Sensing Seasonality by Planktonic Foraminifera
Feldmeijer, W.
2015
document version
Publisher's PDF, also known as Version of record
Link to publication in VU Research Portal
citation for published version (APA)
Feldmeijer, W. (2015). Sensing Seasonality by Planktonic Foraminifera.
General rights
Copyright and moral rights for the publications made accessible in the public portal are retained by the authors and/or other copyright owners and it is a condition of accessing publications that users recognise and abide by the legal requirements associated with these rights. • Users may download and print one copy of any publication from the public portal for the purpose of private study or research. • You may not further distribute the material or use it for any profit-making activity or commercial gain
• You may freely distribute the URL identifying the publication in the public portal ? Take down policy
If you believe that this document breaches copyright please contact us providing details, and we will remove access to the work immediately and investigate your claim.
E-mail address:
Adelseck, C. G. (1977), Dissolution of deep-sea carbonate: preliminary calibration of preservational and morphologic aspects, Deep Sea Research, 24(12), 1167-1185.
Adelseck, C. G., and W. H. Berger (1975), On the dissolution of planktonic foraminifera and associated microfossils during settling and on the sea floor, Dissolution of deep sea
carbonates, 13, 70-81.
Adhemar, J. A. (1842), Revolutions de lamer, Privately published, Paris.
Adkins, J. F. (2013), The role of deep ocean circulation in setting glacial climates, Paleoceanography,
28(3), 539-561.
Adshead, P. C. (1967), Collection and laboratory maintenance of living planktonic foraminifera,
Micropaleontology, 13(1), 32-40.
Aldridge, D., C. J. Beer, and D. A. Purdie (2012), Calcification in the planktonic foraminifera
Globigerina bulloides linked to phosphate concentrations in surface waters of the North
Atlantic Ocean, Biogeosciences, 9(5), 1725-1739.
Alexandersson, E. T. (1976), Actual and anticipated petrographic effects of carbonate undersaturation in shallow seawater, Nature, 262(5570), 653-657.
Alldredge, A. L., and B. M. Jones (1973), Hastigerina pelagica: Foraminiferal habitat for planktonic dinoflagellates, Marine Biology, 22, 131-135.
Anand, P., H. Elderfield, and M. H. Conte (2003), Calibration of Mg/Ca thermometry in planktonic foraminifera from a sediment trap time series, Paleoceanography, 18, 1050.
Andersen, K. K., N. Azuma, J.-M. Barnola, M. Bigler, P. Biscaye, N. Caillon, J. Chappellaz, H. B. Clausen, D. Dahl-Jensen, and H. Fischer (2004), High-resolution record of Northern Hemisphere climate extending into the last interglacial period, Nature, 431(7005), 147-151.
Anderson, D. M., and W. L. Prell (1993), A 300 kyr record of upwelling off Oman during the late Quaternary: evidence of the Asian southwest monsoon, Paleoceanography, 8(2), 193-208. Anderson, L. A., and J. L. Sarmiento (1994), Redfield ratios of remineralization determined by
nutrient data analysis, Global biogeochemical cycles, 8(1), 65-80.
Anderson, O. R., M. Spindler, A. W. H. Be, and C. Hemleben (1979), Trophic activity of planktonic foraminifera, Journal of the Marine Biological Association of the UK, 59, 791-799. Anklin, M., J. M. Barnola, J. Beer, T. Blunier, J. Chappellaz, H. B. Clausen, D. Dahl-Jensen, W.
Dansgaard, M. De Angelis, and R. J. Delmas (1993), Climate instability during the last interglacial period recorded in the GRIP ice core, Nature, 364, 203-207.
Arbuszewski, J., P. B. deMenocal, A. Kaplan, and E. C. Farmer (2010), On the fidelity of shell-derived δ18O
seawater estimates, Earth and Planetary Science Letters, 300(3-4), 185-196.
Arrhenius, G. (1952), Sediment cores from the East Pacific: Swedish Deep-Sea Exped.(1947-1948) Repts., v. 5, fasc. 1, 89 p. 1963, Pelagic sediments in The Sea: New York, edited, Interscience.
Arz, H. W., J. Pätzold, and G. Wefer (1998), Correlated millennial-scale changes in surface hydrography and terrigenous sediment yield inferred from last-glacial marine deposits off northeastern Brazil, Quaternary Research, 50(2), 157-166.
Ashman, K. M., C. M. Bird, and S. E. Zepf (1994), Detecting bimodality in astronomical datasets,
Astron . J ., 108(6), 2348-2361.
Aurahs, R., G. W. Grimm, V. Hemleben, C. Hemleben, and M. Kucera (2009), Geographical distribution of cryptic genetic types in the planktonic foraminifer Globigerinoides ruber,
Molecular Ecology, 18(1692 – 1706).
Auras-Schudnagies, A., D. Kroon, G. M. Ganssen, C. Hemleben, and J. E. Van Hinte (1989), Distributional pattern of planktonic foraminifers and pteropods in surface waters and top core sediments of the Red Sea, and adjacent areas controlled by the monsoonal regime and other ecological factors, Deep Sea Research Part A . Oceanographic Research
Papers, 36(10), 1515-1533.
Balmaseda, M. A., K. Mogensen, and A. T. Weaver (2013), Evaluation of the ECMWF ocean reanalysis system ORAS4, Quarterly Journal of the Royal Meteorological Society, 139(674), 1132-1161.
Bandy, O. L. (1960a), General correlation of foraminiferal structure with environment, paper presented at International Geological Congress.
Bandy, O. L. (1960b), The geologic significance of coiling ratios in the foraminifer Globigerina
pachyderma (Ehrenberg)[California], Journal of Paleontology, 34(4), 671-681.
Bandy, O. L. (1968), Cycles in Neogene paleoceanography and eustatic changes, Palaeogeography,
Palaeoclimatology, Palaeoecology, 5(1), 63-75.
Bandy, O. L. (1972), Origin and development of Globorotalia (Turborotalia) pachyderma (Ehrenberg), Micropaleontology, 294-318.
Bandy, O. L., E. A. Butler, and R. C. Wright (1969), Alaskan upper Miocene marine glacial deposits and the Turborotalia pachyderma datum plane, Science, 166(3905), 607-609.
Bard, E. (2001), Paleoceanographic implications of the difference in deep-sea sediment mixing between large and fine particles, Paleoceanography, 16(3), 235-239.
Bard, E., M. Arnold, J. Duprat, J. Moyes, and J.-C. Duplessy (1987a), Reconstruction of the last deglaciation: deconvolved records of δ18O profiles, micropaleontological variations and
accelerator mass spectrometric 14C dating, Climate Dynamics, 1(101-112).
Bard, E., M. Arnold, P. Maurice, J. Duprat, J. Moyes, and J.-C. Duplessy (1987b), Retreat velocity of the North Atlantic polar front during the last deglaciation determined by 14C accelerator
mass spectrometry, Nature, 328(6133), 791-794.
Barker, S., and H. Elderfield (2002), Foraminiferal Calcification Response to Glacial-Interglacial Changes in Atmospheric CO2, Science, 297(5582), 833-836.
Barker, S., M. Greaves, and H. Elderfield (2003), A study of cleaning procedures used for foraminiferal Mg/Ca paleothermometry, Geochem . Geophys . Geosyst ., 4(9), 8407. Barker, S., I. Cacho, H. Benway, and K. Tachikawa (2005), Planktonic foraminiferal Mg/Ca as a
proxy for past oceanic temperatures: a methodological overview and data compilation for the Last Glacial Maximum, Quaternary Science Reviews, 24(7), 821-834.
Barker, S., W. S. Broecker, E. Clark, and I. Hajdas (2007), Radiocarbon age offsets of foraminifera resulting from differential dissolution and fragmentation within the sedimentary bioturbated zone, Paleoceanography, 22(2).
Bartels-Jónsdóttir, H. B., K. L. Knudsen, F. Abrantes, S. Lebreiro, and J. Eiríksson (2006), Climate variability during the last 2000 years in the Tagus Prodelta, western Iberian Margin: Benthic foraminifera and stable isotopes, Marine Micropaleontology, 59(2), 83-103. Basak, C., A. E. Rathburn, M. E. Pérez, J. B. Martin, J. W. Kluesner, L. A. Levin, P. De Deckker, J.
M. Gieskes, and M. Abriani (2009), Carbon and oxygen isotope geochemistry of live (stained) benthic foraminifera from the Aleutian Margin and the Southern Australian Margin, Marine Micropaleontology, 70(3-4), 89-101.
Bauch, H. A. (1997), Paleoceanography of the North Atlantic Ocean (68–76 N) during the past 450 ky deduced from planktic foraminiferal assemblages and stable isotopes, Contributions
to the Micropaleontology and Paleoceanography of the Northern North Atlantic, 5, 83-100.
1
2
3
4
5
6
7
8
9
R & A
Bé, A. W. H. (1960), Ecology of Recent planktonic foraminifera: Part 2 - Bathymetric and seasonal distributions in the Sargasso Sea off Bermuda, Micropaleontology, 6(4), 373-392.
Bé, A. W. H. (1969), Planktonic Foraminifera, in Distribution of Selected Groups of Marine
Invertebrates in Waters South of 35°S latitude, edited, pp. 9-12, American Geographical
Society.
Bé, A. W. H. (1977), An ecological, zoogeographic, and taxonomic review of recent Planktonic Foraminifera, in Oceanic Micropalaeontology, edited by A. T. S. Ramsay, pp. 1-100, Academic Press, London.
Bé, A. W. H. (1980), Gametogenic calcification in a spinose planktonic foraminifer Globigerinoides
sacculifer (Brady), Marine Micropaleontology, 5, 283-310.
