282
Emerson S, Jahnke R, Bender M, Froelich P, Klinkhammer G, Bowser C, Setlock G (1980) Early
diagenesis in sediments from the eastern equatorial Pacific. I. Pore water nutrient and carbonate
profiles. Earth Planet Sci Lett 49:57–80
Emerson SE, Fischer K, Reimers C, Heggie D (1985) Organic carbon dynamics and preservation
in deep-sea sediments. Deep-Sea Res 32:1–22
EPA (1994) Microwave assisted acid digestion of sediments, sludges, soils, and oils, Method 3051.
U.S. Government Printing Office, Washington, DC
Froelich PN, Klinkhammer GP, Bender ML, Leudtke N, Heath GR, Cullen D, Dauphin P,
Hammond D, Hartman B (1979) Early oxidation of organic matter in pelagic sediments of
the eastern Equatorial Atlantic: suboxic diagenesis. Geochim Cosmochim Acta 43:1075–1090
Finney BP, Lyle MW, Heath GR (1988) Sedimentation at MANOP Site H (eastern equatorial
Pacific) over the past 400,000 years: climatically induced redox variations and their effects on
transition metal cycling. Paleoceanography 3(2):169–189
Gobeil C, Macdonald RW, Sundby B (1997) Diagenetic separation of cadmium and manganese in
suboxic continental margin sediments. Geochim Cosmochim Acta 61(21):4647–4654. https://
doi.org/10.1016/S0016-7037(97)00255-X
Gobeil C, Sundby B, Macdonald RW, Smith JN (2001) Recent change in organic carbon flux to
Arctic Ocean deep basins: evidence from acid volatile sulfide, manganese and rhenium discord
in sediments. Geophys Res Lett 28(9):1743–1746. https://doi.org/10.1029/2000GL012491
Hastings DW, Schwing PT, Brooks GR, Larson RA, Morford JL, Roeder T, Quinn KA, Bartlett T,
Romero IC, Hollander DJ (2016) Changes in sediment redox conditions following the BP DWH
blowout event. Deep-Sea Res II Top Stud Oceanogr 129:167–178. https://doi.org/10.1016/j.
dsr2.2014.12.009
Honjo S, Manganini SJ, Cole JJ (1982) Sedimentation of biogenic matter in the deep ocean. DeepSea Res 29(5):609–625. https://doi.org/10.1016/0198-0149(82)90079-6
Joye SB, MacDonald IR, Leifer I, Asper V (2011) Magnitude and oxidation potential of hydrocarbon gases released from the BP oil well blowout. Nat Geosci 4(3):160–164. http://www.nature.
com/ngeo/journal/v4/n3/abs/ngeo1067.html#supplementary-information
Koide M, Hodge VF, Yang JS, Stallard M, Goldberg EG, Calhoun J, Bertine KK (1986) Some
comparative marine chemistries of rhenium, gold, silver and molybdenum. Appl Geochem
1(6):705–714. https://doi.org/10.1016/0883-2927(86)90092-2
Kuzyk ZZA, Macdonald RW, Stern GA, Gobeil C (2011) Inferences about the modern organic carbon cycle from diagenesis of redox-sensitive elements in Hudson Bay. J Mar Syst 88(3):451–
462. https://doi.org/10.1016/j.jmarsys.2010.11.001
Larson RA, Brooks GR, Schwing PT, Diercks AR, Holmes CW, Chanton JP, Diaz-Asencio M,
Hollander DJ (2020) Characterization of the sedimentation associated with the Deepwater
Horizon blowout: depositional pulse, initial response, and stabilization (Chap. 14). In:
Murawski SA, Ainsworth C, Gilbert S, Hollander D, Paris CB, Schlüter M, Wetzel D (eds)
Scenarios and responses to future deep oil spills – fighting the next war. Springer, Cham
Madison AS, Tebo BM, Mucci A, Sundby B, Luther GW (2013) Abundant Porewater Mn(III) is
a major component of the sedimentary redox system. Science 341(6148):875–878. https://doi.
org/10.1126/science.1241396
Magen C, Mucci A, Sundby B (2011) Reduction rates of sedimentary Mn and Fe oxides: an incubation experiment with Arctic Ocean sediments. Aquat Geochem 17(4–5):629–643. https://doi.
org/10.1007/s10498-010-9117-9
Mayor DJ, Thornton B, Hay S, Zuur AF, Nicol GW, McWilliam JM, Witte UF (2012) Resource
quality affects carbon cycling in deep-sea sediments. ISME J 6(9):1740–1748. https://doi.
org/10.1038/ismej.2012.14
Morford JL, Emerson SE (1999) The geochemistry of redox sensitive trace metals in sediments. Geochim Cosmochim Acta 63(11–12):1735–1750. https://doi.org/10.1016/
S0016-7037(99)00126-X
D. W. Hastings et al.
Emerson S, Jahnke R, Bender M, Froelich P, Klinkhammer G, Bowser C, Setlock G (1980) Early
diagenesis in sediments from the eastern equatorial Pacific. I. Pore water nutrient and carbonate
profiles. Earth Planet Sci Lett 49:57–80
Emerson SE, Fischer K, Reimers C, Heggie D (1985) Organic carbon dynamics and preservation
in deep-sea sediments. Deep-Sea Res 32:1–22
EPA (1994) Microwave assisted acid digestion of sediments, sludges, soils, and oils, Method 3051.
