Abstract
This is an interdisciplinary and synoptic study of Equatorial Atlantic sediment formation in the Late Quaternary aimed at untangling the interlaced signatures of terrigenous and biogenous deposition and early diagenesis. It is based on a stratigraphic network of 16 gravity core records arranged along one meridional and three zonal transects (4°N, 0° and 4°S) crossing the Amazon and Sahara plumes as well as the Equatorial Divergence high productivity region. All newly introduced sediment sequences are collectively dated by their coherent CaCO3 content profiles and two available δ18O age models. To infer proxy records indicative of individual fluxes and processes, we analyze environmental magnetic parameters describing magnetite concentration, magnetic grain sizes and magnetic mineralogy along with CaCO3, Corg, Fe, Mn, Ba and color data. Diagenetically affected layers are identified by a newly introduced Fe/κ index. Reach and climatic variability of the major regional sedimentation systems is delimited from lithological patterns and glacial/interglacial accumulation rate averages. The most prominent regional trends are the N-S decrease in terrigenous accumulation and the Equatorial Divergence high in glacial Corg accumulation, which decays much faster south- than northwards. Glacial enrichments in Corg and proportional depletions in CaCO3, content appear to reflect sedimentary carbonate diagenesis more than lysoclinal oscillations and dominate temporal lithology changes. Suboxic iron mineral reduction is low at Ceara Rise and Sierra Leone Rise, but more intense on both flanks of the Mid-Atlantic ridge, where it occurs within organic rich layers deposited during oxygen isotope stages 6, 10 and 12, in particular at the terminations. To the equator, these zones reflect a full precessional rhythm with individual diagenesis peaks merging into broader magnetite-depleted zones. Rock magnetic and geochemical data show, that the depths of the Fe3+/Fe2+ redox boundary in the Equatorial Atlantic are not indicative of average productivity and were frequently shifted in the past. They are now located just above the topmost preserved productivity pulse. At 4°N, this organically enriched layer coincides with glacial stage 6, at 0° with glacial stage 2. Subsequent oxic and suboxic degradation of organic material entails stratigraphically coincident carbonate and magnetite losses opening new analytical perspectives.
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References
Archer D, Maier-Reimer E (1994) Effect of deep-sea sedimentary calcite preservation on atmospheric CO2 concentration. Nature 367: 260–263
Bassinot FC, Labeyrie LD, Vincent E, Quidelleur X, Shakelton NJ, Lancelot Y (1994) The astronomical theory of climate and the age of the Brunhes-Matuyama magnetic reversal. Earth Planet Sci Lett 126: 546–559
Bickert T (1992) Rekonstruktion der spätquatären Bodenwasserzirkulation im östlichen Südatlantik über stabile Isotope bentischer Foraminiferen. Ber Fachber Geowiss, Univ Bremen 27, 205 p
Bickert T, Wefer G (1996) Late Quaternary deep water circulation in the South Atlantic: Reconstruction from carbonate dissolution and benthic stable isotopes. In: Wefer G, WH Berger, Siedler G, Webb DJ (eds) The South Atlantic: Present and Past Circulation. Springer, Berlin, pp 599–620
Bishop JKB (1988) The barite-opal-organic carbon association in oceanic particulate matter. Nature 332: 341–343
Bloemendal J, King JW, Hall FR, Doh S-J (1992) Rock magnetism of late Neogene and Pleistocene deep-sea sediments: Relationship to sediment source, diagenetic processes, and sediment lithology. J Geophys Res 97: 4361–4375
Bloemendal J, Lamb B, King J (1988) Paleoenvironmental implications of rock — magnetic pro-perties of late Quaternary sediment cores from the eastern equatorial Atantic. Paleoceanography 3: 61–87
Bonifay D, Giresse P (1992) Middle to Late Quaternary sediment flux and post-depositional processes between the continental slope off Gabon and the Mid-Guinean margin. Mar Geol 106: 107–129
Boyle EA, Keigwin LD (1982) Deep circulation of the North Atlantic over the last 200,000 years: Geochemical evidence. Science 218: 784–787