Bé, A. W. H. (1982), Biology of planktonic foraminifera.
Bé, A. W. H., and D. B. Ericson (1963), Aspects of calcification in planktonic foraminifera (Sarcodina)*, Annals of the New York Academy of Sciences, 109(1), 65-81.
Bé, A. W. H., and L. Lott (1964), Shell growth and structure of planktonic foraminifera, Science,
145(3634), 823-824.
Bé, A. W. H., and D. S. Tolderlund (1971), Distribution and ecology of living planktonic foraminifera in surface waters of the Atlantic and Indian Oceans, in Micropaleontology
of Oceans, edited by B. M. Funnell and W. R. Riedel, pp. 105-149, Cambridge University
Press, London.
Bé, A. W. H., and O. R. Anderson (1976), Preservation of planktonic foraminifera and other calcareous plankton, in Zooplankton fixation and preservation, edited by H. J. Steedman, pp. 250-258, UNESCO Press, Paris.
Bé, A. W. H., and W. H. Hutson (1977), Ecology of planktonic foraminifera and biogeographic patterns of life and fossil assemblages in the Indian Ocean, Micropaleontology, 23(369-414).
Bé, A. W. H., A. McIntyre, and D. L. Breger (1966), Shell Microstructure of a Planktonic Foraminifer,
Globorotalia menardii (d’Orbigny), Eclogae geologicae Helvetiae, 59(2), 885-896.
Bé, A. W. H., J. M. Forns, and O. A. Roels (1971), Plankton abundance in the North Atlantic Ocean, in Fertility of the Sea, edited by J. D. Costlow, pp. 17-50, Gordon and Breach Science Publishers, New York.
Bé, A. W. H., S. M. Harrison, and L. Lott (1973), Orbulina universa d’Orbigny in the Indian Ocean. , Micropaleontology 19, 150-192
Bé, A. W. H., J. W. Morse, and S. M. Harrison (1975), Progressive dissolution and ultrastructural breakdown of planktonic foraminifera, in Special Publication: Dissolution of
Deep-Sea carbonates edited by W. Sliter, A. W. H. Bé and W. H. Berger, pp. 27-55, Cushman
Foundation of Foraminiferal Research.
Bé, A. W. H., D. A. Caron, and O. R. Anderson (1981), Effects of feeding frequency on life processes of the planktonic foraminifer Globigerinoides sacculifer in laboratory culture, Journal of
the Marine Biological Association of the UK, 61, 257-277.
Bé, A. W. H., C. Hemleben, O. R. Anderson, and M. Spindler (1979), Chamber formation in planktonic foraminifera, Micropaleontology, 25, 294-307.
Bé, A. W. H., J. K. B. Bishop, M. S. Sverdlove, and W. D. Gardner (1985), Standing stock, vertical distribution and flux of planktonic foraminifera in the Panama Basin, Marine
Micropaleontology, 9(4), 307-333.
Bé, A. W. H., C. Hemleben, O. R. Anderson, M. Spindler, J. Hacunda, and S. Tuntivate-Choy (1977), Laboratory and field observations of living planktonic foraminifera, Micropaleontology,
23(2), 155-179.
Bemis, B. E., H. J. Spero, J. Bijma, and D. W. Lea (1998), Reevaluation of the Oxygen Isotopic Composition of Planktonic Foraminifera: Experimental Results and Revised Paleotemperature Equations, Paleoceanography, 13(2), 150-160.
isotopic composition of Globigerina bulloides and Orbulina universa (planktonic foraminifera), Marine Micropaleontology, 38(3), 213-228.
Berger, A., J. L. Mélice, and M.-F. Loutre (2005), On the origin of the 100‐kyr cycles in the astronomical forcing, Paleoceanography, 20(4).
Berger, A., M. F. Loutre, and J. L. Mélice (2006), Equatorial insolation: from precession harmonics to eccentricity frequencies, Climate of the Past, 2(2), 131-136.
Berger, W. H. (1967), Foraminiferal ooze: solution at depths, Science, 156(3773), 383-385.
Berger, W. H. (1968), Planktonic foraminifera: selective solution and paleoclimatic interpretation, paper presented at Deep Sea Research and Oceanographic Abstracts, Elsevier.
Berger, W. H. (1969), Ecologic patterns of living planktonic Foraminifera, Deep Sea Research and
Oceanographic Abstracts, 16(1), 1-24.
Berger, W. H. (1970a), Biogenous deep-sea sediments: fractionation by deep-sea circulation,
Geological Society of America Bulletin, 81(5), 1385-1402.
Berger, W. H. (1970b), Planktonic foraminifera: selective solution and the lysocline, Marine
Geology, 8, 111-138.
Berger, W. H. (1970c), Planktonic Foraminfera: differential production and expatriation off Baja California, Limnology and Oceanography, 15, 183-204.
Berger, W. H. (1971), Sedimentation of planktonic foraminifera, Marine Geology, 11, 325-358. Berger, W. H. (1972), Deep sea carbonates: dissolution facies and age-depth constancy.
Berger, W. H. (1973), Deep-sea carbonates: evidence for a coccolith lysocline, Deep-Sea Research,
20, 917-921.
Berger, W. H. (1975a), Deep-sea carbonates: dissolution profiles from foraminiferal preservation,
Cushman Foundation for Foraminiferal Research Special Publication, 13, 82-86.
Berger, W. H. (1975b), Dissolution of deep-sea carbonates: an introduction, Cushman Foundation for Foraminiferal Research Special Publication.
Berger, W. H. (1978), Oxygen-18 stratigraphy in deep-sea sediments: additional evidence for the deglacial meltwater effect, Deep Sea Research, 25(5), 473-479.
Berger, W. H. (1979a), Preservation of foraminifera, paper presented at SEPM Short Course: Foraminferal Ecology and Paleoecology, SEPM, Houston.
Berger, W. H. (1979b), Stable isotopes in foraminifera.
Berger, W. H. (1981), Paleoceanography: The deep-sea record, The Oceanic Lithosphere, The Sea, 7 C. Emiliani, 1437–1517, edited, John Wiley, New York.
Berger, W. H. (1992), Pacific carbonate cycles revisited: Arguments for and against productivity control, in Centenary of Japenese Micropaleontology, edited by K. Izhizaki and T. Saito, pp. 15-25, Terra Scientific Publishing Company, Tokyo.
Berger, W. H. (1999), The 100-kyr ice-age cycle: internal oscillation or inclinational forcing?,
International Journal of Earth Sciences, 88(2), 305-316.
Berger, W. H. (2008), Sea level in the late Quaternary: patterns of variation and implications,
International Journal of Earth Sciences, 97(6), 1143-1150.
Berger, W. H. (2013), On the Milankovitch sensitivity of the Quaternary deep-sea record, Climate
of the Past, 9(4), 2003-2011.
Berger, W. H., and G. R. Heath (1968), Vertical mixing in pelagic sediments, J . mar . Res, 26(2), 134-143.
Berger, W. H., and D. J. W. Piper (1972), Planktonic foraminifera: differential settling, dissolution and redeposition., Limnology and Oceanography, 17, 275-287.
Berger, W. H., and E. L. Winterer (1974), Plate stratigraphy and the fluctuating carbonate line,
Pelagic sediments: on land and under the sea, 11-48.
Berger, W. H., and J. V. Gardner (1975), On the determination of Pleistocene temperature from planktonic foraminifera, The Journal of Foraminiferal Research, 5(2), 102-113.
1
2
3
4
5
6
7
8
9
R & A
Berger, W. H., and E. Vincent (1986), Deep-sea carbonates: reading the carbon-isotope signal,
Geologische Rundschau, 75(1), 249-269.
Berger, W. H., and E. Jansen (1995), Younger Dryas episode: ice collapse and super fjord heat pump, in The Younger Dryas edited by S. R. Troelstra, J. E. Van Hinte and G. M. Ganssen, pp. 61-106, Koninklijke Nederlandse Akademie van Wetenschappen, Amsterdam.
Berger, W. H., R. F. Johnson, and J. S. Killingley (1977), `Unmixing’ of the deep-sea record and the deglacial meltwater spike, Nature, 269(5630), 661-663.
Berger, W. H., L. Diesterhaass, and J. S. Killingley (1978a), Upwelling off northwest africa-holocene decrease as seen in carbon isotopes and sedimentological indicators, Oceanologica Acta,
1(1), 3-7.
Berger, W. H., J. S. Killingley, and E. Vincent (1978b), Stable isotopes in deep-sea carbonates-box core erdc-92, west equatorial pacific, Oceanologica Acta, 1(2), 203-216.
Berger, W. H., J. S. Killingley, and E. Vincent (1978c), Stable isotopes in deep-sea carbonates: Box Core ERDC-92, west equatorial Pacific, Oceanological Acta, 1, 203-216.
Berger, W. H., M. C. Bonneau, and F. L. Parker (1982), Foraminifera on the deep-sea floor-lysocline and dissolution rate, Oceanologica Acta, 5(2), 249-258.
Berggren, W. A., D. V. Kent, J. J. Flynn, and J. A. Van Couvering (1985), Cenozoic geochronology,
Geological Society of America Bulletin, 96(11), 1407-1418.
Bian, N., and P. A. Martin (2010), Investigating the fidelity of Mg/Ca and other elemental data from reductively cleaned planktonic foraminifera, Paleoceanography, 25(2), PA2215.
Bijma, J., W. W. Faber, and C. Hemleben (1990), Temperature and salinity limits for growth and survival of some planktonic foraminifers in laboratory cultures, Journal of Foraminiferal
Research, 20(2), 95-116.
