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Trace elements, stable isotopes, and clay mineralogy of the Elles II K–T boundary section in Tunisia: indications for sea level fluctuations and primary productivity

Stüben, D, Kramar, U, Berner, Z, Stinnesbeck, W, Keller, G, Adatte, T·2002·Palaeogeography, Palaeoclimatology, Palaeoecology
DOI 10.1016/s0031-0182(01)00401-1
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  • Revised Carbonate-water isotopic temperature scale

    EPSTEIN, S., BUCHSBAUM, R., LOWENSTAM, H. A., & UREY, H. C. (1953) · Geological Society of America Bulletin · doi:10.1130/0016-7606(1953)64[1315:rcits]2.0.co;2 · Cited by 2,271 · cited 2×

    “…foraminifera is believed to accurately record N18O variations of the ambient seawater and hence variations of temperature, based on the assumption that planktic foraminifera build their tests in isotopic equilibrium with ambient seawater (Epstein et al., 1953; Shackelton, 1967; Erez and Luz, 1992).”
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Research works printed but not linked: 99

  1. Adatte, T., Keller, G., Li, L., Stinnesbeck, W., 2002. Late Cretaceous to Early Palaeocene climate and sea-level fluctuations: The Tunisian record. Palaeogeogr. Palaeoclimatol. Palaeoecol. 178, 165–196. · DOI
  2. Adatte, T., Rumley, G., 1989. Sedimentology and mineralogy of Valanginian and Hauterivian in the stratotypic region (Jura mountains, Switzerland). In: Wiedmann, J. (Ed.), Cretaceous of the Western Tethys. Proceedings 3rd International Cretaceous Symposium. Scheizerbart’sche Verlagsbuchhandlung, Stuttgart, pp. 329–351.
  3. Adatte, T., Stinnesbeck, W., Keller, G., 1996. Lithostratigraphic and mineralogical correlations of near-K-T boundary clastic sediments in northeastern Mexico: Implications for mega-tsunami or sea-level changes? Geol. Soc. Am. Spec. Pap. 037, pp. 197–210. · DOI
  4. Barrera, 1990, Stable isotope evidence for gradual environmental changes and species survivorship across the Cretaceous/Tertiary boundary, Paleoceanography, 5, 867, 10.1029/PA005i006p00867 · DOI
  5. Ben Abdelkader, 1995, Biostratigraphy and lithology of the Cretaceous-Tertiary stratotype boundary of El Kef (Tunisia), Ann. Mines Géol., 35, 11
  6. Berggren, W.A., Kent, D.V., Swisher, C.C., Aubry, M.-P., 1995. A revised Cenozoic geochronology and chronostratigraphy. In: Berggren, W.A. et al. (Eds.), Time Scales and Global Stratigraphic Correlations. Soc. Econ. Paleontol. Mineral. Spec. Publ. 54, pp. 129–131. · DOI
  7. Bijma, J., Spero, H.J., Lea, D.W., 1999. Reassessing foraminiferal stable isotope geochemistry: impact of the oceanic carbonate system (experimental results). In: Fischer, G., Wefer, G. (Eds.), Use of Proxies in Paleoceanography. Springer Verlag, Berlin, pp. 489–512. · DOI
  8. Boyle, 1981, Cadmium, zinc, copper and barium in foraminiferea tests, Earth Planet. Sci. Lett., 53, 11, 10.1016/0012-821X(81)90022-4 · DOI
  9. Boyle, 1986, Paired carbon isotope and cadmium data from benthic foraminifera. Implications for changes in oceanic phosphorous, oceanic circulation, and atmospheric carbon dioxide, Geochim. Cosmochim. Acta, 50, 265, 10.1016/0016-7037(86)90175-4 · DOI
  10. Brasier, M.D., 1995. Fossil indicators of nutrient levels. 1: Eutrophication and climate change. In: Bosence, D.W.J., Allison, P.A. (Eds.), Marine Palaeoenvironmental Analysis from Fossils. Geol. Soc. Spec. Publ. 83, pp. 113–132. · DOI
  11. Brinkhuis, 1988, Dinoflagelate cysts, sealevel changes and planktic foraminiferes across the Cretaceous-Tertiary boundary at El Maria, northwest Tunisia, Mar. Micropaleontol., 13, 153, 10.1016/0377-8398(88)90002-3 · DOI
  12. Broecker, W.S., Peng, T.S., 1984. The climate-chemistry connection. In: Hansen, J.E., Takahashi, T. (Eds.), Climate Sensitivity. Am. Geophys. Union Monogr. 29, pp. 327–336. · DOI
  13. Burollet, P.F., 1967. General Geology of Tunisia. Petroleum Explor. Soc. Libya, 9th Annual Field Conference, Tripoli, pp. 51–58.
