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  • 1
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    PANGAEA
    In:  Supplement to: Feng, Dong; Lin, Zhijia; Bian, Y; Chen, Duofu; Peckmann, Jörn; Bohrmann, Gerhard; Roberts, Harry H (2013): Rare earth elements of seep carbonates: Indication for redox variations and microbiological processes at modern seep sites. Journal of Asian Earth Sciences, 65, 27-33, https://doi.org/10.1016/j.jseaes.2012.09.002
    Publication Date: 2024-01-18
    Description: At marine seeps, methane is microbially oxidized resulting in the precipitation of carbonates close to the seafloor. Methane oxidation leads to sulfate depletion in sediment pore water, which induces a change in redox conditions. Rare earth element (REE) patterns of authigenic carbonate phases collected from modern seeps of the Gulf of Mexico, the Black Sea, and the Congo Fan were analyzed. Different carbonate minerals including aragonite and calcite with different crystal habits have been selected for analysis. Total REE content (SumREE) of seep carbonates varies widely, from 0.1 ppm to 42.5 ppm, but a common trend is that the SumREE in microcrystalline phases is higher than that of the associated later phases including micospar, sparite and blocky cement, suggesting that SumREE may be a function of diagenesis. The shale-normalized REE patterns of the seep carbonates often show different Ce anomalies even in samples from a specific site, suggesting that the formation conditions of seep carbonates are variable and complex. Overall, our results show that apart from anoxic, oxic conditions are at least temporarily common in seep environments.
    Keywords: Center for Marine Environmental Sciences; MARUM
    Type: Dataset
    Format: application/zip, 2 datasets
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  • 2
    Publication Date: 2024-02-02
    Keywords: 1997-JSL-I-2904; 1998-JSL-I-4061; 1998-JSL-I-4063; AC-1990; Alaminos Canyon; ALVIN; Aragonite; BEAM; Beam trawl; Bush Hill; Calcite; Center for Marine Environmental Sciences; Comment; Congo Fan; Dolomite; Event label; GeoB8212-2; GeoB8215-2; Gulf of Mexico; Illite; JSL; Kaolinite; Location; M56/2; MARUM; Meteor (1986); Muscovite; PO201F,G; POS201/6,7; POS201/6,7_UBS1; Poseidon; PV_RBS38; Quartz; Reference/source; Romanian shelf; S-4_2002; Sample ID; Submersible Alvin; Submersible Johnson Sea Link; Television-Grab; TVG; Ukrainian shelf; δ13C, carbonate
    Type: Dataset
    Format: text/tab-separated-values, 142 data points
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  • 3
    Publication Date: 2024-02-02
    Keywords: 1997-JSL-I-2904; 1998-JSL-I-4061; 1998-JSL-I-4063; AC-1990; Alaminos Canyon; ALVIN; BEAM; Beam trawl; Bush Hill; Center for Marine Environmental Sciences; Cerium; Cerium anomaly; Congo Fan; Dysprosium; Erbium; Europium; Europium anomaly; Event label; Gadolinium; GeoB8212-2; GeoB8215-2; Gulf of Mexico; Holmium; Inductively coupled plasma - mass spectrometry (ICP-MS); JSL; Lanthanum; Lutetium; M56/2; MARUM; Meteor (1986); Neodymium; PO201F,G; POS201/6,7; POS201/6,7_UBS1; Poseidon; Praseodymium; PV_RBS38; Rare-earth elements; Romanian shelf; S-4_2002; Samarium; Sample ID; Submersible Alvin; Submersible Johnson Sea Link; Television-Grab; Terbium; Thulium; TVG; Type; Ukrainian shelf; Ytterbium
    Type: Dataset
    Format: text/tab-separated-values, 570 data points
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  • 4
    Publication Date: 2022-05-26
    Description: Author Posting. © The Authors, 2004. This is the author's version of the work. It is posted here by permission of Elsevier B. V. for personal use, not for redistribution. The definitive version was published in Marine and Petroleum Geology 22 (2005): 479-497, doi:10.1016/j.marpetgeo.2004.08.008.
