570
Wagner and Dupont
Engel MH, Macko SA (1993) Organic geochemistry:
principles and applications. Plenum Press, New York
Espitalie J, Laporte JL, Madec M, Marquis F, Leplat P,
Paulet J, Boutefeu A (1977) Methode radide de
characterisation des roches-mere, de leur potential
petrolier et de leur degre d'evolution. Revue del
Institut Francais Petrole 32: 23-42
Espitalie J, Makadi KS, Trichetl (1984) Role of the minerai matrix during kerogen pyrolysis. Org Geochem
6:365-382
Fahl K, Stein R (1997) Modern organic carbon deposition in the Laptev Sea and the adjacent continental
slope: surface-water productivity vs. terrigenous
supply. Org Geochem 26 (5/6): 379-390
Fischer G, MUller Pl, Wefer G (1998) Latitudinal ;SlJC o • g
variations in sinking matter and sediments from the
South Atlantic: effects from anthropogenic CO, and
implications for palaeo-pCO,reconstructions. J Mar
Sci 17:471-495
Fontugne MR, Duplessy JC (1986) Variations of the
monsoon regime during the upper Quaternary: evidence from carbon isotopic record of OM in North
Indian Ocean sediments cores. Palaeogeogr
Palaeoclimatol Palaeoecol56: 69-88
Fredoux A (1994) Pollen analysis ofa deep-sea core in
the Gulf of Guinea: vegetation and climatic changes
during the last 225,000 years B.P. Palaeogeogr
Palaeoclimatol Palaeoecoll 09: 317-330
Gagosian RB, Peltzer ET (1985) The importance of atmospheric input ofterrestial organic material to deep
sea sediments. Org Geochem 10: 661-669
Giresse P, Maley l, Brenac P (1994) Late Quaternary
paleoenvironments in the Lake Barombi Mbo (West
Cameroon) deduced from pollen and carbon
isotopes of OM. Palaeogeogr Palaeoclimatol
Palaeoecol 107: 65-78
Gofii MA, Ruttenberg KC, Eglinton, TI (1997) Sources
and contribution of terrigenous organic carbon to
surface sediments in the Gulf of Mexico. Nature 389:
275-278.
Hamilton SE, Hedges J[ (1988) The comparative
geochemistries of lignins and carbohydrates in an
anoxic fjord. Geochim Cosmochim Acta 52: 129-142
Hebbeln D (1992) Weichselian glacial history of the
Svalbard area: correlating the marine and terrestrial
records. Boreas 21: 295-304
Hebbeln D, Henrich R, Baumann K-H (1998)
Paleoceanography of the last interglacial/glacial
cycle in the polar North Atlantic. Quat Sci Rev 17:
125-153
Hedges JI, Mann DC (1979) The lignin geochemistry of
marine sediments from the southern Washington
coast. Geochim Cosmochim Acta 43: 1809-1818
Henrich R, Kassens H, Vogelsang E, Thiede J (1989)
Sedimentary facies of glacial-interglacial cycles in
the Norwegian Sea during the last 350 ka. Mar Geol
86:283-319
Henrich R, Baumann KH., Wagner T (1997) Modem and
Quaternary pelagic and glaciomarine depositional
regimes in the Nordic Seas: response to climate forcing and ice sheet dynamics. Developments in
Marine Geology I: 1-36
Hiilemann JA, Henrich R (1994) Allochthonous versus
autochthonous OM in Cenozoic sediments of the
Norwegian Sea: evidence for the onset of glaciations
in the Northern Hemisphere. Mar Geol121 (1/2):
87-103
Hooghiemstra H (1989) Variations of the NW African
trade wind regime during the last 140,000 years:
changes in pollen flux evidenced by marine sediment
records. In: Leinen M, Sarnthein M (eds)
Paleoclimatology and Paleometeorology: modern
and past patterns of global atmospheric transport.
NATO ASI Series C 282, pp 733-770
Hooghiemstra H, Agwu COC (1988) Changes in the vegetation and trade winds in equatorial Northwest
Africa 140,000-70,000 yr BP, as deduced from two marine pollen records. Palaeogeogr Palaeoclimatol
Palaeoecol66: 173-213
Hooghiemstra H, Agwu COC, Beug HJ (1986) Pollen and
spore distribution in recent marine sediments: a
record ofNW-African seasonal wind patterns and
vegetation belts. "Meteor" Forsch Ergebn C 40:
87-135
Ittekkot V (1988) Global trends in the nature of OM in
river suspensions. Nature 332: 436-438
Jahns S, HUls M, Sarnthein M (1998) Vegetation and
climate history of west equatorial Africa based on a
marine pollen record off Liberia (Site GIK 16776) covering the last 400,000 years. Rev Palaeobot Palynol
102: 277-288
Jasper JP, Gagosian RB (1989) Glacial-interglacial climatically forced ;SlJC variations in sedimentary OM.