  14. Cande, 1992, A new geomagnetic polarity time scale for the Late Cretaceous and Cenozoic, J. Geophys. Res., 97, 13917, 10.1029/92JB01202 · DOI
  15. Cande, 1995, Revised calibration of the geomagnetic polarity time scale for the Late Cretaceous and Cenozoic, J. Geophys. Res., 100, 6093, 10.1029/94JB03098 · DOI
  16. Chamley, H., 1989. Clay Sedimentology. Springer, Berlin. · DOI
  17. Chamley, 1990, Sur l’abondance des minéraux smectitiques dans les sediments marins communs déposés lors des periodes de haut niveau marin du Jurassique supérieur au Paleogène, C.R. Acad. Sci. Se. 2, Méc, Phys. Chim. Sci. Univers Sci. Terre, 311, 1529
  18. Chamley, H., Masse, J.-P., 1975. Sur la signification des minèraux argileux dans les sèdiments barrèmiens et bèdouliens de Provence (SE de la France). 9ëme Congr. Int. Sèdimentol., Nice, Vol. 1, pp. 25–30
  19. Debrabant, 1992, Clay sedimentology, mineralogy and chemistry of Mesozoic sediments drilled in the northern Paris Basin, Sci. Drill., 3, 138
  20. Deconinck, J.F., 1992. Sédimentologie des argiles dans le Jurassique-Crétacé du Europe occidentale et du Maroc. Mém. Thesis, Univ. Lille I, Lille.
  21. Deconinck, 1985, Contrôles tectonique, eustatique et climatique de la sédimentation argileuse du domaine subalpin francais au Malm-Crétacé, Rev. Géogr. Phys. Geol. Dyn., 26, 311
  22. Dittert, N., Baumann, K.-H., Bickert, T., Heinrich, R., Huber, R., Kinkel, H., Meggers, H., 1999. Carbonate dissolution in the deep-sea: methods, quantification and paleoceanographic application. In: Fischer, G., Wefer, G. (Eds.), Use of Proxies in Paleoceanography. Examples from South Atlantic. Springer, Berlin, pp. 255–284. · DOI
  23. Donovan, A.D., Baum, G.R., Blechschmidt, G.L., Loutit, T.S., Pflum, C.E., Vail, P.R., 1988. Sequence stratigraphic setting of the Cretaceous-Tertiary boundary in Central Alabama. In: Berggren, W.A. et al. (Eds.), Sea Level Changes. Soc. Econ. Paleontol. Mineral. Spec. Publ. 42, pp. 299–307. · DOI
  24. Donze, 1982, Les ostracodes du Campanien terminal à l’Eocène inférieur de la coupe du Kef, Tunisie nord-occidentale, Bull. Centres Rech. Explor. Prod. Elf-Aquitainne, 6, 273
  25. Donze, P., Jardiné, S., Legoux, O., Masure, E., Méon, H., 1985. Les événements à la limite Crétacé-Tertiaire au Kef (Tunisie septentrionale) l’analyse palyno-planctologique montre qu′un changement climatique est décelable à la base du Danien. Actes du 1er Congrès nationale des Sciences de la Terre, Tunis, pp. 161–169
  26. Dymond, 1992, Barium in deep-sea sediments: A proxy for paleoproductivity, Paleoceanography, 7, 163, 10.1029/92PA00181 · DOI
  27. Erez, 1992, Temperature control of oxygen-isotope fractionation of cultured planktic foraminifera, Nature, 297, 220, 10.1038/297220a0 · DOI
  28. Fischer, G., Wefer, G. (Eds.), 1999. Use of Proxies in Paleoceanography – Examples from South Atlantic. Springer, Berlin. · DOI
  29. Gibbs, 1977, Clay mineral segregation in the marine environment, J. Sediment. Petrol., 47, 237
  30. Gingele, F.X., Zabel, M., Kasten, S., Bonn, W.J., Nürnberg, C.C., 1999. Biogenic barium as a proxy for paleoproductivity: Methods and limitations of application. In: Fischer, G., Wefer, G. (Eds.), Use of Proxies in Paleoceanography – Examples from South Atlantic. Springer, Berlin, pp. 345–364. · DOI
  31. Govindaraju, 1994, Compilation of working values and sample description for 383 geostandards, Geostand. Newslet., 18, 1, 10.1111/j.1751-908X.1994.tb00502.x · DOI
  32. Graham, 1982, Strontium calcium ratios in Conocoic planktonic foraminifera, Geochim. Cosmochim. Acta, 46, 1281, 10.1016/0016-7037(82)90012-6 · DOI