Bijma, J., H. J. Spero, and D. W. Lea (1999a), Reassessing foraminiferal stable isotope geochemistry: Impact of the oceanic carbonate system (experimental results), in Use of proxies in
paleoceanography, edited, pp. 489-512, Springer.
Bijma, J., H. J. Spero, and D. W. Lea (1999b), Reassessing foraminiferal stable isotope geochemistry: Impacts of the oceanic carbonate system (Experimental results), in Use of Proxies in
Paleoceanography: Examples from the South Atlantic edited by G. Fischer and G. Wefer,
pp. 489-512, Springer-Verlag, Berlin Heidelberg.
Bijma, J., B. Hönisch, and R. E. Zeebe (2002), Impact of the ocean carbonate chemistry on living foraminiferal shell weight: Comment on “Carbonate ion concentration in glacial-age deep waters of the Caribbean Sea” by W. S. Broecker and E. Clark, Geochem . Geophys .
Geosyst ., 3(11), 1064.
Bijma, J., C. Hemleben, H. Oberhaensli, and M. Spindler (1992), The effects of increased water fertility on tropical spinose planktonic foraminifers in laboratory cultures, Journal of
Foraminiferal Research, 22(3), 242-256.
Billups, K., and H. J. Spero (1995), Relationship between shell size, thickness and stable isotopes in individual planktonic foraminifera from two equatorial Atlantic cores, Journal of
Foraminiferal Research, 25(1), 24-37.
Bintanja, R., and R. S. W. van de Wal (2008), North American ice-sheet dynamics and the onset of 100,000-year glacial cycles, Nature, 454(7206), 869-872.
Birch, H., H. K. Coxall, P. N. Pearson, D. Kroon, and M. O’Regan (2013), Planktonic foraminifera stable isotopes and water column structure: Disentangling ecological signals, Marine
Micropaleontology, 101, 127-145.
Bishop, J. K. B., D. R. Ketten, and J. M. Edmond (1978), The chemistry, biology and vertical flux of particulate matter from the upper 400 m of the Cape Basin in the southeast Atlantic Ocean, Deep Sea Research, 25(12), 1121-1161.
Bloom, A. L., W. S. Broecker, J. M. A. Chappell, R. K. Matthews, and K. J. Mesolella (1974), Quaternary sea level fluctuations on a tectonic coast: New 230Th/234U dates from the Huon
Blunier, T., and E. J. Brook (2001), Timing of millennial-scale climate change in Antarctica and Greenland during the last glacial period, Science, 291(5501), 109-112.
Boiseau, M., and A. Juillet-Leclerc (1997), H2O2 treatment of recent coral aragonite: oxygen and carbon isotopic implications, Chemical Geology, 143(3-4), 171-180.
Bolli, H. M. (1950), The direction of coiling in the evolution of some Globorotaliidae, Contributions
from the Cushman Foundation for Foraminiferal Research, 1, 82-89.
Bolli, H. M. (1951), Notes on the direction of coiling of rotalid Foraminifera.
Bolli, H. M., J. B. Saunders, and K. Perch-Nielsen (1989), Plankton Stratigraphy: Volume 1, Planktic
Foraminifera, Calcareous Nannofossils and Calpionellids, CUP Archive.
Bolton, A., and J. P. Marr (2013), Trace element variability in crust-bearing and non crust-bearing
Neogloboquadrina incompta, P–D intergrade and Globoconella inflata from the Southwest
Pacific Ocean: Potential paleoceanographic implications, Marine Micropaleontology, 100, 21-33.
Bolton, A., J. A. Baker, G. B. Dunbar, L. Carter, E. G. C. Smith, and H. L. Neil (2011), Environmental versus biological controls on Mg/Ca variability in Globigerinoides ruber (white) from core top and plankton tow samples in the southwest Pacific Ocean, Paleoceanography,
26(2), 21-33.
Boltovskoy, E. (1959), Foraminifera as biological indicators in the study of ocean currents,
Micropaleontology, 473-481.
Boltovskoy, E. (1962), Planktonic foraminifera as indicators of different water masses in the South Atlantic, Micropaleontology, 403-408.
Boltovskoy, E. (1964), Seasonal occurrences of some living foraminifera in Puerto Deseado (Patagonia, Argentina), Journal du Conseil, 29(2), 136-145.
Boltovskoy, E. (1966a), Methods for sorting of foraminifera from plankton samples, Journal of
Paleontology, 1244-1246.
Boltovskoy, E. (1966b), Depth at which foraminifera can survive in sediments, Contributions from
the Cushman Foundation for Foraminiferal Research, 17, 43, 45.
Boltovskoy, E. (1969), Living planktonic foraminifera at the 90 E meridian from the equator to the Antarctic, Micropaleontology, 237-255.
Boltovskoy, E. (1971), Planktonic foraminiferal assemblages of the epipelagic zone their thanatocoenoses, in Micropaleontology of the Oceans, edited by B. M. Funnell and W. R. Riedel, pp. 277-288, Cambridge University Press, Cambridge.
Bond, G. C., W. S. Broecker, S. Johnsen, J. McManus, L. Labeyrie, J. Jouzel, and G. Bonani (1993), Correlations between climate records from North Atlantic sediments and Greenland ice,
Nature, 365(6442), 143-147.
Bond, G. C., W. Showers, M. Elliot, M. Evans, R. Lotti, I. Hajdas, G. Bonani, and S. Johnson (1999), The North Atlantic’s 1‐2 Kyr Climate Rhythm: Relation to Heinrich Events, Dansgaard/ Oeschger Cycles and the Little Ice Age, Mechanisms of global climate change at millennial
time scales, 35-58.
Böning, P., and E. Bard (2009), Millennial/centennial-scale thermocline ventilation changes in the Indian Ocean as reflected by aragonite preservation and geochemical variations in Arabian Sea sediments, Geochimica et Cosmochimica Acta, 73(22), 6771-6788.
Bonneau, M.-C., C. Vergnaud-Grazzini, and W. H. Berger (1980), Stable isotope fractionation and differential dissolution in recent planktonic foraminifera from Pacific box-cores,
Oceanological Acta, 3(3), 377-382.
Bouvier-Soumagnac, Y., and Y. Duplessy (1985), Carbon and oxygen isotopic composition of planktonic foraminifera from laboratory culture, plankton tows and recent sediment: implications for the reconstruction of paleoclimatic conditions and of the global carbon cycle, Journal of Foraminiferal Research, 15(4), 302-320.
Bradshaw, J. S. (1959), Ecology of living planktonic foraminifera in the north and equatorial Pacific
1
2
3
4
5
6
7
8
9
R & A
Brady, H. B. (1884), Report on the Foraminifera dredged by H.M.S. Challenger during the years 1873-1876, Report of the scientific results of the voyage of H .M .S . Challenger, 1873-1876,
Zoology,, 9, 1-814.
Bramlette, M. N. (1961), Pelagic sediments, Oceanography, 67, 345-366.
Bramlette, M. N., and W. H. Bradley (1940), Geology and biology of North Atlantic deep-sea cores,
U .S . Geological Survey Professional Papers, 196-A, 1-34.
Bramlette, M. N., and W. H. Bradley (1942), Lithology and geological interpretations; Geology and biology of North Atlantic deep-sea cores: US Geol, Survey, Prof . Paper, 196, 1-34. Brassell, S. C., G. Eglinton, I. T. Marlowe, U. Pflaumann, and M. Sarnthein (1986), Molecular
stratigraphy: a new tool for climatic assessment, Nature, 320(6058), 129-133.
Broecker, W., and E. Clark (2004), Shell weights from the South Atlantic, Geochemistry Geophysics
Geosystems, 5(3).
Broecker, W., G. Bond, M. Klas, E. Clark, and J. McManus (1992), Origin of the northern Atlantic’s Heinrich events, Climate Dynamics, 6(3-4), 265-273.
Broecker, W. S. (1966), Absolute dating and the astronomical theory of glaciation, Science,
151(3708), 299-304.
Broecker, W. S. (1987), The biggest chill.
Broecker, W. S. (1994), Massive iceberg discharges as triggers for global climate change, Nature,
372, 421-424.
Broecker, W. S., and J. Donk (1970), Insolation changes, ice volumes, and the O18 record in deep‐sea
cores, Reviews of Geophysics, 8(1), 169-198.
Broecker, W. S., and G. H. Denton (1989), The role of ocean-atmosphere reorganizations in glacial cycles, Geochimica et Cosmochimica Acta, 53(10), 2465-2501.
Broecker, W. S., and E. Clark (2001), An evaluation of Lohmann’s Foraminifera Weight Dissolution Index, Paleoceanography, 16(5), 531-534.
Broecker, W. S., and E. Clark (2002), Carbonate ion concentration in glacial-age deep waters of the Caribbean Sea, Geochem . Geophys . Geosyst ., 3(3), 1021.
Broecker, W. S., and E. Clark (2003), Holocene atmospheric CO2 increase as viewed from the seafloor, Global Biogeochem . Cycles, 17(2), 1052.
Broecker, W. S., S. Sutherland, and T.-H. Peng (1999), A possible 20th-century slowdown of Southern Ocean deep water formation, Science, 286(5442), 1132-1135.
Broecker, W. S., G. C. Bond, M. Klas, G. Bonani, and W. Wolfli (1990), A salt oscillator in the glacial Atlantic? 1. The concept, Paleoceanography, 5(4), 469-477.
Broecker, W. S., M. Andree, W. Wolfli, H. Oeschger, G. Bonani, J. P. Kennett, and D. Peteet (1988), The chronology of the last deglaciation: Implications to the cause of the Younger Dryas event, Paleoceanography, 3(1), 1-19.
