Berger, W.H., Wefer, G., Richter, C., Lange, C.B., Giraudeau, J., Hermelin, O., and Shipboard Scientific Party, 1998. The Angola-Benguela upwelling system: paleoceanographic synthesis of shipboard results from Leg 175. In Wefer, G., Berger, W.H., and Richter, C., et al., Proc. ODP, Init. Repts., 175: College Station, TX (Ocean Drilling Program), 505-531.
Diester-Haass, L., Meyers, P.A., and Rothe, P., 1992. The Benguela Current and associated upwelling on the southwest African margin: a synthesis of the Neogene-Quaternary sedimentary record at DSDP Sites 362 and 352. In Summerhayes, C.P., Prell, W.L., and Emeis, K.C. (Eds.), Upwelling Systems: Evolution Since the Early Miocene. Geol. Soc. Spec. Publ. London, 64:331-342.
Emerson, S., and Hedges, J.I., 1988. Processes controlling the organic carbon content of open ocean sediments. Paleoceanography, 3:621-634.
Gooday, A.J., and Turley, C.M., 1990. Responses by benthic organisms to input of organic material to the ocean floor: a review. Philos. Trans R. Soc. London A, 331:119-138.
Herguera, J.C., and Berger, W.H., 1991. Paleoproductivity: glacial to postglacial change in the western equatorial Pacific, from benthic foraminifera. Geology, 19:1173-1176.
Lange, C.B., and Berger, W.H., 1993. Diatom productivity and preservation in the western equatorial Pacific: the Quaternary record. In Berger, W.H., Kroenke, L.W., Mayer, L.A., et al., Proc. ODP, Sci. Results, 130: College Station, TX (Ocean Drilling Program), 509-523.
Meyers, P.A., 1994. Preservation of elemental and isotopic source identification of sedimentary organic matter. Chem. Geol., 144:289-302.
————, 1997. Organic geochemical proxies of paleoceanographic, paleolimnologic, and paleoclimatic processes. Org. Geochem., 27:213-250.
Müller, G., and Gastner, M., 1971. The "Karbonat-Bombe," a simple device for the determination of the carbonate content in sediments, soils and other materials. Neues. Jahrb. Mineral. Monatsh., 10:466-469.
Nees, S., 1997. Late Quaternary palaeoceanography of the Tasman Sea: the benthic foraminiferal view. Palaeogeogr., Palaeoclimatol., Palaeoecol., 131:365-389.
Nelson, D.M., Treguer, P., Brzezinski, M.A., Leynaert, A., and Queguiner, B., 1995. Production and dissolution of biogenic silica in the ocean: revised global estimates, comparison with regional data and relationship to biogenic sedimentation. Global Biogeochem. Cycles, 9:359-372.
Schmiedl, G., and Mackensen, A., 1997. Late Quaternary paleoproductivity and deep water circulation in the eastern South Atlantic Ocean: evidence from benthic foraminifera. Palaeogeogr., Palaeoclimatol., Palaeoecol., 130:43- 80.
Siesser, W.G., 1980. Late Miocene origin of the Benguela upwelling system off northern Namibia. Science, 208:283-285.
Summerhayes, C.P., Kroon, D., Rosell-Melé, A., Jordan, R.W., Schrader, H.-J., Hearn, R., Villanueva, J., Grimalt, J.O., and Eglinton, G., 1995. Variability in the Benguela Current upwelling system over the past 70,000 years. Prog. Oceanogr., 35:207-251.
Verardo, D.J., Froelich, P.N., and McIntyre, A., 1990. Determination of organic carbon and nitrogen in marine sediments using the Carlo Erba NA-1500 Analyzer. Deep-Sea Res. Part A, 37:157-165.
Wefer, G., Berger, W.H., and Richter, C., et al., 1998. Proc. ODP, Init. Repts., 175: College Station, TX (Ocean Drilling Program).