  33. Hallam, A., 1992. Phanerozoic Sea-Level Changes. Columbia University Press, New York.
  34. Hendriks, 1990, Early Tertiary marine palygorskite and sepiolite neoformation in SE Egypt, Z. Dtsch. Geol. Ges., 141, 87
  35. Herbert, T.D., Silva, I.P., Erba, E., Fischer, A.G., 1995. Orbital chronology of Cretaceous-Paleocene marine sediments. In: Berggren, W.A. et al. (Eds.), Time Scales and Global Stratigraphic Correlations. Soc. Econ. Paleontol. Mineral. Spec. Publ. 54, pp. 81–93. · DOI
  36. Jenkyns, 1996, Relative sea-level change and carbon isotopes: data from the Upper Jurassic (Oxfordian) of central and Southern Europe, Terra Nova, 8, 75, 10.1111/j.1365-3121.1996.tb00727.x · DOI
  37. Jenkyns, 1994, Carbon- and oxygen-isotope stratigraphy of the English Chalk and Italian Scaglia and its palaeoclimatic significance, Geol. Mag., 131, 1, 10.1017/S0016756800010451 · DOI
  38. Jenkyns, 1995, Upper Cretaceous carbon- and oxygen-isotope stratigraphy of deep-water sediments from the North-Central Pacific (Site 869, Flank of Pikinni-Wodejebato, Marshall Islands), Proc. ODP Sci. Results, 143, 105
  39. Kaiho, 1999, Oceanic primary productivity and dissolved oxygen levels at the Creataceous-Tertiary boundary: Their decrease, subsequent warming and recovery, Paleoceanography, 14, 511, 10.1029/1999PA900022 · DOI
  40. Karoui, N., Zaghbib-Turki, D., 1998. Une nouvelle coupe complète pur son passage Crétacé-Tertiaire: la coupe d’Elles, témoignage des foraminiféres planctoniques. In: International Workshop on Cretaceous-Tertiary Transition, Tunis, pp. 55–57.
  41. Karoui-Yakoub, 2002, The Cretaceous–Tertiary (K–T) mass extinction in planktic foraminifera at Elles I and El Melah, Tunisia. Palaeogeogr. Palaeoclimatol. Palaeoecol., 178, 233, 10.1016/S0031-0182(01)00398-4 · DOI
  42. Karpoff, 1989, L’authigenèse océanique de palygorskite, par halmyrolyse de péridotites serpentinisées (marge de Galice): ses implications géodynamiques, C.R. Acad. Sci. Paris, 308, 647
  43. Keller, 1988, Biotic turnover in benthic foraminifera across the Cretaceous/Tertiary boundary at El Kef, Tunisia, Palaeogeogr. Palaeoclimatol. Palaeoecol., 66, 153, 10.1016/0031-0182(88)90198-8 · DOI
  44. Keller, 1988, Extinction, survivorship and evolution of planktic foraminifera across the Cretaceous/Tertiary boundary at El Kef, Tunisia, Mar. Micropaleontol., 13, 239, 10.1016/0377-8398(88)90005-9 · DOI
  45. Keller, 2002, Paleoecology of the Cretaceous–Tertiary mass extinction in planktic foraminifera, Palaeogeogr. Palaeoclimatol. Palaeoecol., 178, 257, 10.1016/S0031-0182(01)00399-6 · DOI
  46. Keller, 1998, The Cretaceous–Tertiary transition on the shallow Saharan Platform of Southern Tunisia, Geobios, 30, 951, 10.1016/S0016-6995(97)80218-5 · DOI
  47. Keller, 1993, Gradual mass extinction, species survivorship and long-term environmental changes across the Cretaceous/Tertiary boundary in high latitudes, Geol. Soc. Am. Bull., 105, 979, 10.1130/0016-7606(1993)105<0979:GMESSA>2.3.CO;2 · DOI · Paper page
  48. Keller, 1996, The Cretaceous Tertiary boundary stratotype at El Kef, Tunisia: How catastrophic was the mass extinction, Palaeogeogr. Palaeoclimatol. Palaeoecol., 119, 221, 10.1016/0031-0182(95)00009-7 · DOI
  49. Keller, 1989, Stable isotope, TOC, CaCO3 record across the Creataceous/Tertiary boundary at El Kef, Tunisia, Palaeogeogr. Palaeoclimatol. Palaeoecol., 73, 243, 10.1016/0031-0182(89)90007-2 · DOI
  50. Keller, G., Stinnesbeck, W., 1996. Sea level changes, clastic deposits and megatsunamis across the Cretaceous–Tertiary boundary. In: MacLeod, N., Keller, G. (Eds.), Cretaceous–Tertiary Mass Extinctions. Norton Press, New York, pp. 415–450.