Boyle EA, Keigwin LD (1985) Comparison of Atlantic and Pacific paleochemical records for the last 215,000 years: Changes in deep ocean circulation and chemi-cal inventories. Earth Planet Sci Lett 76: 135–140
Broecker WS, Denton GH (1989) The role of oceanatmosphere reorganisations in glacial cycles. Geochim Cosmochim Acta 53: 2465–2501
Brummer GJA, Van Eijden AJM (1992) ‘Blue-ocean’ paleoproductivity estimates from pelagic carbonate mass accumulation rates. Mar Micropaleontol 19: 99–117
Canfield DE, Berner RA (1987) Dissolution and pyritization of magnetite in anoxic marine sediments. Geochim Cosmochim Acta 51: 645–659
Colley S, Thomson J, Wilson TRS, Higgs NC (1984) Post-depositional migration of elements during diagenesis in brown clay and turbidite sequences in the North East Atlantic. Geochim Cosmochim Acta 48: 1223–1235
Curry WB, Lohmann GP (1986) Late Quaternary sedimentation at the Sierra Leone Rise (eastern equatorial Atlantic Ocean). Mar Geol 70: 223–250
Curry WB, Lohmann GP (1990) Reconstructing past particle fluxes in the tropical Atlantic Ocean. Paleoceanography 5: 487–506
Curry WB (1996) Late Quaternary deep circulation in the western Equatorial Atlantic. In: Wefer G, Berger WH, Siedler G, Webb D (eds) The South Atlantic: Present and Past Circulation. Springer, Berlin, pp 577–598
Damuth JE (1977) Late Quaternary sedimentation in the western equatorial Atlantic. Geol Soc Am Bull 88: 695–710
deMenocal PB, Ruddiman WF, Pokras EM (1993) Influences of high-and low-latitude processes on African terrestrial climate: Pleistocene eolian records from equatorial Atlantic ocean drilling program Site 663. Paleoceanography 8: 209–242
Dunlop DJ (1973) Superparamagnetic and single-domain threshold sizes in magnetite. J Geophys Res 78:1780–1793
Duplessy J C, Labeyrie L, Paterne M, Hovine S, Fichefet T, Duprat J, Labracherie M (1996) High latitude deep water sources during the Last Glacial Maximum and the intensity of the global oceanic circulation. In: Wefer G, Berger WH, Siedler G, Webb D (eds) The South Atlantic: Present and Past Circulation. Sprin-ger, Berlin, pp 445–460
Dupont LM, Jahns S, Marret F, Ning S (2000) Vegetation change in equatorial West Africa: Time-slices for the last 150 ka. Palaeogeogr Palaeoclimatol Palaeoecol 155: 95–122
Fischer G and participants (1998) Report and preliminary results of METEOR cruise M38/1, Las Palmas — Recife, 25.1.–1.3.1997. Ber Fachber Geowiss, Univ Bremen 94, 178 p
François R, Bacon MP (1991) Variations in terrigenous input into the deep Equatorial Atlantic during the past 24,000 years. Science 251: 1473–1475
François R, Bacon MP, Suman DO (1990) Thorium 230 profiling in deep-sea sediments: High-resolution records of flux and dissolution of carbonate in the equatorial Atlantic during the last 24000 years. Paleoceanography 5: 761–787
Frederichs T, Bleil U, Däumler K, von Dobeneck T, Schmidt A (1999) The magnetic view on the marine paleoenvironment: Parameters, techniques, and potentials of rock magnetic studies as a key to paleoclimatic and paleoceanographic changes. In: Fischer G, Wefer G (eds) Use of Proxies in Paleoceanography: Examples from the South Atlantic. Springer, Berlin, pp 575–599
Froelich PN, Klinkhammer GP, Bender ML, Luedtke NA, Heath GR, Cullen D, Dauphin P, Hammond D, Hartman B, Maynard V (1979) Early oxidation of organic matter in pelagic sediments of the eastern equatorial Atlantic: Suboxic diagenesis. Geochim Cosmochim Acta 43: 1075–1090
Gardner JV, Burkle LH (1975) Upper Pleistocene Ethmodiscus rex from the eastern equatorial Atlantic. Micropaleontology 21: 236–242
Gingele F, Dahmke A (1994) Discrete barite particles and barium as tracers of paleoproductivity in South Atlantic sediments. Paleoceanography 9: 151–168
Gingele FX, Zabel M, Kasten S, Bonn WJ, Nürnberg CC (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 the South Atlantic. Springer, Berlin, pp 345–364
Haese RR, Petermann H, Dittert L, Schulz HD (1998) The early diagenesis of iron in pelagic sediments: A multidisciplinary approach. Earth Planet Sci Lett 157: 233–248.