Broerse, A. T. C., P. Ziveri, J. E. van Hinte, and S. Honjo (2000), Coccolithophore export production, species composition, and coccolith-CaCO3 fluxes in the NE Atlantic (34°N 21°W and 48°N 21°W), Deep Sea Research Part II: Topical Studies in Oceanography, 47(9), 1877-1905.
Brown, S. J., and H. Elderfield (1996), Variations in Mg/Ca and Sr/Ca ratios of planktonic foraminifera caused by postdepositional dissolution: Evidence of shallow Mg-dependent dissolution, Paleoceanography, 11, 543–551.
Brummer, G.-J. A., and D. Kroon (1988), Genetically controlled planktonic foraminiferal coiling ratios as tracers of past ocean dynamics, Planktonic foraminifers as tracers of
ocean-climate history, 293-298.
Brummer, G.-J. A., C. Hemleben, and M. Spindler (1986), Planktonic foraminiferal ontogeny and new perspectives for micropalaeontology, Nature Publishing Group.
Cacho, I., J. O. Grimalt, C. Pelejero, M. Canals, F. J. Sierro, J. A. Flores, and N. J. Shackleton (1999), Dansgaard‐Oeschger and Heinrich event imprints in Alboran Sea paleotemperatures,
Paleoceanography, 14(6), 698-705.
Cai, W., and R. J. Greatbatch (1995), Compensation for the NADW outflow in a global ocean general circulation model, Journal of physical oceanography, 25(2), 226-241.
Caley, T., J. Giraudeau, B. Malaizé, L. Rossignol, and C. Pierre (2012), Agulhas leakage as a key process in the modes of Quaternary climate changes, Proceedings of the National Academy
of Sciences, 109(18), 6835-6839.
Caron, D. A., A. W. H. Be, and A. O.R. (1981), Effects of variations in light intensity on life processes of the planktonic foraminifera Globigerinoides sacculifer in laboratory culture, Journal of
the Marine Biological Association of the UK, 62, 435-451.
Carpenter, W. B., W. K. Parker, and T. R. Jones (1862), Introduction to the study of the Foraminifera, Ray society.
Carstens, J., and G. Wefer (1992), Recent distribution of planktonic foraminifera in the Nansen Basin, Arctic Ocean, Deep Sea Research Part A . Oceanographic Research Papers, 39(2), S507-S524.
Channell, J. E. T., D. A. Hodell, and J. H. Curtis (2012), ODP Site 1063 (Bermuda Rise) revisited: oxygen isotopes, excursions and paleointensity in the Brunhes Chron, Geochemistry,
Geophysics, Geosystems, 13(2).
Chapman, M. R. (2010), Seasonal production patterns of planktonic foraminifera in the NE Atlantic Ocean: Implications for paleotemperature and hydrographic reconstructions,
Paleoceanography, 25(1).
Chappell, J., and N. J. Shackleton (1986), Oxygen isotopes and sea level, Nature, 324(6093), 137-140.
Chappell, J. M. A. (1973), Astronomical theory of climatic change: status and problem, Quaternary
Research, 3(2), 221-236.
Charles, C. D., and R. G. Fairbanks (1992), Evidence from Southern Ocean sediments for the effect of North Atlantic deep-water flux on climate, Nature, 355, 416-419.
Charney, J. G., and A. Eliassen (1949), A numerical method for predicting the perturbations of the middle latitude westerlies, Tellus, 1(2), 38-54.
Chen, M.-T., H.-W. Ho, T.-D. Lai, L. Zheng, Q. Miao, K.-S. Shea, M.-P. Chen, P. Wang, K.-Y. Wei, and C.-Y. Huang (1998), Recent planktonic foraminifers and their relationships to surface ocean hydrography of the South China Sea, Marine Geology, 146(1), 173-190.
Cheng, H., R. L. Edwards, W. S. Broecker, G. H. Denton, X. Kong, Y. Wang, R. Zhang, and X. Wang (2009), Ice age terminations, Science, 326(5950), 248-252.
Chiessi, C. M., S. Ulrich, S. Mulitza, J. Pätzold, and G. Wefer (2007), Signature of the Brazil-Malvinas Confluence (Argentine Basin) in the isotopic composition of planktonic foraminifera from surface sediments, Marine Micropaleontology, 64(1), 52-66.
Chiessi, C. M., S. Mulitza, A. Paul, J. Pätzold, J. Groeneveld, and G. Wefer (2008), South Atlantic interocean exchange as the trigger for the Bølling warm event, Geology, 36(12), 919-922. Cifelli, R. (1961), Globigerina incompta, a new species of pelagic foraminfera from the North
Atlantic, Contributions from the Cushman Foundation for Foraminiferal Research, 12(3), 83-86.
Cifelli, R. (1962), Some dynamic aspects of the distribution of planktonic foraminifera in the western North Atlantic, Journal of Marine Research, 20(3), 201-213.
Cifelli, R. (1965), Planktonic foraminifera from the western North Atlantic, 36 pp., Smithsonian Institution, Washington.
Cifelli, R. (1967), Distributional analysis of North Atlantic Foraminifera collected in 1961 during
Cruises 17 and 21 of the R/V Chain, Woods Hole Oceanographic Institution.
1
2
3
4
5
6
7
8
9
R & A
edited by J. Gray and A. J. Boucot, pp. 417-425, Oregon State University Press, Oregon. Cifelli, R. (1982), Textural Observations on Some Living Species of Planktonic Foraminifera,
Smithsonian Contributions to Paleobiology, 45, 1-45.
Cifelli, R., and R. K. Smith (1970), Distribution of Planktonic Foraminifera in the Vicinity of the North Atlantic Current, Smithsonian Contributions to Paleobiology, 4, 51p.
Cifelli, R., and R. K. Smith (1974), Distributional patterns of planktonic foraminifera in the western North Atlantic, The Journal of Foraminiferal Research, 4(3), 112-125.
Cifelli, R., and C. S. Benier (1976), Planktonic foraminifera from near the West African coast and a consideration of faunal parcelling in the North Atlantic, The Journal of Foraminiferal
Research, 6(4), 258-273.
Clark, P. U., N. G. Pisias, T. F. Stocker, and A. J. Weaver (2002), The role of the thermohaline circulation in abrupt climate change, Nature, 415(6874), 863-869.
Claussen, M., J. Fohlmeister, A. Ganopolski, and V. Brovkin (2006), Vegetation dynamics amplifies precessional forcing, Geophysical Research Letters, 33(9).
Cléroux, C., E. Cortijo, J.-C. Duplessy, and R. Zahn (2007), Deep-dwelling foraminifera as thermocline temperature recorders, Geochemistry, Geophysics, Geosystems, 8(4), Q04N11. Cléroux, C., E. Cortijo, P. Anand, L. Labeyrie, F. Bassinot, N. Caillon, and J.-C. Duplessy (2008),
Mg/Ca and Sr/Ca ratios in planktonic foraminifera: Proxies for upper water column temperature reconstruction, Paleoceanography, 23(3), PA3214.
Coadic, R., F. Bassinot, D. Dissard, E. Douville, M. Greaves, and E. Michel (2013), A core‐top study of dissolution effect on B/Ca in Globigerinoides sacculifer from the tropical Atlantic: Potential bias for paleo‐reconstruction of seawater carbonate chemistry, Geochemistry,
Geophysics, Geosystems, 14(4), 1053-1068.
Conan, S. M. H., and G.-J. A. Brummer (2000), Fluxes of planktic foraminifera in response to monsoonal upwelling on the Somalia Basin margin, Deep Sea Research Part II: Topical
Studies in Oceanography, 47(9-11), 2207-2227.
Conan, S. M. H., E. M. Ivanova, and G.-J. A. Brummer (2002), Quantifying carbonate dissolution and calibration of foraminiferal dissolution indices in the Somali Basin, Marine Geology,
182(3-4), 325-349.
Conolly, J. R., and M. Ewing (1965), Ice-rafted detritus as a climatic indicator in Antarctic deep-sea cores, Science, 150(3705), 1822-1824.
Coulbourn, W. T., F. L. Parker, and W. H. Berger (1980), Faunal and solution patterns of planktonic foraminifera in surface sediments of the North Pacific, Marine Micropaleontology, 5, 329-399.
Cox, P. M., R. A. Betts, C. D. Jones, S. A. Spall, and I. J. Totterdell (2000), Acceleration of global warming due to carbon-cycle feedbacks in a coupled climate model, Nature, 408(6809), 184-187.
Cox, P. M., D. Pearson, B. B. Booth, P. Friedlingstein, C. Huntingford, C. D. Jones, and C. M. Luke (2013), Sensitivity of tropical carbon to climate change constrained by carbon dioxide variability, Nature, 494(7437), 341-344.
Cramer, B. S., K. G. Miller, P. J. Barrett, and J. D. Wright (2011), Late Cretaceous–Neogene trends in deep ocean temperature and continental ice volume: reconciling records of benthic foraminiferal geochemistry (δ18O and Mg/Ca) with sea level history, Journal of
Geophysical Research: Oceans (1978–2012), 116(C12).
Croll, J. (1875), ``Climate and Time’’, Nature, 12, 329.
Curry, W. B., and R. Matthews (1981), Equilibrium 18O fractionation in small size fraction planktonic
foraminifera:evidence from recent Indian Ocean sediments, Marine Micropaleontology,
6, 327-337.
Curry, W. B., and R. K. Matthews (1981), Equilibrium 18O fractionation in small size fraction planktic
foraminifera: evidence from recent Indian Ocean sediments, Marine Micropaleontology,
Curry, W. B., D. R. Ostermann, M. V. S. Guptha, and V. Ittekkot (1992), Foraminiferal production and monsoonal upwelling in the Arabian Sea: evidence from sediment traps, Geological
Society, London, Special Publications, 64(1), 93-106.