  51. Knauer, G.A., Martin, J.H., 1982. Trace elements and primary production: Problems, effects and solutions. In: Wong, C.S., Boyle, E., Bruland, K.W., Burton, J.D., Goldberg, E.D. (Eds.), Trace Metals in Sea Water, NATO Conf. Ser. 9. Plenum Press, New York, pp. 825–840. · DOI
  52. Kouwenhoven, 1997, Benthic foraminiferal assemblages between two major extinction events – the Paleocene El Kef section, Tunisia, Mar. Micropaleontol., 29, 105, 10.1016/S0377-8398(96)00030-8 · DOI
  53. Kramar, 1984, First experiences with a tube-excited energy-dispersive X-ray fluorescence, J. Geochem. Explor., 21, 373, 10.1016/0375-6742(84)90061-X · DOI
  54. Kramar, 1997, Advances in energy-dispersive X-ray fluorescence, J. Geochem. Explor., 58, 73, 10.1016/S0375-6742(96)00053-2 · DOI
  55. Li, 1998, Maastrichtian climate, productivity and faunal turnovers in planktic foraminifera in South Atlantic DSDP Sites 525A and 21, Mar. Micropaleontol., 33, 55, 10.1016/S0377-8398(97)00027-3 · DOI · Paper page
  56. Li, 2000, Late Cretaceous sea level changes in Tunisia: A multi-disciplinary approach, J. Geol. Soc. London, 157, 447, 10.1144/jgs.157.2.447 · DOI
  57. Luciani, 2002, High resolution planktic foraminiferal analysis form the Cretaceous/Tertiary boundary at Ain Settara (Tunisia): Evidence of an extended mass extinction, Palaeogeogr. Palaeoclimatol. Palaeoecol., 178, 299, 10.1016/S0031-0182(01)00400-X · DOI
  58. MacLeod, 1991, Hiatus distribution and mass extinction at the Cretaceous/Tertiary boundary, Geology, 19, 497, 10.1130/0091-7613(1991)019<0497:HDAMEA>2.3.CO;2 · DOI · Paper page
  59. McManus, 1998, Geochemistry of barium in marine sediments: Implications for its use as a paleoproxy, Geochim. Cosmochim. Acta, 62, 3453, 10.1016/S0016-7037(98)00248-8 · DOI
  60. McManus, 1999, Barium cycling in the North Pacific: Implications for the utility of Ba as a paleoproductivity and paleoalkalinity proxy, Paleoceanography, 14, 53, 10.1029/1998PA900007 · DOI
  61. Méon, 1990, Palynologic studies of the Cretaceous/Tertiary boundary interval at El Kef outcrop, north-western Tunisia: Paleogeographic implication, Rev. Paleobot. Palynol., 65, 85, 10.1016/0034-6667(90)90059-R · DOI
  62. Mitchell, 1997, Isotope data from cretaceous chalks and foraminifera: Environmental or diagenetic signals?, Geology, 25, 691, 10.1130/0091-7613(1997)025<0691:IDFCCA>2.3.CO;2 · DOI
  63. Molina, 1998, Mass extinction in planktic foraminifera at the Cretaceous/Tertiary boundary in subtropical to temperate latitudes, Bull. Soc. Geol. France, 169, 351
  64. Monaco, 1982, Critères mineralogiques pour la reconnaissance des turbidites fines, C.R. Acad. Sci. Paris Ser. II, 295, 43
  65. Murray, 1996, Scavenged excess aluminum and its relationship to bulk titanium in biogenic sediment from central equatorial Pacific Ocean, Geochim. Cosmochim. Acta, 60, 3869, 10.1016/0016-7037(96)00236-0 · DOI
  66. Oberhänsli, 1998, Diagenetically and environmentally controled changes across a K/T transition at Koshak Mangyshlak (Kazakstan), Bull. Soc. Geol. France, 169, 493
  67. Pardo, A., Ortiz, N., Keller, G., 1996. Latest Maastrichtian foraminiferal turnover and its environmental implications at Agost, Spain. In: MacLeod, N., Keller, G. (Eds.), Cretaceous-Tertiary Boundary Mass Extinction: Biotic and Environmental Changes. Norton Press, New York, pp. 139–172.