Higgs HC, Thomson J, Wilson TRS, Croudace IW (1994). Modification and complete removal of eastern Medi-terranean sapropels by postdepositional oxidation. Geology 22: 423–426
Jansen JHF, Van der Gaast SJ, Koster AJ (1998) CORTEX, a shipboard XRF-scanner for element analyses in split sediment cores. Mar Geol 151: 143–153
Johns WE, Schott FA, Zantopp RJ, Evans RH (1990) The North Brazil Current retroflexion: Seasonal structure and eddy variability, J Geophys Res 95: 22103–22120
Karlin R, Levi S (1983) Diagenesis of magnetic minerals in recent haemipelagic sediments. Nature 303:327–330
Karlin R, Levi S (1985) Geochemical and sedimentologi-cal control of the magnetic properties of hemipelagic sediments. J Geophys Res 90: 10,373–10,392
Karlin R, Lyle M, Heath GR (1987) Authigenic magnetic formation in suboxic marine sediments. Nature 326: 490–493
Karlin R (1990) Magnetite diagenesis in marine sediments from the Oregon continental margin. J Geophys Res 95: 4405–4419
Kasten S, Haese RR, Zabel M, Ruhlemann C, Schulz HD (2001) Barium peaks at glacial terminations in sediments of the equatorial Atlantic Ocean — relicts of deglacial productivity pulses? Chem Geol 175: 635–651
Kidd RB, Cita MB, Ryan WBF (1978) Stratigraphy of eastern Mediterranean sapropel sequences recovered during DSDP Leg 42A and their paleoenvironmental significance. In: Hsü KJ et al. (eds) Initial Reports of the Deep-Sea Drilling Project. US Government Printing Office, Washington, pp 421–443
Kumar N, Embley RW (1977) Evolution and origin of Ceará Rise: An aseismic rise in the western equatorial Atlantic. Geol Soc Am Bull 88: 683–694
Kutzbach JE (1981) Monsoon climate of the early Holocene: Climatic experiment with the Earth’s orbital parameters for 9000 years ago. Science 214: 59–61
Lutjeharms JRE (1996) The exchange of water between the South Indian and South Atlantic Oceans. In: Wefer G, Berger WH, Siedler G, Webb D (eds) The South Atlantic: Present and Past Circulation. Springer, Berlin, pp 125–162
Lyle M (1983) The brown-green color transition in marine sediments: A marker of the Fe(III)-Fe(II) redox boundary. Limnol Oceanogr 28: 1026–1033
Lyle M (1988) Climatically forced organic carbon burial in equatorial Atlantic and Pacific Oceans. Nature 335: 529–532
Maher BA (1988) Magnetic properties of some synthetic submicron magnetites. Geophys J 94: 83–96
Martin WR, Sayles FL (1996) CaCO3 dissolution in sediments of the Ceara Rise, western equatorial Atlantic. Geochim Cosmochim Acta 60: 243–263
Maslin M, Mikkelsen N (1997) Amazon fan mass-transport deposits and underlying interglacial deposits: Age estimates and fan dynamics. Proc ODP Sci Results 155:353–365
Meinecke G (1992) Spätquartäre Oberflächenwasser-temperaturen im östlichen äquatorialen Atlantik. Ber Fachber Geowiss, Univ Bremen 29, 181 p
Mercone D, Thomson J, Croudace IW, Siani G, Paterne M, Troelsta S (2000) Duration of S1, the most recent sapropel in the eastern Mediterranean Sea, as indicated by accelerator mass spectrometry radiocarbon and geochemical evidence. Paleoceanography 15: 336–347