Cushman, J. A., and L. G. Henbest (1940), Geology and biology of North Atlantic deep-sea cores between Newfoundland and Ireland. Part 2. Foraminifera, US Geol . Survey, Prof .
Paper(196-A), 35-50.
d’Orbigny, A. D. (1826a), Tableau méthodique de la classe des Céphalopodes, Crochard.
d’Orbigny, A. D. (1826b), Tableu méthodique de la classe des Cephalopodes, Annales de Sciences
Naturelles, 1, 96-169 & 245-314.
d’Orbigny, A. D. (1839a), Foraminiferes des tles Canaries, Barker-Webb, P . & Berthelot, S ., Histoire
naturelle des Tles Canaries, tome, 2.
d’Orbigny, A. D. (1839b), Foraminifers in Raman de la Sagra: Hisforire physique, politique et naturelle de lile de Cuba, edited, Paris.
Dansgaard, W., et al. (1993), Evidence for general instability of past climate from a 250-kyr ice-core record, Nature, 364(6434), 218-220.
Darling, K. F., C. M. Wade, D. Kroon, and A. J. L. Brown (1997), Planktic foraminiferal molecular evolution and their polyphyletic origins from benthic taxa, Marine Micropaleontology,
30(4), 251-266.
Darling, K. F., M. Kucera, C. J. Pudsey, and C. M. Wade (2004), Molecular evidence links cryptic diversification in polar planktonic protists to Quaternary climate dynamics, Proceedings
of the National Academy of Sciences of the United States of America, 101(20), 7657-7662.
Darling, K. F., M. Kucera, D. Kroon, and C. M. Wade (2006), A resolution for the coiling direction paradox in Neogloboquadrina pachyderma, Paleoceanography, 21(PA2011).
Darling, K. F., C. M. Wade, I. A. Stewart, D. Kroon, R. Dingle, and A. J. L. Brown (2000), Molecular evidence for genetic mixing of Arctic and Antarctic subpolar populations of planktonic foraminifers, Nature, 405(6782), 43-47.
de Moura, J. C., A. de Moraes Rios-Netto, M. D. Wanderley, and F. P. de Sousa (1999), Using acid to extract calcareous microfossils from carbonate rocks, Micropaleontology, 45(4), 429-436. de Nooijer, L. J., E. C. Hathorne, G.-J. Reichart, G. Langer, and J. Bijma (2014), Variability in calcitic
Mg/Ca and Sr/Ca ratios in clones of the benthic foraminifer Ammonia tepida, Marine
Micropaleontology, 107, 32-43.
de Vargas, C., S. Renaud, and H. Hilbrecht (2001a), Pleistocene adaptive radiation in Globorotalia
truncatulinoides: genetic, morphologic, and environmental evidence, Paleobiology, 27(1),
104-125.
de Vargas, C., S. Renaud, H. Hilbrecht, and J. Pawlowski (2001b), Pleistocene adaptive radiation in Globorotalia truncatulinoides: genetic, morphologic, and environmental evidence,
Paleobiology, 27(1), 104-125.
de Villiers, S. (2004), Optimum growth conditions as opposed to calcite saturation as a control on the calcification rate and shell-weight of marine foraminifera, Marine Biology, 144(1), 45-49.
de Villiers, S. (2005), Foraminiferal shell-weight evidence for sedimentary calcite dissolution above the lysocline, Deep Sea Research Part I: Oceanographic Research Papers, 52(5), 671-680. DeDeckker, P., M. Moros, K. Perner, and E. Jansen (2012), Influence of the tropics and southern
westerlies on glacial interhemispheric asymmetry, Nature Geosci, 5(4), 266-269.
Dekens, P. S., D. W. Lea, D. K. Pak, and H. J. Spero (2002), Core top calibration of Mg/Ca in tropical foraminifera: Refining paleotemperature estimation, Geochemistry, Geophysics,
Geosystems, 3(4), 1-29.
Delaney, M. L., A. W. H. Bé, and E. A. Boyle (1985), Li, Sr, Mg, and Na in foraminiferal calcite shells from laboratory culture, sediment traps, and sediment cores, Geochimica et
Cosmochimica Acta, 49(6), 1327-1341.
1
2
3
4
5
6
7
8
9
R & A
(2001a), Oxygen isotope/salinity relationship in the Indian Ocean, Journal of Geophysical
Research, 106, 4565-4574.
Delaygue, G., E. Bard, C. Rollion, J. Jouzel, M. Stiévenard, J. C. Duplessy, and G. Ganssen (2001b), Oxygen isotope/salinity relationship in the northern Indian Ocean, Journal of Geophysical
Research: Oceans (1978–2012), 106(C3), 4565-4574.
DeMaster, D. J., and J. K. Cochran (1982), Particle mixing rates in deep-sea sediments determined from excess 210Pb and 32Si profiles, Earth and Planetary Science Letters, 61(2), 257-271.
deMenocal, P. B., J. Ortiz, T. Guilderson, and M. Sarnthein (2000), Coherent high-and low-latitude climate variability during the Holocene warm period, Science, 288(5474), 2198-2202. DeNiro, M. J., and S. Epstein (1978), Influence of diet on the distribution of carbon isotopes in
animals, Geochimica et cosmochimica acta, 42(5), 495-506.
Denton, G. H., R. F. Anderson, J. R. Toggweiler, R. L. Edwards, J. M. Schaefer, and A. E. Putnam (2010), The last glacial termination, Science, 328(5986), 1652-1656.
Deuser, W. G. (1986), Seasonal and interannual variations in deep-water particle fluxes in the Sargasso Sea and their relation to surface hydrography, Deep Sea Research Part A .
Oceanographic Research Papers, 33(2), 225-246.
Deuser, W. G. (1987), Seasonal variations in isotopic composition and deep-water fluxes of the tests of perennially abundant planktonic foraminifera of the Sargasso Sea; results from sediment-trap collections and their paleoceanographic significance, The Journal of
Foraminiferal Research, 17(1), 14-27.
Deuser, W. G., and E. H. Ross (1980), Seasonal change in the flux of organic carbon to the deep Sargasso Sea, Nature, 283(5745), 364-365.
Deuser, W. G., and E. H. Ross (1989), Seasonally abundant planktonic foraminifera of the Sargasso Sea: Succession, deep-water fluxes, isotopic compositions, and paleoceanographic implications, Journal of Foraminiferal Research, 19(4), 268-293.
Deuser, W. G., E. H. Ross, and R. F. Anderson (1981a), Seasonality in the supply of sediment to the deep Sargasso Sea and implications for the rapid transfer of matter to the deep ocean,
Deep Sea Research Part A . Oceanographic Research Papers, 28(5), 495-505.
Deuser, W. G., E. H. Ross, C. Hemleben, and M. Spindler (1981b), Seasonal changes in species composition, numbers, mass, size, and isotopic composition of planktonic foraminifera settling into the deep Sargasso sea, Palaeogeography, Palaeoclimatology, Palaeoecology,
33(1-3), 103-127.
Dissard, D., G. Nehrke, G.-J. Reichart, and J. Bijma (2010), The impact of salinity on the Mg/ Ca and Sr/Ca ratio in the benthic foraminifera Ammonia tepida: Results from culture experiments, Geochimica et Cosmochimica Acta, 74(3), 928-940.
Dittert, N., and R. Henrich (2000), Carbonate dissolution in the South Atlantic Ocean: evidence from ultrastructure breakdown in Globigerina bulloides, Deep Sea Research Part I:
Oceanographic Research Papers, 47(4), 603-620.
Douglas, R. G., and S. M. Savin (1978), Oxygen isotopic evidence for the depth stratification of Tertiary and Cretaceous planktic foraminifera, Marine Micropaleontology, 3(2), 175-196. Dowsett, H. J. (1989), Application of the graphic correlation method to Pliocene marine sequences,
Marine Micropaleontology, 14(1), 3-32.
Dudley, W. C., J. C. Duplessy, P. L. Blackwelder, L. E. Brand, and R. R. L. Guillard (1980), Coccoliths in Pleistocene–Holocene nannofossil assemblages.
Dueñas-Bohórquez, A., R. E. da Rocha, A. Kuroyanagi, J. Bijma, and G.-J. Reichart (2009), Effect of salinity and seawater calcite saturation state on Mg and Sr incorporation in cultured planktonic foraminifera, Marine Micropaleontology, 73(3), 178-189.
Duplessy, J. C., A. W. H. Bé, and P. L. Blanc (1981), Oxygen and carbon isotopic composition and biogeographic distribution of planktonic foraminifera in the Indian Ocean,
Palaeogeography, Palaeoclimatology, Palaeoecology, 33(1), 9-46.
did the ocean—atmosphere system run during the last deglaciation?, Earth and Planetary
Science Letters, 103(1), 27-40.
Durazzi, J. T. (1981), Stable-isotope studies of planktonic foraminifera in North Atlantic core tops,
Palaeogeography, Palaeoclimatology, Palaeoecology, 33(1-3), 157-172.
Eggins, S. M., P. de Deckker, and J. Marshall (2003), Mg/Ca variation in planktonic foraminifera tests: implications for reconstructing palaeo-seawater temperature and habitat migration,
Earth and Planetary Science Letters, 212(3), 291-306.
Eggins, S. M., A. Sadekov, and P. de Deckker (2003), Modulation and daily banding of Mg/Ca in
Orbulina universa tests by symbiont photosynthesis and respiration: a complication for
seawater thermometry, Earth and Planetary Science Letters, 225, 411-419.
