Terrestrial Organic Matter in Marine Sediments
571
Koopmann B (1981) Saharan dust deposition in the
northern subtropical Atlantic during the last 25,000
years. "Meteor" Forsch Ergebn C 35: 23-59
Laine EP, Gardner WD, Richardson MJ, Kominz M (1994)
Abyssal currents and advection of resuspended
sediment along the northeastern Bermuda Rise. Mar
Geo1119: 159-171
Lallier-Verges E, Bertrand P, Berner U (1990) Optical and
geochemical study of organic matter in present oxic
sediments (equatorial North Pacific Ocean, NIOX
area). Oceanol Acta (Spec Vol) 10: 281-291
Lallier-Verges E, Bertrand P, Desprairies A (1993) OM
composition and sulfate reduction intensity in Oman
Margin sediments. Mar Geol 112: 57-69
Langford FF, Blanc-Valleron MM (1990) Interpreting
Rock-Eva1 Pyrolysis data using graphs ofpyrolizable
hydrocarbons vs. Total Organic Carbon. AAPG Bull
74(6): 799-804
Liebezeit G, Wiesner MG (1990) Pyroysis of recent marine sediments - I. Biopolymers. Org Geochem 16
(4-6): 1179-1185
Littke R (1993) Deposition, diagensis, and weathering
of OM-rich sediments. Lecture Notes in Earth Sciences 47: 0-216
Littke R, Sachseuhofer RF (1994) Organic petrology of
deep sea sediments: a compilation of results from the
Ocean Drilling Program and the Deep Sea Drilling
Project. Energy & Fuels 8: 1498-1512
Littke R, Baker DR, Rullktitter J (1997a) Deposition of
petroleum source rocks. In: Welte DH, Horsfield B,
Baker DR (eds) Petroleum and Basin Evolution.
Springer, Berlin, pp 271-334
Littke R, Luckge A, Welte DH (1997b) Quantification of
organic matter degradation by microbial sulfate reduction for Quaternary sediments from the Northern Arabian Sea. Geowissenschaften 84: 312-315.
Uickge A (1997) Ablagerung und Friihdiagenese
organischen Materials in marinen Hochproduktionsgebieten. Ber Forschungszentr Jiilich 3413, pp 1-166.
Liickge A, Boussafir M, Lallier-Verges E, Littke R (1996)
Comparative study of organic matter preservation
in immature sediments along the continental margins
of Peru and Oman. Part I: Results of petrographic and
bulk geochemical data. Org Geochem 24(4): 437-451.
Mackenzie FT (1981) Global carbon cycles: some minor
sinks for CO,. In: Lickens GE, Mackenzie TF, Richey
JE, Sedell JR, Turekian KK (eds) Flux of organic carbon by rivers to the oceans. US Dept of Energy,
Washington DC, pp 360-384
Mariotti A, Gadel F, Giresse P, Kinga-Mouzeo (1991)
Carbon isotope composition and geochemistry of
particulate OM in the Congo River (Central Africa):
application to the study of Quaternary sediments off
the mouth of the river. Chern Geo186: 345-357
Marret F (1994) Evolution paleoclimatique et
paleohydrologique de I' Atlantique est-equatorial et
du proche continent au Quaternaire terminal. Contribution palynologique (kystes de dinoflagelles,
pollen et spores). Thesis Univ Bordeaux I, pp 1-255
McCave IN (1986) Local and global aspects of the bottom nepheloid layers in the world ocean. Neth ] Sea
Res 20 (2/3): 167-181
Michaelis W, Ittekkot V, Degen ET (1986) River inputs
into oceans. In: Lassere P, Martin 1M (eds) Biochemical processes at the Land-sea Boundary. Elsevier,
Amsterdam, pp 37-52
Mix AC (1989) Influence of productivity variations on
long-term atmospheric CO,. Nature 337: 541-544
Miiller PJ (1977) CIN ratios in Pacific deep-sea
sediments: Effect on inorganic ammonium and organic nitrogen compounds sorbed by clays.
Geochim CosmochimActa41: 765-776
Muller PJ, Suess E (1979) Productivity, sedimentation
rate, and sedimentary OM in the oceans - 1. Organic
carbon preservation. Deep-Sea Res 26 (A):
1347-1362
Miiller PJ, Erlenkeuser H, von 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: Its sedimentary record, Part B.