Milliman JD, Summerhayes CP, Barretto HT (1975) Qua-ternary sedimentation on the Amazon continental margin: A model. Geol Soc Am Bull 86: 610–614
Milliman JD (1993) Production and accumulation of calcium carbonate in the ocean: Budget of a nonsteady. Glob Biochem Cycl 7: 927–957
Mix AC, Rugh W, Pisias N G, Veirs S (1992) Color reflec-tance spectroscopy: A tool for rapid charakterization of deep-sea sediments. Proc ODP, Initial Reports 138: 67–77
Müller PJ, Erlenkeuser H, v Grafenstein R (1983) Glacial — interglacial cycles in oceanic productivity inferred from organic carbon contents in eastern north Atlantic sediment cores. In: Thiede J, Suess E (eds) Coastal Upwelling Part B. Plenum Press, New York, USA, pp 365–398
Müller PJ, Hartmann M, Suess E (1988) The chemical environment of pelagic sediments. In: Halbach P, Friedrich G, von Stackelberg U (eds) The manganese nodule belt of the Pacific Ocean. Enke, Stuttgart, 254 p
Oppo DW, Fairbanks RG (1987) Variability in the deep and intermediate water circulation of the Atlantic Ocean during the past 25,000 years: Northern Hemis-phere modulation of the Southern Ocean. Earth Planet Sci Lett 86: 1–15
Parry LG (1965) Magnetic properties of dispersed magnetite powders. Philosophical Magazine 11: 303–312
Passier HF, Dekkers MJ, de Lange GJ (1998) Sediment chemistry and magnetic properties in an anomalously reducing core from the eastern Mediterranean Sea. Chem Geol 152: 287–306
Passier HF, Dekkers MJ (2002) Assessment of the formation of iron oxides in the active oxidation front above sapropel S 1 in the eastern Mediterranean Sea by low-temperature magnetic properties. Geophys J Int, in press
Petermann H, Bleil U (1993) Detection of live magnetotactic bacteria in South Atlantic deep-sea sediments. Earth Planet Sci Lett 117: 223–228
Pfeifer K, Hensen C, Adler M, Wenzhöfer F, Weber B, Schulz HD (2002) Modeling of subsurface calcite dissolution — including the respiration and re-oxidation processes of marine sediments in the region of the equatorial upwelling off Gabon. Geochim Cosmochim Acta 66: 4247–4259
Pickard GL, Emery WJ (1990) Descriptive Physical Oceanography. Pergamon Press Oxford UK, 320 p
Rath S, Wagner T, Henrich S (1999) Pleistozäne Schwankungen im Staubeintrag und in der Karbonaterhaltung im äquatorialen Atlantik (ODP Site 663) zwischen 480 und 390 Ka: Hinweise aus KorngroBen-analysen. Zentralblatt Geologie-Palaontologie Teil I H 7–10: 1–19
Ratmeyer V, Balzer W, Bergametti G, Chiapello I, Fischer G, Wyputta U (1999a) Seasonal impact of mineral dust on deep-ocean particle flux in the eastern subtropical Atlantic Ocean. Mar Geol 159: 241–252
Ratmeyer V, Fischer G, Wefer G (1999b) Lithogenic particle fluxes and grain size distributions in the deep ocean off northwest Africa: Implications for seasonal changes of aeolian dust input and downward trans-port. Deep-Sea Res 46: 1289–1337
Raymo ME, Ruddiman WF, Shakleton NJ, Oppo DW (1990) Evolution of Atlantic — Pacific δ13C gradients over the last 2.5 my. Earth Planet Sci Lett 97: 353–368
Raymo ME, Oppo DW, Curry W (1997) The mid-Pleistocene climate transition: A deep-sea carbon isotopic perspective. Paleoceanography 12: 546–559