  68. Pardo, 1999, Paleoenvironmental changes across the Cretaceous-Tertiary boundary at Koshak, Kazakhstan, based on planktic foraminifera and clay mineralogy, Palaeogeogr. Palaeoclimatol. Palaeoecol., 154, 247, 10.1016/S0031-0182(99)00114-5 · DOI
  69. Paul, 1999, The Cenomanian–Turonian boundary at Eastbourne (Sussex, U.K): a proposed European reference section, Palaeogeogr. Palaeoclimatol. Palaeoecol., 150, 83, 10.1016/S0031-0182(99)00009-7 · DOI
  70. Perch-Nielsen, 1981, Les coccolithes du Paléocène près de El Kef, Tunisie, et leurs ancetres, Cah. Micropaléontol., 3, 7
  71. Perch-Nielsen, K, McKenzie, J.A., He, Q., 1982. Biostratigraphy and isotope stratigraphy and the ‘catastropic’ extinction of calcareous nannoplankton at the K/T boundary. In: Silver, L.T., Schulz, P.H. (Eds.), Geol. Soc. Am. Mem. 190, pp. 353–371. · DOI
  72. Peypouquet, 1986, Paleoceanography of the Mesogean Sea based on ostracods of the northern Tunisian continental shelf between the late Cretaceous and early Paleogene, Geol. Rundsch., 75, 159, 10.1007/BF01770185 · DOI
  73. Pospichal, 1994, Calcareous nannofossils at the K/T boundary, El Kef: No evidence of stepwise extinctions, Geology, 22, 99, 10.1130/0091-7613(1994)022<0099:CNATKT>2.3.CO;2 · DOI
  74. Rathburn, 1997, Magnesium and strontium compositions of recent benthic formainifera from the Coral Sea, Australia and Prydz Bay, Antarctica, Mar. Micropaleontol., 32, 231, 10.1016/S0377-8398(97)00028-5 · DOI
  75. Remane, 1999, International workshop on Cretaceous-Paleogene transitions in Tunisia: The El Kef stratotype for the Cretaceous-Paleogene boundary reconfirmed, Episodes, 22, 47
  76. Robert, 1991, Development of early Eocene warm climates, as inferred from clay mineral variations in oceanic sediments, Palaeogeogr. Palaeoclimatol. Palaeoecol., 89, 315, 10.1016/0031-0182(91)90169-R · DOI
  77. Robert, 1994, Antarctic subtropical humid episod at the Paleocene-Eocene boundary: Clay mineral evidence, Geology, 22, 211, 10.1130/0091-7613(1994)022<0211:ASHEAT>2.3.CO;2 · DOI
  78. Rocchia, 1995, L‘iridium à la limite Crétacé-Tertiaire du site d’El Kef Tunisia, Ann. Mines Géol., 35, 103
  79. Rocchia, R., Robin, E., Pierrard, O., Lefevre, I., 2002. The stratigraphic distribution of iridium and Ni-rich spinels at the Cretaceous–Tertiary boundary of El Kef, Tunisia. Palaeogeogr. Palaeoclimatol. Palaeoecol. In press.