Eggins, S. M., A. Sadekov, and P. de Deckker (2004), Modulation and daily banding of Mg/Ca in
Orbulina universa tests by symbiont photosynthesis and respiration: a complication for
seawater thermometry?, Earth and Planetary Science Letters, 225(3), 411-419.
Eguchi, N. O., H. Kawahata, and A. Taira (1999), Seasonal response of planktonic foraminifera to surface ocean condition: sediment trap results from the central North Pacific Ocean,
Journal of Oceanography, 55(6), 681-691.
Ehrenberg, C. G. (1861), Über die Tiefgrund-Verhältnisse des oceans am Eingange der Davisstrasse
und bei Island.
Ehrenberg, C. G. (1873), Mikrogeologische Studien über das kleinste Leben der Meeres-Tiefgründe aller
Zonen und dessen geologischen Einfluss, Buchdr. der K. Akademie der Wissenschaften, in
Kommission bei F. Dümmler.
Elderfield, H., and G. M. Ganssen (2000), Past temperature and δ18O of surface ocean waters
inferred from foraminiferal Mg/Ca ratios, Nature, 405(6785), 442-445.
Elderfield, H., M. Vautravers, and M. Cooper (2002), The relationship between shell size and Mg/ Ca, Sr/Ca, 18O, and 13C of species of planktonic foraminifera, Geochemistry Geophysics
Geosystems, 3(8).
Elkibbi, M., and J. A. Rial (2001), An outsider’s review of the astronomical theory of the climate: is the eccentricity-driven insolation the main driver of the ice ages?, Earth-Science Reviews,
56(1), 161-177.
Emiliani, C. (1954a), Depth habitats of some species of pelagic foraminifera as indicated by oxygen isotope ratios, American Journal of Science, 252(3), 149-158.
Emiliani, C. (1954b), Temperatures of Pacific bottom waters and polar superficial waters during the Tertiary, Science, 119(3103), 853-855.
Emiliani, C. (1955), Pleistocene Temperatures, The Journal of Geology, 63(6), 538-578. Emiliani, C. (1958), Ancient Temperatures, in Scientific America, edited, pp. 2-11.
Emiliani, C. (1971), Isotopic paleotemperatures and shell morphology of Globigerinoides rubra in the type section of the Pliocene-Pleistocene boundary, Micropaleontology, 17(2), 233-237.
Emiliani, C. (1974), Isotopic paleotemperatures and shell morphology of Globigerinoides rubra in the Mediterranean deep-sea core 189, Micropaleontology, 20(1), 106-109.
Epstein, S., R. Buchsbaum, H. A. Lowenstam, and H. C. Urey (1951), Carbonate-water isotopic temperature scale, Geological Society of America Bulletin, 62, 417-425.
Epstein, S., R. Buchsbaum, H. A. Lowenstam, and H. C. Urey (1953), Revised carbonate-water isotopic temperature scale, Geological Society of America Bulletin, 64(11), 1315-1326. Erez, J. (1978), The influence of differential production and dissolution on the stable isotope
composition of planktonic foraminifera, Massachusetts Institute of Technology and Woods Hole Oceanographic Institution.
Erez, J., and S. Honjo (1981), Comparison of isotopic composition of planktonic foraminifera in plankton tows, sediment traps and sediments, Palaeogeography, Palaeoclimatology,
Palaeoecology, 33(1–3), 129-156.
1
2
3
4
5
6
7
8
9
R & A
Geochemica et Cosmochimica Acta, 47, 1025-1031.
Ericson, D. B. (1959), Coiling direction of Globigerina pachyderma as a climatic index, Science,
130(3369), 219-220.
Ericson, D. B., and G. Wollin (1956a), Micropaleontological and isotopic determinations of Pleistocene climates, Micropaleontology, 2(3), 257-270.
Ericson, D. B., and G. Wollin (1956b), Correlation of six cores from the equatorial Atlantic and the Caribbean, Deep Sea Research (1953), 3(2), 104-125.
Ericson, D. B., G. Wollin, and J. Wollin (1955), Coiling direction of Globorotalia truncatulinoides in deep-sea cores, Deep Sea Research (1953), 2(2), 152-158.
Ericson, D. B., M. Ewing, and G. Wollin (1964), The Pleistocene Epoch in Deep-Sea Sediments A complete time scale dates the beginning of the first ice age at about 1½ million years ago,
Science, 146(3645), 723-732.
Ericson, D. B., M. Ewing, G. Wollin, and B. C. Heezen (1961), Atlantic deep-sea sediment cores,
Geological Society of America Bulletin, 72(2), 193-286.
Fabry, V. J., B. A. Seibel, R. A. Feely, and J. C. Orr (2008), Impacts of ocean acidification on marine fauna and ecosystem processes, ICES Journal of Marine Science: Journal du Conseil, 65(3), 414-432.
Fairbanks, R. G., P. H. Wiebe, and A. W. H. Be (1980), Vertical distribution and Isotopic Composition of Living Planktonic Foraminifera in the Western North Atlantic, Science, 207, 61-63. Fairbanks, R. G., M. Sverdlove, R. Free, P. H. Wiebe, and A. W. H. Bé (1982a), Vertical distribution
and isotopic fractionation of living planktonic foraminifera from the Panama Basin,
Nature, 298(5877), 841-844.
Fairbanks, R. G., M. S. Sverdlove, R. Free, P. H. Wiebe, and A. W. H. Bé (1982b), Vertical distribution and isotopic fractionation of living planktonic foraminifera from the Panama Basin,
Nature, 298(5877), 841-844.
Fallet, U., W. Boer, C. van Assen, M. Greaves, and G.-J. A. Brummer (2009), A novel application of wet-oxidation to retrieve carbonates from large, organic-rich samples for application in climate research, Geochemistry Geophysics Geosystems, 10(8).
Farmer, E. C., P. B. DeMenocal, and T. M. Marchitto (2005), Holocene and deglacial ocean temperature variability in the Benguela upwelling region: Implications for low‐latitude atmospheric circulation, Paleoceanography, 20(2).
Farmer, E. C., A. Kaplan, P. B. de Menocal, and J. Lynch‐Stieglitz (2007), Corroborating ecological depth preferences of planktonic foraminifera in the tropical Atlantic with the stable oxygen isotope ratios of core top specimens, Paleoceanography, 22(3).
Farmer, E. J., M. R. Chapman, and J. E. Andrews (2011), Holocene temperature evolution of the subpolar North Atlantic recorded in the Mg/Ca ratios of surface and thermocline dwelling planktonic foraminifers, Global and Planetary Change, 79(3), 234-243.
Fehrenbacher, J. S., and P. A. Martin (2014), Exploring the dissolution effect on the intrashell Mg/ Ca variability of the planktic foraminifer Globigerinoides ruber, Paleoceanography. Feldmeijer, W., B. Metcalfe, P. Scussolini, and K. Arthur (2013), The effect of chemical pretreatment
of sediment upon foraminiferal-based proxies, Geochemistry, Geophysics, Geosystems,
14(10), 3996-4014.
Feldmeijer, W., B. Metcalfe, G.-J. A. Brummer, and G. M. Ganssen (Accepted), Reconstructing the depth of the permanent theromcline through the morphology and geochemistry of the deep dwelling foraminifer Globorotalia truncatulinoides, Paleoceanography.
Ferreira, D., J. Marshall, and B. Rose (2011), Climate determinism revisited: Multiple equilibria in a complex climate model, Journal of Climate, 24(4), 992-1012.
Field, D. B. (2004), Variability in vertical distributions of planktonic foraminifera in the California Current: Relationships to vertical ocean structure, Paleoceanography, 19(2).
benthic foraminifera and hydrographic data, Estuaries, 27(5), 867-881.
Fletcher, W. J., U. C. Müller, A. Koutsodendris, K. Christanis, and J. Pross (2013), A centennial-scale record of vegetation and climate variability from 312 to 240 ka (Marine Isotope Stages 9c–a, 8 and 7e) from Tenaghi Philippon, NE Greece, Quaternary Science Reviews, 78, 108-125.
Fok-Pun, L., and P. D. Komar (1983), Settling velocities of planktonic foraminifera; density variations and shape effects, The Journal of Foraminiferal Research, 13(1), 60-68.
Franco-Fraguas, P., K. B. Costa, and F. A. L. Toledo (2011), Relationship between isotopic composition (Δ18O and Δ13C) and plaktonic foraminifera test size in core tops from the
Brazilian Continental Margin, Brazilian Journal of Oceanography, 59(4), 327-338. Friedrich, O., R. Schiebel, P. A. Wilson, S. Weldeab, C. J. Beer, M. J. Cooper, and J. Fiebig (2012),
Influence of test size, water depth, and ecology on Mg/Ca, Sr/Ca, δ18O and δ13C in nine
modern species of planktic foraminifers, Earth and Planetary Science Letters, 319-320(0), 133-145.
Furbish, D. J., and A. J. Arnold (1997), Hydrodynamic strategies in the morphological evolution of spinose planktonic foraminifera, Geological Society of America Bulletin, 109(8), 1055-1072.
Galloway, J. J., and S. G. Wissler (1927), Pleistocene foraminifera from the Lomita Quarry, Palos Verdes Hills, California, Journal of Paleontology, 35-87.
Ganopolski, A., and S. Rahmstorf (2001), Rapid changes of glacial climate simulated in a coupled climate model, Nature, 409(6817), 153-158.
Ganopolski, A., S. Rahmstorf, V. Petoukhov, and M. Claussen (1998), Simulation of modern and glacial climates with a coupled global model of intermediate complexity, Nature,
391(6665), 351-356.