Rhein M, Schott F, Fischer J, Send U, Stramma L (1996) The deep water regime in the Equatorial Atlantic. In: Wefer G, Berger WH, Siedler G, Webb D (eds) The South Atlantic: Present and Past Circulation. Springer, Berlin, pp 261–271
Robinson SG, Sahota JTS, Oldfield F (2000) Early diagenesis in North Atlantic abyssal plain sediments characterized by rock magnetic and geochemical indices. Mar Geol 163: 77–107
Röhl U, Abrams LJ (2000) High-resolution, downhole, and nondestructive core measurements from Sites 999 and 1001 in the Caribbean Sea: Application to the Late Paleocene thermal maximum. In: Leckie RM, Sigurdsson H, Acton GD, Draper G (eds) Proc ODP Sci Results. College Station Texas, pp 191–203
Rossignol-Strick M, Nesteroff W, Olive P, Vergnaud-Grazzini C (1982) After the deluge: Mediterranean stagnation and sapropel formation. Nature 295:105–110
Ruddiman WF (1997) Tropical Atlantic terrigenous fluxes since 25,000 yrs BP. Mar Geol 136: 189–207
Ruddiman WF, Janecek TR (1989) Pliocene-Pleistocene biogenic and terrigenous fluxes at equatorial Atlantic Sites 662, 663, and 664. In: Ruddiman W, Sarnthein M (eds) Proc ODP Sci Results. College Station, Texas pp 211–240
Rühlemann C, Frank M, Hale W, Mangini A, Mulitza S, Muller PJ, Wefer G (1996) Late Quaternary productivity changes in the western equatorial Atlantic: Evidence from 230Th-normalized carbonate and organic carbon accumulation rates. Mar Geol 135: 127–152
Sahota JTS, Robinson SG, Oldfield F (1995) Magnetic measurements used to identify paleoxidation fronts from the Madeira abyssal plain. Geophys Res Lett 22: 1961–1964
Sarnthein M, Tetzlaff G, Koopmann B, Wolter K, Pflaumann, U 1981. Glacial and interglacial wind regimes over the eastern subtropical Atlantic and North-West Africa. Nature 293: 193–196
Sarnthein M, Thiede J, Pflaumann U, Erlenkeuser H, Fütterer D, Koopmann B, Lange H, Seibold E (1982) Atmospheric and oceanic circulation patterns off Northwest Africa during the past 25 million years. In: von Rad U, Hinz K et al. (eds) Geology of the Northwest African Continental Margin. Springer, Berlin, pp 545–604
Sarnthein M, Winn K, Jung S JA, Duplessy J-C, Labeyrie L, Erlenkeuser H, Ganssen G (1994) Changes in east Atlantic deepwater circulation over the last 30,000 years: Eight time slice reconstructions. Paleoceanography 9: 209–267
Schmieder F, von Dobeneck T, Bleil U (2000) The Mid-Pleistocene climate transition as documented in the deep South Atlantic Ocean: Initiation, interim state and terminal event. Earth Planet Sci Lett 179: 539–549
Schneider RR, Schulz HD, Hensen C (2000) Marine carbonates: Their formation and destruction. In: Schulz HD, Zabel M (eds) Marine Geochemistry. Springer, Berlin, pp 283–307
Schulte S, Bard E (2003) Past changes of biologically mediated dissolution of calcite above the chemycal lysocline documented in Indian Ocean sediments. Quater Sci Rev 22: 1757–1770
Schulz, HD and participants (1991) Report and preliminary results of Meteor cruise M16/2, Recife — Belem, 28.4.–20.5.1991. Ber Fachber Geowiss, Univ Bremen 19, 149 p
Showers WJ, Angle DG (1986) Stable isotopic characterization of organic carbon accumulation on the Amazon continental shelf. Continent Shelf Res 6: 227–244
