzman, J., Hays, J. D., and Burckle, L. H. (1991). Evidence for lower productivity in the Antarctic Ocean during the last glaciations. Nature 351, 220-223.
68. Orsi, A. H., Whitworth, T., and Worth, N. (1995). On the meridional extent and fronts of the Antarctic Circumpolar current. Deep Sea Res. Part I Oceanogr. Res. Pap. 42, 641-673.
69. Peterson,R. G.,and Stramma,L. (1991). Upper-level circulation in the South Atlantic Ocean. Prog. Oceanogr. 26, 1-73.
70. Raymo, M. E., Oppo, D. W., Flower, B. P., Hodell, D. A., McManus, J., Venz, K. A., Kleiven, K. F., and McIntyre, K. (2004). Stability of North Atlantic water masses in face of pronounced climate variability during the Pleistocene. Paleoceanography 19, 2008-2021.
71. Reid, J. L., Nowlin, W. D., and Patzert, W. C. (1977). On the characteristics and circulation of the Southwestern Atlantic Ocean. J. Phys. Oceanogr. 7, 62-91.
72. Rodrigues, T., Grimalt, J., Abrantes, F., Flores, J. A., and Lebriero, S. M. (2009). Holocene interdependences of changes in sea surface temperature, productivity, and fluvial inputs in the Iberian continental shelf (Tagus mud patch). Geochem. Geophys. Geosyst.10, 10.1029/2008GC002367.
73. Rohling, E. J., Fenton, M., Jorissen, F. J., and Bertrand, P., Ganssen, G., Caulet, J. P. (1998). Magnitudes of sea-level lowstands of the past 500,000 years. Nature 394, 162-165.
74. Rühlemann, C., Mulitza, S., Muller, P. J., Wefer, G., and Zahn, R. (1999). Warming of the tropical Atlantic Ocean and slowdown of thermohaline circulation during the last deglaciation. Nature 402, 511-514.
75. Sañudo-Wilhelmy, S. A., Kustka, A. B., Gobler, C. J., Hutchins, D. A., Yang, M., Lwiza, K., Burns, J., Capone, D. G., Raven, J. A., and Carpenter, E. J. (2001). Phosphorus limitation of nitrogen fixation by Trichodesmium in Central Atlantic Ocean. Nature 411, 66-69.
76. Scherer, R. P., Aldahan, A., Tulaczyk, S., Kamb, B., Engelhardt, H., and Possnert, G. (1998). Pleistocene collapse of the West Antarctic Ice Sheet. Science 281, 82-85.
77. Shipboard Scientific Party. (1999). "Leg summary: Southern Ocean paleoceanography," in Proceedings of the Ocean Drilling Program, Initial Reports (College Station: Texas A&M), 1-101.
78. Siegenthaler, U., Stocker, T., Monnin, E., Luthi, D., Schwander, J., Stauffer, B., Raynaud, D., Barnola, J. M., Fischer, H., Masson-Delmotte, V., and Jouzel,J. (2005). Stable carbon cycleclimate relationship during the late Pleistocene. Science 310, 1313-1317.
79. Sigman, D. M., and Boyle, E. A. (2000). Glacial/interglacial variations in atmospheric carbon dioxide. Nature 407, 859-869.
80. Stoll, H. M., Rosenthal, Y., and Falkowski,P. (2002). Climate proxies from Sr/Ca of coccolith calcite: calibrations from continuousFlores et al. Coccolithophores and phosphorus cycling culture of Emiliania Huxley. Geochim. Cosmochim. Acta 66, 927-936.
81. Stoll, H. M., and Schrag, D. P. (2000). Coccolith Sr/Ca as a new indicator of coccolithophorid calcification and growth rate. Geochem. Geophys. Geosyst. 1, 1-24.
82. Tyrell, T. (1999). The relative influence of nitrogen and phosphorus on oceanic primary production. Nature 400, 525-527.
83. Wang, P., Tian, J., Cheng, X., Liu, C., and Xu, J. (2003). Carbon reservoir changes preceded major icesheet expansion at the Mid-Brunhes event. Geology 31, 239-242.
84. Watson, A. J., Bakker, D. C. E., Ridgwell, A. J., Boyd, P. W., and Law, C. S. (2002). Effect of iron supply on Southern Ocean CO2 uptake and implications for glacial atmospheric CO2. Nature 407, 730-733.
85. Wells, P., and Okada, H. (1997). Response of nannoplankton to major changes in sea-surface temperature and movements of hydrological fronts over Site DSDP 594 (South Chatham Rise, southeastern New Zealand), during the last 130 kyr. Mar. Micropaleontol. 32, 341-363.
86. Winter, A., Jordan, R. W., and Roth, P. H. (1994). "Biogeography of living coccolithophores in ocean waters," in Coccolithophores, eds A. Winter and W. G. Siesser (Cambridge: Cambridge University Press), 161-177.
87. Wu, J., Sunda, W., Boyle, E. A., and Karl, D. S. (2000). Phosphate depletion in the western North Atlantic Ocean. Science 289, 759-762.
88. Young, J. (1994). "Functions of coccoliths," in Coccolithophores, eds A. Winter and W. G. Siesser (Cambridge:CambridgeUniversityPress), 63-82.
89. Young, J. R., and Ziveri, P. (2000). Calculation of coccolith volume and its use in calibration of carbonate flux estimates. Deep Sea Res. Part II Top. Stud. Oceanogr. 47, 1679-1700.