Ganssen, G. M. (1981), Isotopic analysis of foraminifera shells: Interference from chemical treatment, Palaeogeography, Palaeoclimatology, Palaeoecology, 33, 271-276.
Ganssen, G. M. (1983), Dokumentation von kϋstennahem Auftrieb anhand stabiler Isotope in rezenten Foraminiferan vor Nordwest-Afrika, “Meteor” Forschungsergebnisse
Herausgegeben von der Deutschen Forschungsgemeinschaft, C(37), 1-46.
Ganssen, G. M., and M. Sarnthein (1983), Stable-isotope composition of foraminifers: the surface and bottom water record of coastal upwelling, in Coastal Upwelling Its Sediment Record, edited, pp. 99-121, Springer.
Ganssen, G. M., and D. Kroon (1991), Evidence for Red Sea surface circulation from oxygen isotopes of modern surface waters and planktonic foraminiferal tests, Paleoceanography,
6(1), 73-82.
Ganssen, G. M., and D. Kroon (2000), The isotopic signature of planktonic foraminifera from NE Atlantic surface sediments: implications for the reconstruction of past oceanic conditions,
Journal of the Geological Society London, 157(3), 693-699.
Ganssen, G. M., F. J. C. Peeters, B. Metcalfe, P. Anand, S. Jung, D. Kroon, and G.-J. A. Brummer (2011), Quantifying sea surface temperature ranges of the Arabian Sea for the past 20,000 years, Climate of the Past, 7, 1337-2686.
Geikie, A. (1863), On the phenomena of the glacial drift of Scotland, Published for the Society of J. Gray.
Geikie, J. (1879), The Great Ice Age and Its Relation to the Antiquity of Man. 1874, New York:
Appleton.
Genovesi, L., A. De Vernal, B. Thibodeau, C. Hillaire-Marcel, A. Mucci, and D. Gilbert (2011), Recent changes in bottom water oxygenation and temperature in the Gulf of St. Lawrence: Micropaleontological and geochemical evidence, Limnology and Oceanography, 56(4), 1319-1329.
1
2
3
4
5
6
7
8
9
R & A
data, Nature, 421(6925), 833-837.Gillett, N. P., V. K. Arora, K. Zickfeld, S. J. Marshall, and W. J. Merryfield (2011), Ongoing climate change following a complete cessation of carbon dioxide emissions, Nature Geoscience,
4(2), 83-87.
Giraudeau, J. (1993), Planktonic foraminiferal assemblages in surface sediments from the southwest African continental margin, Marine Geology, 110(1), 47-62.
Giraudeau, J., and J. Rogers (1994), Phytoplankton biomass and sea-surface temperature estimates from sea-bed distribution of nannofossils and planktonic foraminifera in the Benguela upwelling system, Micropaleontology, 275-285.
Godad, S. P., P. D. Naidu, and B. A. Malmgren (2011), Sea surface temperature changes during May and August in the western Arabian Sea over the last 22kyr: Implications as to shifting of the upwelling season, Marine Micropaleontology, 78(1), 25-29.
Goosse, H., V. Brovkin, T. Fichefet, R. Haarsma, P. Huybrechts, J. Jongma, A. Mouchet, F. Selten, P. Y. Barriat, and J. M. Campin (2010), Description of the Earth system model of intermediate complexity LOVECLIM version 1.2, Geoscientific Model Development, 3(2), 603-633. Greaves, M., S. Barker, C. Daunt, and H. Elderfield (2005), Accuracy, standardization, and
interlaboratory calibration standards for foraminiferal Mg/Ca thermometry, Geochem .
Geophys . Geosyst ., 6(2), Q02D13.
Groeneveld, J., and C. M. Chiessi (2011), Mg/Ca of Globorotalia inflata as a recorder of permanent thermocline temperatures in the South Atlantic, Paleoceanography, 26(2), PA2203. Grootes, P. M., and M. Stuiver (1997), Oxygen 18/16 variability in Greenland snow and ice with
10−3‐to 105‐year time resolution, Journal of Geophysical Research: Oceans (1978–2012),
102(C12), 26455-26470.
Grootes, P. M., M. Stuiver, J. W. C. White, S. J. Johnsen, and J. Jouzel (1993), Comparison of oxygen isotope records from the GISP2 and GRIP Greenland ice cores, Nature, 366(552), 552-554.
Groß, O. (2002), Sediment interactions of foraminifera: implications for food degradation and bioturbation processes, The Journal of Foraminiferal Research, 32(4), 414-424.
Grötsch, J., G. Wu, and W. H. Berger (1991), 1.6 Carbonate Cycles in the Pacific: Reconstruction of Saturation Fluctuations, in Cycles and Event Stratigraphy, edited by G. Einsele, W. Ricken and A. Seilacher, pp. 110-125, Springer-Verlag, Berlin Heidelberg.
Grottoli, A. G., L. J. Rodrigues, K. A. Matthews, J. E. Palardy, and O. T. Gibb (2005), Pre-treatment effects on coral skeletal δ13C and δ18O, Chemical Geology, 221(3-4), 225-242.
Gruber, N., C. D. Keeling, and N. R. Bates (2002), Interannual variability in the North Atlantic Ocean carbon sink, Science, 298(5602), 2374-2378.
Guinasso, N. L., and D. R. Schink (1975), Quantitative estimates of biological mixing rates in abyssal sediments, Journal of Geophysical Research, 80(21), 3032-3043.
Gupta, A. K., D. M. Anderson, and J. T. Overpeck (2003), Abrupt changes in the Asian southwest monsoon during the Holocene and their links to the North Atlantic Ocean, Nature,
421(6921), 354-357.
Guptha, M. V. S., W. B. Curry, V. Ittekkot, and A. S. Muralinath (1997), Seasonal variation in the flux of planktic Foraminifera; sediment trap results from the Bay of Bengal, northern Indian Ocean, The Journal of Foraminiferal Research, 27(1), 5-19.
Gutjahr, M., B. A. A. Hoogakker, M. Frank, and I. N. McCave (2010), Changes in North Atlantic Deep Water strength and bottom water masses during Marine Isotope Stage 3 (45– 35kaBP), Quaternary Science Reviews, 29(19), 2451-2461.
Haarmann, T., E. C. Hathorne, M. Mohtadi, J. Groeneveld, M. Kölling, and T. Bickert (2011), Mg/ Ca ratios of single planktonic foraminifer shells and the potential to reconstruct the thermal seasonality of the water column, Paleoceanography, 26(3).
Hammer, Ø., D. A. T. Harper, and P. D. Ryan (2001), PAST: Paleontological Statistics software package for education and data analysis, Palaeontologica Electronica, 4(1), 9.
Hamner, W. M. (1975), Underwater observations of blue-water plankton: logistics, techniques, and safety procedures for divers at sea, Limnol . Oceanogr, 20(6), 1045-1051.
Hathorne, E. C., R. H. James, and R. S. Lampitt (2009), Environmental versus biomineralization controls on the intratest variation in the trace element composition of the planktonic foraminifera G . inflata and G . scitula, Paleoceanography, 24(4).
Hathorne, E. C., O. Alard, R. H. James, and N. W. Rogers (2003), Determination of intratest variability of trace elements in foraminifera by laser ablation inductively coupled plasma‐ mass spectrometry, Geochemistry, Geophysics, Geosystems, 4(12).
Hathorne, E. C., R. H. James, P. Savage, and O. Alardc (2008), Physical and chemical characteristics of particles produced by laser ablation of biogenic calcium carbonate, Journal of Analytical
Atomic Spectrometry, 23, 240-243.
Hays, J. D., and W. A. Berggren (1971), Quaternary boundaries and correlations, The
Micropaleontology of Oceans . Cambridge University Press, Cambridge, 669-691.
Hays, J. D., J. Imbrie, and N. J. Shackleton (1976), Variations in the Earth’s orbit: Pacemaker of the ice ages, American Association for the Advancement of Science.
Healy-Williams, N., and D. F. Williams (1981), Fourier analysis of test shape of planktonic foraminifera.
Healy-Williams, N., R. Ehrlich, and D. F. Williams (1985), Morphometric and stable isotopic evidence for subpopulations of Globorotalia truncatulinoides, Journal of Foraminiferal
Research, 15(4), 242-253.
Hecht, A. D. (1974a), Intraspecific variation in recent populations of Globigerinoides ruber and
Globigerinoides trilobus and their application to paleoenvironmental analysis, Journal of Paleontology, 1217-1234.
Hecht, A. D. (1974b), The oxygen isotopic record of foraminifera in deep-sea sediment,
Foraminifera ., Academic Press, London, 1-43.
Hecht, A. D., A. W. H. Be, and L. Lott (1976), Ecologic and paleoclimatic implications of morphologic variation of Orbulina universa in the Indian Ocean, Science, 194, 422-424. Heier-Nielsen, S., A. Kuijpers, and T. Laier (1995), Holocene sediment deposition and organic
matter burial in the upwelling zone off Yemen, Northwest Indian Ocean, in Netherlands
Indian Ocean Programme: Tracing a seasonal upwelling, edited by J. E. van Hinte, T. C.
E. van Weering and S. R. Troelstra, pp. 111-119, National Museum of Natural History, Leiden.
Heinrich, H. (1988), Origin and consequences of cyclic ice rafting in the northeast Atlantic Ocean during the past 130,000 years, Quaternary research, 29(2), 142-152.
Hemleben, C. (1982), Cytologic and ecologic aspects of morphogenesis and structure of recent and fossil protistan and pteropod skeletons, Neues Jahrbuch für Geologie und Paläontologie .
Abhandlungen, 164, 82-96.