Stolz JF (1992) Magnetotactic Bacteria: Biomineralization, Ecology, Sediment Magnetism, Environ-mental Indicator. In: Skinner HGW, Fitzpatrick RW (eds) Biomineralization processes of iron and manganese. Catena-Verl Cremlingen-Destedt, pp 133–145
Street-Perrott FA, Perrott RA (1990) Abrupt climate fluctuations in the tropics: The influence of Atlantic Ocean circulation. Nature 343: 607–612
Tarduno JA (1994) Temporal trends of magnetic dissolu-tion in the pelagic realm: Gauging paleoproductivity? Earth Planet Sci Lett 123: 39–48
Tarduno JA, Tian W, Wilkison S (1998) Biogeochemical remanent magnetization in pelagic sediments of the western equatorial Pacific Ocean. Geophys Res Lett 25: 3987–3990
Tarduno JA, Wilkison SL (1996) Non-steady state magnetic mineral reduction, chemical lock-in, and delayed remanence acquisition in pelagic sediments. Earth Planet Sci Lett 144: 315–326
Thießen W (1993) Magnetische Eigenschaften von Sedimenten des östlichen Südatlantiks und ihre paläozeanographische Relevanz. Ber Fachber Geowiss, Univ Bremen 4, 170 p
Thomson J, Higgs NC, Wilson TRS, Croudace IW, de Lange GJ, van Santvoort, PJM (1995) Redistribution and geochemical behaviour of redox — sensitive elements around S 1, the most recent eastern Mediterranean sapropel. Geochim Cosmochim Acta 59: 3487–3501
Tiedemann R, Sarnthein M, Shackleton NJ (1994) Astronomic timescale for the Pliocene Atlantic δ18O and dust flux records of Ocean Drilling Program Site 659. Paleoceanography 9: 619–638
Tiedemann R, Sarnthein M, Stein R (1989) Climatic changes in the western Sahara: Aeolo-marine sediment record of the last 8 million years (Sites 657–661) In: Ruddimann W, Sarnthein M et al. (eds) Proc ODP Sci Results. Vol 108, pp 241–277
van Kreveld S A, Knappertsbusch M, Ottens J, Ganssen GM, van Hinte JE (1996) Biogenic carbonate and ice-rafted debris (Heinrich layer) accumulation in deep-sea sediments from a Northeast Atlantic piston core. Mar Geol 131: 21–46
van Santvoort PJM, de Lange GJ, Thomson J, Cussen H, Wilson TRS, Krom MD, Ströhle K (1996) Active post-depositional oxidation of the most recent sapropel (S1) in sediments of the eastern Mediterranean Sea. Geochim Cosmochim Acta 60: 4007–4024
van Santvoort PJM, de Lange GJ, Langereis CG, Dekkers MJ, Paterne M (1997) Geochemical and paleomag-netic evidence for the occurence of ‘missing’ sapropels in eastern Mediterranean sediments. Paleoceanography 12: 773–786
Verardo DJ, McIntyre A (1994) Production and destruction: Control of biogenous sedimentation in the tropical Atlantic 0–300,000 years BP. Paleoceanography 9: 63–86
von Dobeneck T (1996) A sytematic analysis of natural magnetic mineral assemblages based on modelling hysteresis loops with coercivity-related hyberbolic basis functions. Geophys J Int 124: 675–694
von Dobeneck T (1998) The concept of ‘partial susceptibilities’. Geologica Carpathica 49: 228–229
von Dobeneck T, Schmieder F (1999) Using rock magnetic proxy records for orbital tuning and extented time series analyses into the Super-and Sub-Milankovitch bands. In: Fischer G, Wefer G (eds) Use of Proxies in Paleoceanography: Examples from the South Atlantic. Springer; Berlin, pp 601–633