  80. Rosenthal, 1997, Last glacial maximum paleochemistry and deepwater circulation in the Southern Ocean: Evidence from foraminiferal cadmium, Paleoceanography, 12, 787, 10.1029/97PA02508 · DOI
  81. Rosenthal, 1997, Temperature control on the incorporation of magnesium, strontium, fluorine and cadmium into benthic foraminiferal shells from Little Bahama Bank: Prospects for thermocline paleoceanography, Geochim. Cosmochim. Acta, 61, 3633, 10.1016/S0016-7037(97)00181-6 · DOI
  82. Rühlemann, 1996, Late quarternary productivity changes in the western equatorial Atlantic: Evidence from 230Th-normalised carbonate and organic carbon accumulation rates, Mar. Geol., 135, 127, 10.1016/S0025-3227(96)00048-5 · DOI
  83. Saint-Marc, 1992, Biogeographic and bathymetric distribution of benthic foraminifera in Paleocene El Haria Formation of Tunisia, J. Afric. Earth Sci., 15, 473, 10.1016/0899-5362(92)90029-C · DOI
  84. Schlanger, S.O., 1988. Strontium storage and release during deposition and diagenesis of marine carbonates related to sea level variations. In: Lerman, A., Meybeck, M. (Eds.), Physical and Chemical Weathering on Geochemical Cycles. Kluwer, Dordrecht, pp. 323–341. · DOI
  85. Schmitz, 1992, Stable isotope and foraminiferal changes across the Cretaceous/Tertiary boundary at Stevns Klint, Denmark: Arguments for long-term oceanic instability before and after bolide impact, Palaeogeogr. Palaeoclimatol. Palaeoecol., 96, 233, 10.1016/0031-0182(92)90104-D · DOI
  86. Schroeder, 1997, Barium in equatorial Pacific carboanate sediment: Terrigeous, oxide and biogenic associations, Paleoceanography, 12, 125, 10.1029/96PA02736 · DOI
  87. Shackelton, 1967, Oxygen isotope analyses and paleotemperatures reassessed, Nature, 215, 15, 10.1038/215015a0 · DOI
  88. Shackelton, N.J., 1987. The carbon isotope record of the Cenozoic: History of organic carbon burial and of oxygen in the ocean and atmosphere. In: Brooks, J., Fleet, A.J. (Eds.), Marine Petroleum Source Rocks. Geol. Soc. London Spec. Publ. 26, pp. 423–434. · DOI · Paper page
  89. Shackelton, 1983, Oygen and carbon isotope record of East Pacific core V19-30: implications for the formation of deep water in the late Pleistocene North Atlantic, Earth Planet. Sci. Lett., 65, 233, 10.1016/0012-821X(83)90162-0 · DOI
  90. Smit, J., 1982. Extinction and evolution of planktic foraminifera after a major impact at the Cretaceous/Tertiary boundary. Geol. Soc. Am. Spec. Pap. 190, pp. 329–352. · DOI
  91. Spero, 1997, Effect of seawater carbonate concentration on foraminiferal carbon and oxygen isotopes, Nature, 390, 497, 10.1038/37333 · DOI · Paper page
  92. Stinnesbeck, W., Keller, G., Adatte, T., 1998. Lithological characteristics of the K/T transition in Tunisia: Evidence of a tsunami event? In: International Workshop on Cretaceous–Tertiary Transition, Tunis, pp. 53–55.
  93. Stoll, 1996, Evidence for glacial control of rapid sea level changes in the early cretaceous, Science, 272, 1771, 10.1126/science.272.5269.1771 · DOI
  94. Stoll, 1998, Effects of Quaternary sea level cycles on strontium in seawater, Geochim. Cosmochim. Acta, 62, 1107, 10.1016/S0016-7037(98)00042-8 · DOI
  95. Stott, L.D., Kennet, J.P., 1990. The paleoceanographic and paleoclimatic signature of the Cretaceous/Paleogene boundary in the Antarctic: Stable isotope results from ODP Leg 113. In: Barker, P.F., Kennet, J.P. (Eds.). Proc. ODP Sci. Results 113, pp. 829–848. · DOI
  96. von Breymann, M.T., Emeis, K.-C., Suess, E., 1992. Water depth and diagenetic constraints on the use of barium as palaeoproductivity indicator. In: Summerhayes, C.P., Prell, W.L., Emeis, K.-C. (Eds.), Upwelling Systems: Evolution since Early Miocene. Geol. Soc. London Spec. Publ. 64, pp. 273–284. · DOI
  97. Weaver, C.E., 1989. Clays, Muds and Shales. Development in Sedimentology 44. Elsevier, Amsterdam, 819 pp.
  98. Zachos, 1986, Paleoceanography of the Cretaceous/Tertiary boundary event: Inferences from stable isotopic and other data, Paleoceanography, 1, 5, 10.1029/PA001i001p00005 · DOI
  99. Zachos, 1989, Geochemical evidence for suppression of pelagic marine productivity at the Createceous/Tertiary boundary, Nature, 337, 61, 10.1038/337061a0 · DOI

Cited by

Metadata

Authors
Stüben, D., Kramar, U., Berner, Z., Stinnesbeck, W., Keller, G., & Adatte, T.
Venue
Palaeogeography, Palaeoclimatology, Palaeoecology
Publisher
Elsevier BV
Published
2002-02
Volume
178
Issue
3-4
Pages
321-345
ISSN
0031-0182
DOI
10.1016/s0031-0182(01)00401-1
Cited by
63
References
1
Language
en
Licence
www.elsevier.com/tdm/userlicense/1.0/ (tdm)

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