Nature 342: 60-62
Jasper JP, Gagosian RB (1990) The sources and deposition of OM in the Late Quaternary Pigmy Basin, Gulf
of Mexico. Geochim Cosmochim Acta 54: 1117-1132
Jones R W (1983) OM characteristics near the shelf-slope
boundary. SEPM Spec Pub133: 391-405
Jones RW (1987) Organic facies. Adv Petrol Geochem
2: 1-80
Katz BJ (1983) Limitations of "Rock Eva1" pyrolysis for
typing. Org Geochem 4 (3/4): 195-199
Wagner and Dupont
Engel MH, Macko SA (1993) Organic geochemistry:
principles and applications. Plenum Press, New York
Espitalie J, Laporte JL, Madec M, Marquis F, Leplat P,
Paulet J, Boutefeu A (1977) Methode radide de
characterisation des roches-mere, de leur potential
petrolier et de leur degre d'evolution. Revue del
Institut Francais Petrole 32: 23-42
Espitalie J, Makadi KS, Trichetl (1984) Role of the minerai matrix during kerogen pyrolysis. Org Geochem
6:365-382
Fahl K, Stein R (1997) Modern organic carbon deposition in the Laptev Sea and the adjacent continental
slope: surface-water productivity vs. terrigenous
supply. Org Geochem 26 (5/6): 379-390
Fischer G, MUller Pl, Wefer G (1998) Latitudinal ;SlJC o • g
variations in sinking matter and sediments from the
South Atlantic: effects from anthropogenic CO, and
implications for palaeo-pCO,reconstructions. J Mar
Sci 17:471-495
Fontugne MR, Duplessy JC (1986) Variations of the
monsoon regime during the upper Quaternary: evidence from carbon isotopic record of OM in North
Indian Ocean sediments cores. Palaeogeogr
Palaeoclimatol Palaeoecol56: 69-88
Fredoux A (1994) Pollen analysis ofa deep-sea core in
the Gulf of Guinea: vegetation and climatic changes
during the last 225,000 years B.P. Palaeogeogr
Palaeoclimatol Palaeoecoll 09: 317-330
Gagosian RB, Peltzer ET (1985) The importance of atmospheric input ofterrestial organic material to deep
sea sediments. Org Geochem 10: 661-669
Giresse P, Maley l, Brenac P (1994) Late Quaternary
paleoenvironments in the Lake Barombi Mbo (West
Cameroon) deduced from pollen and carbon
isotopes of OM. Palaeogeogr Palaeoclimatol
Palaeoecol 107: 65-78
Gofii MA, Ruttenberg KC, Eglinton, TI (1997) Sources
and contribution of terrigenous organic carbon to
surface sediments in the Gulf of Mexico. Nature 389:
275-278.
Hamilton SE, Hedges J[ (1988) The comparative
geochemistries of lignins and carbohydrates in an
anoxic fjord. Geochim Cosmochim Acta 52: 129-142
Hebbeln D (1992) Weichselian glacial history of the
Svalbard area: correlating the marine and terrestrial
records. Boreas 21: 295-304
Hebbeln D, Henrich R, Baumann K-H (1998)
Paleoceanography of the last interglacial/glacial
cycle in the polar North Atlantic. Quat Sci Rev 17:
125-153
Hedges JI, Mann DC (1979) The lignin geochemistry of
marine sediments from the southern Washington
coast. Geochim Cosmochim Acta 43: 1809-1818
Henrich R, Kassens H, Vogelsang E, Thiede J (1989)
Sedimentary facies of glacial-interglacial cycles in
the Norwegian Sea during the last 350 ka. Mar Geol
86:283-319
Henrich R, Baumann KH., Wagner T (1997) Modem and
Quaternary pelagic and glaciomarine depositional
regimes in the Nordic Seas: response to climate forcing and ice sheet dynamics. Developments in
Marine Geology I: 1-36
Hiilemann JA, Henrich R (1994) Allochthonous versus
autochthonous OM in Cenozoic sediments of the
Norwegian Sea: evidence for the onset of glaciations
in the Northern Hemisphere. Mar Geol121 (1/2):
87-103
Hooghiemstra H (1989) Variations of the NW African
trade wind regime during the last 140,000 years:
changes in pollen flux evidenced by marine sediment
records. In: Leinen M, Sarnthein M (eds)
Paleoclimatology and Paleometeorology: modern
and past patterns of global atmospheric transport.
NATO ASI Series C 282, pp 733-770
Hooghiemstra H, Agwu COC (1988) Changes in the vegetation and trade winds in equatorial Northwest
Africa 140,000-70,000 yr BP, as deduced from two marine pollen records. Palaeogeogr Palaeoclimatol
Palaeoecol66: 173-213
Hooghiemstra H, Agwu COC, Beug HJ (1986) Pollen and
spore distribution in recent marine sediments: a
record ofNW-African seasonal wind patterns and
vegetation belts. "Meteor" Forsch Ergebn C 40:
87-135
Ittekkot V (1988) Global trends in the nature of OM in
river suspensions. Nature 332: 436-438
Jahns S, HUls M, Sarnthein M (1998) Vegetation and
climate history of west equatorial Africa based on a
marine pollen record off Liberia (Site GIK 16776) covering the last 400,000 years. Rev Palaeobot Palynol
102: 277-288
Jasper JP, Gagosian RB (1989) Glacial-interglacial climatically forced ;SlJC variations in sedimentary OM.
Nature 342: 60-62
Jasper JP, Gagosian RB (1990) The sources and deposition of OM in the Late Quaternary Pigmy Basin, Gulf
of Mexico. Geochim Cosmochim Acta 54: 1117-1132
Jones R W (1983) OM characteristics near the shelf-slope
boundary. SEPM Spec Pub133: 391-405
Jones RW (1987) Organic facies. Adv Petrol Geochem
2: 1-80
Katz BJ (1983) Limitations of "Rock Eva1" pyrolysis for
typing. Org Geochem 4 (3/4): 195-199