Wagner T (2002) Organic sedimentation in the Equatorial Atlantic: Evolution from Cretaceous to early Quaternary depositional environments. Palaeogeogr Palaeoclimatol Palaeoecol 179: 113–147
Wagner T (2000) Control of organic carbon accumulation in the late Quaternary equatorial Atlantic (Ocean Drilling Program sites 664 and 663): Productivity versus terrigenous supply. Paleoceanography 15: 181–199
Wagner T, Dupont LM (1999) Terrestrial organic matter in marine sediments: Analytical approaches and eolian-marine records in the Central Equatorial Atlantic. In: Fischer G, Wefer G (eds) Use of Proxies in Paleoceanography: Examples from the South Atlantic. Springer, Berlin, pp 547–574
Wefer G, Berger W H, Bickert T, Donner B, Fischer G, Kemle-von Mücke S, Meinecke G, Müller P J, Mulitza S, Niebler H-S, Pätzold J, Schmidt H, Schneider R R, Segl M (1996) Late Quaternary surface circulation in the South Atlantic: The stable isotope record and implications for heat transport and productivity. In: Wefer G, Berger WH, Siedler G, Webb D (eds) The South Atlantic: Present and Past Circulation. Springer, Berlin, pp 461–502
Wefer G and participants (1988) Report and preliminary results of Meteor cruise M6/6, Libreville — Las Palmas, 18.2.–23.3.1988. Ber Fachber Geowiss, Univ Bremen 3, 97 p
Wefer G and participants (1989) Report and preliminary results of Meteor cruise M9/4, Dakar — Santa Cruz, 19.2.–16.3.1989. Ber Fachber Geowiss, Univ Bremen 7, 103 p
Wefer G and participants (1991) Report and preliminary results of Meteor cruise M16/1, Pointe Noir — Recife, 27.3.–25.4.1991. Ber Fachber Geowiss, Univ Bremen 18, 120 p
Wefer G and participants (1994) Report and preliminary results of Meteor cruise M23/3, Recife — Las Palmas, 21.3.–12.4.1993. Ber Fachber Geowiss, Univ Bremen 44, 71 p
Wilson TRS, Thomson J, Colley S, Hydes DJ, Higgs NC, Sorensen J (1985) Early organic diagenesis: The significance of progressive subsurface oxidation fronts in pelgic sediments. Geochim Cosmochim Acta 49: 811–822
Wilson TRS, Thomson J, Hydes DJ, Colley S, Culkin F, Sorensen J (1986) Oxidation fronts in pelagic sedi-ments: Diagenetic formation of metal-rich layers. Science 232: 972–975
Wilson TRS, Thomson J (1998) Calcite dissolution accompanying early diagenesis in turbiditic deep ocean sediments. Geochim Cosmochim Acta 62: 2087–2096
Zabel M, Bickert T, Dittert L, Haese RR (1999) Significance of the sedimentary Al:Ti ratio as an indicator for variations in the circulation patterns of the equatorial North Atlantic. Paleoceanography 14: 789–799
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Funk, J.A., von Dobeneck, T., Wagner, T., Kasten, S. (2003). Late Quaternary Sedimentation and Early Diagenesis in the Equatorial Atlantic Ocean: Patterns, Trends and Processes Deduced from Rock Magnetic and Geochemical Records. In: Wefer, G., Mulitza, S., Ratmeyer, V. (eds) The South Atlantic in the Late Quaternary. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-642-18917-3_21
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