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Authigenic Carbonate Formation at Hydrocarbon Seeps in Continental Margin Sediments: a Comparative Study

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Authigenic Carbonate Formation at Hydrocarbon Seeps in Continental Margin Sediments: a Comparative Study ARTICLE IN PRESS Deep-Sea Research II 54 (2007) 1268–1291 www.elsevier.com/locate/dsr2 Authigenic carbonate formation at hydrocarbon seeps in continental margin sediments: A comparative study Thomas H. Naehra,Ã, Peter Eichhublb, Victoria J. Orphanc, Martin Hovlandd, Charles K. Paulle, William Ussler IIIe, Thomas D. Lorensonf, H. Gary Greeneg aDepartment of Physical and Environmental Sciences, Texas A&M University-Corpus Christi, 6300 Ocean Drive, Corpus Christi, TX 78412, USA bUniversity of Texas at Austin, Bureau of Economic Geology, University Station, Box X, Austin, TX 78713-8924, USA cDivision of Geological and Planetary Sciences, California Institute of Technology, Mail Code 100-23, Pasadena, CA 91125, USA dStatoil, 4001 Stavanger, Norway eMonterey Bay Aquarium Research Institute, 7700 Sandholdt Road, Moss Landing, CA 95039, USA fUSGS, 345 Middlefield Road, M.S. 999, Menlo Park, CA 94025, USA gMoss Landing Marine Laboratories, 8272 Moss Landing Road, Moss Landing, CA 95039, USA Accepted 16 April 2007 Available online 20 July 2007 Abstract Authigenic carbonates from five continental margin locations, the Eel River Basin, Monterey Bay, Santa Barbara Basin, the Sea of Okhotsk, and the North Sea, exhibit a wide range of mineralogical and stable isotopic compositions. These precipitates include aragonite, low- and high-Mg calcite, and dolomite. The carbon isotopic composition of carbonates varies widely, ranging from À60% to +26%, indicating complex carbon sources that include 13C-depleted microbial and thermogenic methane and residual, 13C-enriched, bicarbonate. A similarly large variability of d18O values (À5.5% to +8.9%) demonstrates the geochemical complexity of these sites, with some samples pointing toward an 18O-enriched oxygen source possibly related to advection of 18O-enriched formation water or to the decomposition of gas hydrate. Samples depleted in 18O are consistent with formation deeper in the sediment or mixing of pore fluids with meteoric water during carbonate precipitation. A wide range of isotopic and mineralogical variation in authigenic carbonate composition within individual study areas but common trends across multiple geographic areas suggest that these parameters alone are not indicative for certain tectonic or geochemical settings. Rather, the observed variations probably reflect local controls on the flux of carbon and other reduced ions, such as faults, fluid conduits, the presence or absence of gas hydrate in the sediment, and the temporal evolution of the local carbon reservoir. Areas with seafloor carbonates that indicate formation at greater depth below the sediment–water interface must have undergone uplift and erosion in the past or are still being uplifted. Consequently, the occurrence of carbonate slabs on the seafloor in areas of active hydrocarbon seepage is commonly an indicator of exhumation following carbonate precipitation in the shallow subsurface. Therefore, careful petrographic and geochemical analyses are critical components necessary for the correct interpretation of processes related to hydrocarbon seepage in continental margin environments and elsewhere. r 2007 Elsevier Ltd. All rights reserved. Keyword: Seeps; Methane; Authigenic; Carbonate; Continental margins ÃCorresponding author. Tel.: +1 361 825 2470; fax: +1 361 825 2025. E-mail address: [email protected] (T.H. Naehr). 0967-0645/$ - see front matter r 2007 Elsevier Ltd. All rights reserved. doi:10.1016/j.dsr2.2007.04.010 ARTICLE IN PRESS T.H. Naehr et al. / Deep-Sea Research II 54 (2007) 1268–1291 1269 1. Introduction records of an otherwise ephemeral phenomenon (Naehr et al., 2000b; Martin et al., 2004; Hein et al., Hydrocarbon seeps are ubiquitous features of 2006). many active and passive continental margins. They The aim of this paper is to develop a more represent discrete sites where fluids in chemical comprehensive understanding of the complex geo- disequilibrium with seawater and typically rich in chemical, physical, and biological interactions at methane and other hydrocarbons travel through the seep sites by comparing the mineralogy, petrology, sub-seafloor environment and emanate at the and isotope geochemistry of authigenic carbonates sediment–water interface. Thiotrophic or methano- from five different hydrocarbon seep locations. In trophic biological communities and precipitates of doing so, we hope to address the question whether authigenic minerals mark such areas of fluid the biogeochemistry of hydrocarbon seeps varies discharge, and are the result of both biogeochemical systematically between different locations or if the turnover and the interaction between fluids and