Plenum Press, New York, pp 365-393
Muller PJ, Schneider RR, Ruhland G (1994) Late Quaternary pCO 2 variations in the Angola Current: evidence
from organic carbon 8 13 C alkenone temperatures. In
Zahn R, Pedersen TF, Kaminski MA, Labeyrie L (eds)
Carbon Cycling in the Glacial Ocean: Constraints on
the Ocean's Role in Global Change. NATO ASI
Series, Vol 17, Springer, Berlin Heidelberg New York,
pp 343-366
Peters KE (1986) Guidelines for evaluating petroleum
source rock using programmed pyrolysis. AAPG 70
(3):318-329
Pokras EM, Mix AC (1985) Eolian evidence for spatial
variability of Late Quaternary climates in tropical
Africa. Quat Res 24: 137-149
Powell TG, Creaney S, Snowdon LR(1982) Limitations
of use of Organic Petrographic Techniques
for identification of Petroleum Source Rocks. AAPG
66 (4): 430-435
Poynter JG, Eglinton G (1991) A biomarker conceptstrengths and weaknesses. Fresenius J Anal Chern
339: 725-731
571
Koopmann B (1981) Saharan dust deposition in the
northern subtropical Atlantic during the last 25,000
years. "Meteor" Forsch Ergebn C 35: 23-59
Laine EP, Gardner WD, Richardson MJ, Kominz M (1994)
Abyssal currents and advection of resuspended
sediment along the northeastern Bermuda Rise. Mar
Geo1119: 159-171
Lallier-Verges E, Bertrand P, Berner U (1990) Optical and
geochemical study of organic matter in present oxic
sediments (equatorial North Pacific Ocean, NIOX
area). Oceanol Acta (Spec Vol) 10: 281-291
Lallier-Verges E, Bertrand P, Desprairies A (1993) OM
composition and sulfate reduction intensity in Oman
Margin sediments. Mar Geol 112: 57-69
Langford FF, Blanc-Valleron MM (1990) Interpreting
Rock-Eva1 Pyrolysis data using graphs ofpyrolizable
hydrocarbons vs. Total Organic Carbon. AAPG Bull
74(6): 799-804
Liebezeit G, Wiesner MG (1990) Pyroysis of recent marine sediments - I. Biopolymers. Org Geochem 16
(4-6): 1179-1185
Littke R (1993) Deposition, diagensis, and weathering
of OM-rich sediments. Lecture Notes in Earth Sciences 47: 0-216
Littke R, Sachseuhofer RF (1994) Organic petrology of
deep sea sediments: a compilation of results from the
Ocean Drilling Program and the Deep Sea Drilling
Project. Energy & Fuels 8: 1498-1512
Littke R, Baker DR, Rullktitter J (1997a) Deposition of
petroleum source rocks. In: Welte DH, Horsfield B,
Baker DR (eds) Petroleum and Basin Evolution.
Springer, Berlin, pp 271-334
Littke R, Luckge A, Welte DH (1997b) Quantification of
organic matter degradation by microbial sulfate reduction for Quaternary sediments from the Northern Arabian Sea. Geowissenschaften 84: 312-315.
Uickge A (1997) Ablagerung und Friihdiagenese
organischen Materials in marinen Hochproduktionsgebieten. Ber Forschungszentr Jiilich 3413, pp 1-166.
Liickge A, Boussafir M, Lallier-Verges E, Littke R (1996)
Comparative study of organic matter preservation
in immature sediments along the continental margins
of Peru and Oman. Part I: Results of petrographic and
bulk geochemical data. Org Geochem 24(4): 437-451.
Mackenzie FT (1981) Global carbon cycles: some minor
sinks for CO,. In: Lickens GE, Mackenzie TF, Richey
JE, Sedell JR, Turekian KK (eds) Flux of organic carbon by rivers to the oceans. US Dept of Energy,
Washington DC, pp 360-384
Mariotti A, Gadel F, Giresse P, Kinga-Mouzeo (1991)
Carbon isotope composition and geochemistry of
particulate OM in the Congo River (Central Africa):
application to the study of Quaternary sediments off
the mouth of the river. Chern Geo186: 345-357
Marret F (1994) Evolution paleoclimatique et
paleohydrologique de I' Atlantique est-equatorial et
du proche continent au Quaternaire terminal. Contribution palynologique (kystes de dinoflagelles,
pollen et spores). Thesis Univ Bordeaux I, pp 1-255
McCave IN (1986) Local and global aspects of the bottom nepheloid layers in the world ocean. Neth ] Sea
Res 20 (2/3): 167-181
Michaelis W, Ittekkot V, Degen ET (1986) River inputs
into oceans. In: Lassere P, Martin 1M (eds) Biochemical processes at the Land-sea Boundary. Elsevier,
Amsterdam, pp 37-52
Mix AC (1989) Influence of productivity variations on
long-term atmospheric CO,. Nature 337: 541-544
Miiller PJ (1977) CIN ratios in Pacific deep-sea
sediments: Effect on inorganic ammonium and organic nitrogen compounds sorbed by clays.
Geochim CosmochimActa41: 765-776
Muller PJ, Suess E (1979) Productivity, sedimentation
rate, and sedimentary OM in the oceans - 1. Organic
carbon preservation. Deep-Sea Res 26 (A):
1347-1362
Miiller PJ, Erlenkeuser H, von 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: Its sedimentary record, Part B.
Plenum Press, New York, pp 365-393
Muller PJ, Schneider RR, Ruhland G (1994) Late Quaternary pCO 2 variations in the Angola Current: evidence
from organic carbon 8 13 C alkenone temperatures. In
Zahn R, Pedersen TF, Kaminski MA, Labeyrie L (eds)
Carbon Cycling in the Glacial Ocean: Constraints on
the Ocean's Role in Global Change. NATO ASI
Series, Vol 17, Springer, Berlin Heidelberg New York,
pp 343-366
Peters KE (1986) Guidelines for evaluating petroleum
source rock using programmed pyrolysis. AAPG 70
(3):318-329
Pokras EM, Mix AC (1985) Eolian evidence for spatial
variability of Late Quaternary climates in tropical
Africa. Quat Res 24: 137-149
Powell TG, Creaney S, Snowdon LR(1982) Limitations
of use of Organic Petrographic Techniques
for identification of Petroleum Source Rocks. AAPG
66 (4): 430-435
Poynter JG, Eglinton G (1991) A biomarker conceptstrengths and weaknesses. Fresenius J Anal Chern
339: 725-731