    Description: Large volumes of gas have vented through a north-south transect of the offshore northern Gulf of Mexico. An overview of surface and subsurface manifestations of this gas venting is presented. This gas movement has caused extensive alteration of reservoired oils to the north of the transect which are estimated to have equilibrated with, or been gas washed by, as much as 30 volumes of gas for every volume of oil. This gas washing entrains and carries upward the most volatile oil components depositing them in either shallower reservoirs or venting them to the overlying sediments and the water column. A significant amount of this gas bypasses the reservoirs and vents upward into the overlying sediments and waters. In spite of the significant amounts of the gas involved, the venting at the seafloor appears to occur primarily through highly localized faults and fractures. This gas discharge is spatially and temporally heterogeneous, making it difficult to estimate the actual hydrocarbon fluxes involved. This upward gas movement leaves characteristic signatures at the sediment water interface including carbonate pavements in older seep areas, and chemosynthetic biological communities, methane hydrates, and gas seeps in more recent long-term seep areas. In some cases where gas venting is very recent, massive disruption of surface and subsurface sediments is observed to be occasionally accompanied by mud volcanoes. Venting can be vigorous enough to produce methane gas bubbles, which appear to be injected rapidly into surface waters and which may constitute a significant source of methane, a greenhouse gas, to the atmosphere. In the northern Gulf of Mexico, gas venting is sometimes accompanied by natural oil slicks at the sea surface, which can be tracked for many miles in non-productive areas. These gas-venting signatures are not unique to the Gulf of Mexico; similar seep features are observed in sediments worldwide. The widespread occurrence of these seep features, which may or may not be related to subsurface oil and gas deposits, may explain why use of surface seeps has often proved to be so controversial in oil exploration. Indeed, most seeps are probably not linked with economic subsurface petroleum reservoirs. The relationships between surface seep features and productive subsurface reservoirs along a N-S transect of the Northern Gulf of Mexico are presented as an example of how all surface and subsurface geochemical, geological, geophysical data might be used together to better constrain interpretations regarding the nature and dynamics of subsurface oil and gas deposits and their plumbing in frontier areas.
    Description: Support for this work was provided by the Department of Energy, Grant No. DE-FG02-86EF13466 and U.S. Department of Energy Grant No. DE-FC26-00NT40920 through the University of Mississippi to Jean Whelan and; Gas Research Institute Contract GRI50972603787 to Larry Cathles, Cornell University with a subcontract to Jean Whelan.
    Keywords: Methane ; Hydrate ; Seep ; Migration ; Petroleum ; Gas ; Biodegradation
    Repository Name: Woods Hole Open Access Server
    Type: Preprint
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  • 5
    Electronic Resource
    Electronic Resource
    Springer
    Geo-marine letters 6 (1986), S. 57-61 
    ISSN: 1432-1157
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Type of Medium: Electronic Resource
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  • 6
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    New York : Periodicals Archive Online (PAO)
    Journal of marketing. 22:1/4 (1957:July/Oct.-1958:Jan./Apr.) 21-32 
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  • 7
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    New York : Periodicals Archive Online (PAO)
    Journal of marketing. 27:1 (1963:Jan.) 1 
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  • 8
    Electronic Resource
    Electronic Resource
    Springer
    Geo-marine letters 10 (1990), S. 177-181 
    ISSN: 1432-1157
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Notes: Abstract The hummocky continental slope in the northwestern Gulf of Mexico is the result of active salt tectonism and accompanying faulting. Fluid and gassy hydrocarbons rise through the sediment column and along faults causing the formation of gas hydrates, gassy sediments, mud volcanoes and mounds, chemosynthetic communities and authigenic carbonates, reefs, and hardgrounds. Salt activity coupled with processes associated with relative sea level fluctuations create a feedback relationship resulting in the above-mentioned phenomena as well as others such as seafloor erosion at great water depths.
    Type of Medium: Electronic Resource
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  • 9
    ISSN: 1432-1157
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Notes: Abstract Cyclic sequences occur worldwide in nearly every stratigraphic sequence; they are particularly well developed in marine deposits associated with large river systems. Superimposed on those cycles attributed to shifting sites of deposition are those related to high-frequency sea level changes. The large data base for this study (including 471 deep foundation borings, thousands of line kilometers of high-resolution seismic, and sedimentological and dating analyses) represents the most complete information on high-resolution chronostratigraphy and lithostratigraphy that is available on any modern continental shelf/upper slope. These data are used to document sedimentological characteristics and spatial depositional patterns during three complete sea level cycles over the entire continental shelf/upper slope of offshore Louisiana. Sedimentation during periods of high sea level is characterized by: 1) thin, slowly accumulated depositional sequences, referred to as condensed sections, 2) calcareous-rich deposits, including hemipelagic sediments and shell hashes, and 3) wide lateral continuity. Sedimentation during periods of low sea level is characterized by; 1) variable-thickness, rapidly accumulated sequences referred to as expanded sections, 2) coarse-grained elastic deposits, including abundant sands and gravels, and 3) well-defined depositional trends. Even though the data set covers only a short period of geologic time (240 000 yrs), these high frequency events are responsible for the deposition of excellent reservoir-quality facies in well-defined and predictable trends.
    Type of Medium: Electronic Resource
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  • 10
    Electronic Resource
    Electronic Resource
    Springer
    Geo-marine letters 5 (1985), S. 185-191 
    ISSN: 1432-1157
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Notes: Abstract Mass movement processes are the most important transport agents on the modern delta front. Changes in relative abundances of kaolinite, illite, and smectite proved to be valuable descriptors for distinguishing mudflow deposits (derived from the shallow delta front) from outer shelf/upper slope sediments. Fine-grained sediments, rapidly deposited from the turbid distributary plumes in the upper delta front, are typically high in smectite relative to illite and kaolinite. Distal shelf and upper slope sediments display an increased abundance of kaolinite and illite at the expense of smectite. Shifts in abundances of clay minerals define the bases and internal stratigraphy of complex mudflows.
    Type of Medium: Electronic Resource
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