observed geochemical trends reflect local controls ambient bottom water at hydrocarbon seep sites on the flux of carbon from the subsurface to the (Hovland et al., 1985; Suess et al., 1985; Paull et al., seafloor. To this end, we present a comparative 1995b; Naehr et al., 2000a, b). Bicarbonate and study that illustrates the diverse processes asso- sulfate activities at hydrocarbon seeps are predomi- ciated with the flux of fluids and gases to the nately controlled by the flux of gases, mostly seafloor and the precipitation of authigenic minerals methane, to the seafloor, and by rates of biologically at hydrocarbon seeps. We shall discuss and contrast induced reactions. Furthermore, chemosymbiotic the formation and early diagenesis of authigenic benthic fauna is supported by the microbially driven mineral deposits in a variety of geologic and anaerobic oxidation of methane (AOM) (Elvert geochemical environments including Eel River and Suess, 1999; Hinrichs et al., 1999; Thiel et al., Basin, Monterey Bay, Santa Barbara Basin, the 1999), which increases pore water alkalinity by the Sea of Okhotsk, and the North Sea (Fig. 1). À production of bicarbonate [HCO3 ]: 2À À À 2. Geologic setting CH4 þ SO4 3 HCO3 þ HS þ H2O (1) thus favoring precipitation of authigenic carbonate The Eel River Basin is a forearc basin located at minerals in the shallow subsurface by the reaction the southern end of the Cascadia accretionary prism that is associated with the Gorda-North American 2HCO À þ Ca2þ 3 CaCO þ CO þ H O (2) 3 3 2 2 plate margin (Fig. 1A). The dominant structural (Baker and Burns, 1985). features that define the Eel River Basin include a Authigenic carbonates associated with hydrocar- series of NNW–SSE trending synclines, anticlines, bon seepage are known to show a wide range of and faults that form a 250-km-long and 70-km-wide mineralogical as well as carbon and oxygen isotopic sedimentary basin (Hoskins and Griffiths, 1971; compositions. The occurrence of high-Mg calcite Carver, 1987; Clarke, 1992). The Eel River Basin is (HMC) and low-Mg calcite (LMC), aragonite, underlain by Jurassic to Eocene rocks of the dolomite, and other less common mineral species, Franciscan Complex and contains a 4000-m thick such as glendonite or ikaite, has been documented sequence of Neogene age sediments that primarily by various authors (e.g., Claypool and Kaplan, consist of marine mudstones, siltstones, and fine 1974; Greinert et al., 2001; Greinert and Derkachev, sandstones (Carver, 1987; Clarke, 1992). Because 2004; Orphan et al., 2004). The carbon isotopic the organic carbon content and thickness of these composition of these carbonates can vary by as sediments are adequate to generate petroleum, the much as 85%, indicating an almost equally wide basin has been a recurring target for hydrocarbon range of geochemical processes involved in carbo- exploration. Gas production still occurs from the nate precipitation. Oxygen isotopes also may show Tomkins Hill Gas Field and small amounts of oil considerable variation, documenting the effects of were produced from onshore basins (McCulloch temperature and/or fluid composition on carbonate et al., 1977; Horan and Hopps, 1987). Modern formation. Regardless of their mineralogical and sedimentation in the Eel River Basin is controlled isotopic composition, however, seep-related authi- by sediment input from the Eel and Mad rivers, genic minerals provide an important geological with the vast majority of sediment being trans- archive, as they represent one of the few permanent ported during short-duration storm events (Orange, ARTICLE IN PRESS 1270 T.H. Naehr et al. / Deep-Sea Research II 54 (2007) 1268–1291 Fig. 1. Location maps of the study areas. (A) Location of Eel River Basin, Monterey Bay, and Santa Barbara Basin along the western continental margin of the North American plate. (B) Location of the Tommeliten study area in the central North Sea. (C) Location map of samples from the western flank of the Derugin Basin in the Sea of Okhotsk. 1999). Secondary transport of sediment by mass during floods of the Eel and other rivers (Leithold wasting and sediment redistribution also plays an et al., 1999). important role in this tectonically active environ- Monterey Bay and its deep canyon rest on the ment. Rapid tectonic uplift and high erosion rates active transform boundary that separates the Pacific are responsible for high sediment-accumulation plate from the North American plate (Fig. 1A). In rates in the Eel River Basin (Alexander et al., central California, this boundary is more than 1999). Furthermore, the basin receives large quan- 100 km wide and includes the San Andreas fault to tities of young, relatively fresh organic matter the east, as well as offshore segments of the Palo ARTICLE IN PRESS T.H. Naehr et al. / Deep-Sea Research II 54 (2007) 1268–1291 1271 Colorado–San Gregorio fault and Monterey Bay ability of the siliceous
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