Hemleben, C., and M. Spindler (1983), Recent advances in research on living planktonic foraminifera, in Reconstruction of marine Paleoenvironments, edited by J. E. Meulenkamp, pp. 141-170.
Hemleben, C., and A. Auras (1984), Variations in the calcite dissolution pattern on the Barbados Ridge Complex at site-541 and site-543, Deep-Sea Drilling Project Leg-78A, Initial
Reports of the Deep Sea Drilling Project, 78(AUG), 471-497.
Hemleben, C., and J. Bijma (1994), Foraminiferal population dynamics and stable carbon isotopes, in Carbon Cycling in the Glacial Ocean: Constraints on the Ocean’s Role in Global Change, edited, pp. 145-166, Springer.
Hemleben, C., M. Spindler, and O. R. Anderson (1989), Modern Planktonic Foraminifera, 363 pp., Springer-Verlag, New York.
1
2
3
4
5
6
7
8
9
R & A
on the ontogeny and ecology of some globorotaliid species from the Sargasso Sea off Bermuda, The Journal of Foraminiferal Research, 15(4), 254-272.
Hemleben, C., M. Spindler, I. Breitinger, and R. Ott (1987), Morphological and physiological responses of Globigerinoides sacculifer(Brady) under varying laboratory conditions,
Marine Micropaleontology, 12, 305-324.
Hemming, S. R. (2004), Heinrich events: Massive late Pleistocene detritus layers of the North Atlantic and their global climate imprint, Reviews of Geophysics, 42(1).
Herguera, J. C. (2000), Last glacial paleoproductivity patterns in the eastern equatorial Pacific: benthic foraminifera records, Marine Micropaleontology, 40(3), 259-275.
Hilbrecht, H. (1997), Morphologic gradation and ecology in Neogloboquadrina pachyderma and
N . dutertrei(planktic foraminifera) from core top sediments, Marine Micropaleontology, 31(1), 31-43.
Hodell, D. A., and J. H. Curtis (2008), Oxygen and carbon isotopes of detrital carbonate in North Atlantic Heinrich Events, Marine Geology, 256(1-4), 30-35.
Holden, P. B., N. R. Edwards, E. W. Wolff, P. J. Valdes, and J. S. Singarayer (2011), The Mid‐Brunhes Event and West Antarctic ice sheet stability, Journal of Quaternary Science, 26(5), 474-477.
Honjo, S. (1978), Sedimentation of materials in Sargasso Sea at a 5,367 m deep station, Journal of
Marine Research, 36(3), 469-492.
Honjo, S. (2013), The rain of ocean particles and Earth’s carbon cycle, Life, 50(2).
Honjo, S., and M. R. Roman (1978), Marine copepod fecal pellets-Production, preservation and sedimentation, Journal of Marine Research, 36(1), 45-57.
Horibe, Y., and T. Oba (1972), Temperature scales of aragonite-water and calcite-water systems,
Fossils(23-24), 69-78.
Hutson, W. H. (1980), Bioturbation of deep-sea sediments: Oxygen isotopes and stratigraphic uncertainty, Geology, 8, 127-130.
Huybers, P. J. (2007), Glacial variability over the last two million years: an extended depth-derived agemodel, continuous obliquity pacing, and the Pleistocene progression, Quaternary
Science Reviews, 26(1), 37-55.
Huybers, P. J. (2009), Pleistocene glacial variability as a chaotic response to obliquity forcing. Huybers, P. J. (2011), Combined obliquity and precession pacing of late Pleistocene deglaciations,
Nature, 480(7376), 229-232.
Huybers, P. J., and C. Wunsch (2005), Obliquity pacing of the late Pleistocene glacial terminations,
Nature, 434(7032), 491-494.
Imbrie, J., and N. G. Kipp (1971), A new micropaleontological method for quantitative paleoclimatology: application to a late Pleistocene Caribbean core, The late Cenozoic
glacial ages, 3, 71-181.
Imbrie, J., E. A. Boyle, S. C. Clemens, A. Duffy, W. R. Howard, G. Kukla, J. Kutzbach, D. G. Martinson, A. McIntyre, and A. C. Mix (1992), On the structure and origin of major glaciation cycles 1. Linear responses to Milankovitch forcing, Paleoceanography, 7(6), 701-738.
Ingle, J. C. (1973), Neogene foraminifera from the northeastern Pacific Ocean, Leg 18, Deep Sea Drilling Project, Initial Reports of the Deep Sea Drilling Project, 18, 517-567.
Ishimura, T., U. Tsunogai, and F. Nakagawa (2008), Grain-scale heterogeneities in the stable carbon and oxygen isotopic compositions of the international standard calcite materials (NBS 19, NBS 18, IAEA-CO-1, and IAEA-CO-8), Rapid Communications in Mass Spectrometry,
22, 1925-1932.
Ivanochko, T. S., R. S. Ganeshram, G.-J. A. Brummer, G. M. Ganssen, S. J. A. Jung, S. G. Moreton, and D. Kroon (2005a), Variations in tropical convection as an amplifier of global climate change at the millennial scale, Earth and Planetary Science Letters, 235(1), 302-314. Ivanochko, T. S., R. S. Ganeshram, G.-J. A. Brummer, G. M. Ganssen, S. J. A. Jung, G. Steven, S.
global climate change at the millennial scale, Earth and Planetary Science Letters, 235, 302-314.
Jansen, E., and T. Veum (1990), Evidence for two-step deglaciation and its impact on North Atlantic deep-water circulation, Nature, 343, 612-616.
Jansen, J. H. F., S. J. Van der Gaast, B. Koster, and A. J. Vaars (1998), CORTEX, a shipboard XRF-scanner for element analyses in split sediment cores, Marine Geology, 151(1), 143-153. Jenkins, D. G., and J. W. Murray (1989), Stratigraphical atlas of fossil foraminifera, Ellis Horwood. Jochum, K. P., et al. (2011), Determination of Reference Values for NIST SRM 610–617 Glasses
Following ISO Guidelines, Geostandards and Geoanalytical Research, 35(4), 397-429. Johnsen, S. J., W. Dansgaard, H. B. Clausen, and C. C. Langway (1972), Oxygen isotope profiles
through the Antarctic and Greenland ice sheets, Nature, 235(5339), 429-434.
Johnsen, S. J., H. B. Clausen, W. Dansgaard, K. Fuhrer, N. S. Gundestrup, C. U. Hammer, P. l. Iversen, J. Jouzel, B. Stauffer, and J. P. Steffensen (1992), Irregular glacial interstadials recorded in a new Greenland ice core, Nature, 359(6393), 311-313.
Johnson, H. L., and D. P. Marshall (2002), A theory for the surface Atlantic response to thermohaline variability, Journal of Physical Oceanography, 32(4), 1121-1132.
Johnstone, H. J. H., M. Schulz, S. Barker, and H. Elderfield (2010), Inside story: An X-ray computed tomography method for assessing dissolution in the tests of planktonic foraminifera,
Marine Micropaleontology, 77(1–2), 58-70.
Jones, G. A., and W. F. Ruddiman (1982), Assessing the global meltwater spike, Quaternary
Research, 17(2), 148-172.
Jonkers, L., S. Heuven, R. Zahn, and F. J. C. Peeters (2013), Seasonal patterns of shell flux, δ18O
and δ13C of small and large N . pachyderma (s) and G. bulloides in the subpolar North
Atlantic, Paleoceanography, 28(1), 164-174.
Jonkers, L., G. J. A. Brummer, F. J. C. Peeters, H. M. van Aken, and M. F. De Jong (2010), Seasonal stratification, shell flux, and oxygen isotope dynamics of left‐coiling N . pachyderma and
T . quinqueloba in the western subpolar North Atlantic, Paleoceanography, 25(2).
Jonkers, L., L. J. De Nooijer, G.-J. Reichart, R. Zahn, and G.-J. A. Brummer (2012), Encrustation and trace element composition of Neogloboquadrina dutertrei assessed from single chamber analyses, implications for paleotemperature estimates, Biogeosciences Discussions, 9(8), 10615-10644.
Juday, C. (1916), Limnological apparatus, Trans . Wisconsin Acad . Sci, 18, 566-592.
Jung, S. J. A., G. R. Davies, G. M. Ganssen, and D. Kroon (2004), Synchronous Holocene sea surface temperature and rainfall variations in the Asian monsoon system, Quaternary Science
Reviews, 23(20), 2207-2218.
Jung, S. J. A., D. Kroon, G. M. Ganssen, F. J. C. Peeters, and R. S. Ganeshram (2009), Enhanced Arabian Sea intermediate water flow during glacial North Atlantic cold phases, Earth and
Planetary Science Letters, 280(1), 220-228.
Jung, S. J. A., E. Ivanova, G.-J. Reichart, G. R. Davies, G. M. Ganssen, D. Kroon, and J. E. Van Hinte (2002), Centennial-millennial-scale monsoon variations off Somalia over the last 35 ka,
Geological Society, London, Special Publications, 195(1), 341-352.
Kahn, M. I. (1979), Non-equilibrium oxygen and carbon isotopic fractionation in tests of living planktonic-foraminifera, Oceanologica Acta, 2(2), 195-208.
Kahn, M. I., and D. F. Williams (1981), Oxygen and carbon isotopic composition of living planktonic foraminifera from the northeast Pacific Ocean, Palaeogeography, palaeoclimatology,
palaeoecology, 33(1), 47-69.
Kallel, N., L. D. Labeyrie, M. Arnold, H. Okada, W. C. Dudley, and J. C. Duplessy (1988), Evidence of cooling during the Younger Dryas in the western North Pacific, Oceanologica Acta,
11(4), 369-375.