Authigenic carbonate burial in the Late Devonian-Early Mississippian Bakken Formation (Williston Basin, USA)

被引:9
作者
Barnes, Ben Davis [1 ,2 ]
Husson, Jon M. [1 ,3 ]
Peters, Shanan E. [1 ]
机构
[1] Univ Wisconsin, Dept Geosci, 1215 W Dayton St, Madison, WI 53706 USA
[2] Penn State Univ, Dept Geosci, Deike Bldg, University Pk, PA 16802 USA
[3] Univ Victoria, Sch Earth & Ocean Sci, 2800 Finnerty Rd, Victoria, BC V8W 2Y2, Canada
关键词
Authigenic carbonate; Bakken Formation; black shale; Devonian; Hangenberg Event; UPPER SHALE MEMBER; DARK-SEDIMENTARY PROCESSES; CARBONIFEROUS BOUNDARY; ORGANIC-MATTER; GLOBAL CARBON; NORTH-DAKOTA; GEOCHEMICAL EVIDENCE; MICROBIAL CARBONATE; FACIES GRADIENTS; HANGENBERG EVENT;
D O I
10.1111/sed.12695
中图分类号
P5 [地质学];
学科分类号
0709 ; 081803 ;
摘要
Late Devonian (Famennian) marine successions globally are typified by organic-rich black shales deposited in anoxic and euxinic waters and the cessation of shelf carbonate sedimentation. This global 'carbonate crisis', known as the Hangenberg Event, coincides with a major extinction of reef-building metazoans and perturbations to the global carbon cycle, evidenced by positive carbon-isotope excursions of up to 4 parts per thousand. It has been suggested that authigenic carbonate, formed as cements in sedimentary pore spaces during early burial diagenesis, is a significant mass fraction of the total global carbon burial flux, particularly during periods of low oxygen concentration. Because some authigenic carbonate could have originated from remineralization of organic carbon in sediments, it is possible for this reservoir to be isotopically depleted and thereby drive changes in the carbon isotopic composition of seawater. This study presents bulk isotopic and elemental analyses from fine-grained siliciclastics of the Late Devonian-Early Mississippian Bakken Formation (Williston Basin, USA) to assess the volume and isotopic composition of carbonates in these sediments. Carbonate in the Bakken black shales occurs primarily as microscopic disseminated dolomite rhombs and calcite cements that, together, comprise a significant mass-fraction (ca 9%). The elemental composition of the shales is indicative of a dynamic anoxic to sulphidic palaeoenvironment, likely supported by a fluctuating chemocline. Despite forming in an environment favourable to remineralization of organic matter and the precipitation of isotopically depleted authigenic carbonates, the majority of carbon isotope measurements of disseminated carbonate fall between -3 parts per thousand and +3 parts per thousand, with systematically more depleted carbonates in the deeper-water portions of the basin. Thus, although there is evidence for a significant total mass-fraction of carbonate with contribution from remineralized organic matter, Bakken authigenic carbonates suggest that Famennian black shales are unlikely to be sufficiently C-13-depleted relative to water column dissolved inorganic carbon to serve as a major lever on seawater isotopic composition.
引用
收藏
页码:2065 / 2094
页数:30
相关论文
共 126 条
[21]   Joining forces: Combined biological and geochemical proxies reveal a complex but refined high-resolution palaeo-oxygen history in Devonian epeiric seas [J].
Boyer, Diana L. ;
Owens, Jeremy D. ;
Lyons, Timothy W. ;
Droser, Mary L. .
PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY, 2011, 306 (3-4) :134-146
[22]   Reevaluating the carbon sink due to sedimentary carbonate formation in modern marine sediments [J].
Bradbury, Harold J. ;
Turchyn, Alexandra, V .
EARTH AND PLANETARY SCIENCE LETTERS, 2019, 519 :40-49
[23]   Biochemostratigraphy of the Devonian-Carboniferous boundary Global Stratotype Section and Point, Griotte Formation, La Serre, Montagne Noire, France [J].
Brand, U ;
Legrand-Blain, M ;
Streel, M .
PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY, 2004, 205 (3-4) :337-357
[24]  
BRAND U, 1980, J SEDIMENT PETROL, V50, P1219
[25]  
BRENNAN SW, 2016, THESIS
[26]   OXYGEN ISOTOPE MICROANALYSIS BY SECONDARY ION MASS SPECTROMETRY SUGGESTS CONTINUOUS 300-MILLION-YEAR HISTORY OF CALCITE CEMENTATION AND DOLOMITIZATION IN THE DEVONIAN BAKKEN FORMATION [J].
Brodie, Mark W. ;
Aplin, Andrew C. ;
Hart, Bruce ;
Orland, Ian J. ;
Valley, John W. ;
Boyce, Adrian J. .
JOURNAL OF SEDIMENTARY RESEARCH, 2018, 88 (01) :91-104
[27]   A BOUNDARY CONDITION ON EVOLUTION OF ATMOSPHERIC OXYGEN [J].
BROECKER, WS .
JOURNAL OF GEOPHYSICAL RESEARCH, 1970, 75 (18) :3553-+
[28]   Carbon isotope stratigraphy of the Devonian of Central and Southern Europe [J].
Buggisch, Werner ;
Joachimski, Michael M. .
PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY, 2006, 240 (1-2) :68-88
[29]  
Calvert SE, 2007, DEV MARINE GEOL, V1, P567, DOI 10.1016/S1572-5480(07)01019-6
[30]   Palaeoceanographic controls on geochemical characteristics of organic-rich Exshaw mudrocks: role of enhanced primary production [J].
Caplan, ML ;
Bustin, RM .
ORGANIC GEOCHEMISTRY, 1999, 30 (2-3) :161-188