U.S. Government Printing Office, Washington, DC
Froelich PN, Klinkhammer GP, Bender ML, Leudtke N, Heath GR, Cullen D, Dauphin P,
Hammond D, Hartman B (1979) Early oxidation of organic matter in pelagic sediments of
the eastern Equatorial Atlantic: suboxic diagenesis. Geochim Cosmochim Acta 43:1075–1090
Finney BP, Lyle MW, Heath GR (1988) Sedimentation at MANOP Site H (eastern equatorial
Pacific) over the past 400,000 years: climatically induced redox variations and their effects on
transition metal cycling. Paleoceanography 3(2):169–189
Gobeil C, Macdonald RW, Sundby B (1997) Diagenetic separation of cadmium and manganese in
suboxic continental margin sediments. Geochim Cosmochim Acta 61(21):4647–4654. https://
doi.org/10.1016/S0016-7037(97)00255-X
Gobeil C, Sundby B, Macdonald RW, Smith JN (2001) Recent change in organic carbon flux to
Arctic Ocean deep basins: evidence from acid volatile sulfide, manganese and rhenium discord
in sediments. Geophys Res Lett 28(9):1743–1746. https://doi.org/10.1029/2000GL012491
Hastings DW, Schwing PT, Brooks GR, Larson RA, Morford JL, Roeder T, Quinn KA, Bartlett T,
Romero IC, Hollander DJ (2016) Changes in sediment redox conditions following the BP DWH
blowout event. Deep-Sea Res II Top Stud Oceanogr 129:167–178. https://doi.org/10.1016/j.
dsr2.2014.12.009
Honjo S, Manganini SJ, Cole JJ (1982) Sedimentation of biogenic matter in the deep ocean. DeepSea Res 29(5):609–625. https://doi.org/10.1016/0198-0149(82)90079-6
Joye SB, MacDonald IR, Leifer I, Asper V (2011) Magnitude and oxidation potential of hydrocarbon gases released from the BP oil well blowout. Nat Geosci 4(3):160–164. http://www.nature.
com/ngeo/journal/v4/n3/abs/ngeo1067.html#supplementary-information
Koide M, Hodge VF, Yang JS, Stallard M, Goldberg EG, Calhoun J, Bertine KK (1986) Some
comparative marine chemistries of rhenium, gold, silver and molybdenum. Appl Geochem
1(6):705–714. https://doi.org/10.1016/0883-2927(86)90092-2
Kuzyk ZZA, Macdonald RW, Stern GA, Gobeil C (2011) Inferences about the modern organic carbon cycle from diagenesis of redox-sensitive elements in Hudson Bay. J Mar Syst 88(3):451–
462. https://doi.org/10.1016/j.jmarsys.2010.11.001
Larson RA, Brooks GR, Schwing PT, Diercks AR, Holmes CW, Chanton JP, Diaz-Asencio M,
Hollander DJ (2020) Characterization of the sedimentation associated with the Deepwater
Horizon blowout: depositional pulse, initial response, and stabilization (Chap. 14). In:
Murawski SA, Ainsworth C, Gilbert S, Hollander D, Paris CB, Schlüter M, Wetzel D (eds)
Scenarios and responses to future deep oil spills – fighting the next war. Springer, Cham
Madison AS, Tebo BM, Mucci A, Sundby B, Luther GW (2013) Abundant Porewater Mn(III) is
a major component of the sedimentary redox system. Science 341(6148):875–878. https://doi.
org/10.1126/science.1241396
Magen C, Mucci A, Sundby B (2011) Reduction rates of sedimentary Mn and Fe oxides: an incubation experiment with Arctic Ocean sediments. Aquat Geochem 17(4–5):629–643. https://doi.
org/10.1007/s10498-010-9117-9
Mayor DJ, Thornton B, Hay S, Zuur AF, Nicol GW, McWilliam JM, Witte UF (2012) Resource
quality affects carbon cycling in deep-sea sediments. ISME J 6(9):1740–1748. https://doi.
org/10.1038/ismej.2012.14
Morford JL, Emerson SE (1999) The geochemistry of redox sensitive trace metals in sediments. Geochim Cosmochim Acta 63(11–12):1735–1750. https://doi.org/10.1016/
S0016-7037(99)00126-X
D. W. Hastings et al.