Cited by 113Paleontology and Stratigraphy of FossilsPaleontology and Evolutionary BiologyGeological formations and processes

The DOI matches its Crossref record; 5 of the 5 references it cites were found in a registry or an index.

A new hypothesis for organic preservation of Burgess Shale taxa in the middle Cambrian Wheeler Formation, House Range, Utah

Gaines, Robert R., Kennedy, Martin J., Droser, Mary L.·2005·Palaeogeography, Palaeoclimatology, Palaeoecology

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Crossref · 10.1016/j.palaeo.2004.07.034

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5 of 5 references verified0 citation errors · 0 not checkable

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  • The ubiquitous presence of bed-capping cements in BST bearing beds of all deposits analyzed suggests that they may have acted as a barrier, reducing porosity at the bed tops and restricting diffusion of oxidants into the sediments.

    “The ubiquitous presence of bed-capping cements in BST bearing beds of all deposits analyzed suggests that they may have acted as a barrier, reducing porosity at the bed tops and restricting diffusion of oxidants into the sediments (9).”

    From Mechanism for Burgess Shale-type preservation (2012) · cites this paper as [9]

  • BST deposits accumulated under anoxic or dysoxic bottom waters.

    “It is broadly accepted that BST deposits accumulated under anoxic or dysoxic bottom waters (4, 9, 12, 28)”

    From Mechanism for Burgess Shale-type preservation (2012) · cites this paper as [9]

  • With oxygen-deficient conditions in the overlying bottom waters and burial in anoxic sediments, microbial degradation of soft-tissues with O2 was insignificant.

    “Hence, with oxygen-deficient conditions in the overlying bottom waters and burial in anoxic sediments (4, 9, 12, 28), microbial degradation of soft-tissues with O2 was insignificant.”

    From Mechanism for Burgess Shale-type preservation (2012) · cites this paper as [9]

  • Several hypotheses have been proposed to account for BST preservation, but none have been previously tested.

    “Although several hypotheses have been proposed to account for BST preservation (4, 9, 13), none have been previously tested”

    From Mechanism for Burgess Shale-type preservation (2012) · cites this paper as [9]

  • Claystone beds are cemented by pervasive micron-sized authigenic calcium carbonates, which are concentrated at bed tops and penetrate downward.

    “Claystone beds are cemented by pervasive micron-sized authigenic calcium carbonates (9, 17), which are concentrated at bed tops and penetrate downward (Fig. 2 B–E and SI Appendix, Figs. S2–S4).”

    From Mechanism for Burgess Shale-type preservation (2012) · cites this paper as [9]

Citations

Cites

Flagged first, then by citations

Research works printed but not linked: 32

  1. Allison, 1988, The role of anoxia in the decay and mineralization of proteinaceous macro-fossils, Paleobiology, 14, 139, 10.1017/S009483730001188X · DOI
  2. Allison, 1995, In situ benthos and paleo-oxygenation in the middle Cambrian Burgess Shale, British Columbia, Canada, Geology, 23, 1079, 10.1130/0091-7613(1995)023<1079:ISBAPO>2.3.CO;2 · DOI · Paper page
  3. Allison, 1993, Exceptional fossil record: distribution of soft-tissue preservation through the Phanerozoic, Geology, 21, 527, 10.1130/0091-7613(1993)021<0527:EFRDOS>2.3.CO;2 · DOI
  4. Allison, 1993, Burgess Shale biotas: burrowed away?, Lethaia, 26, 184, 10.1111/j.1502-3931.1993.tb01813.x · DOI
  5. Babcock, 2001, The Chengjiang biota; record of the early Cambrian diversification of life and clues to exceptional preservation of fossils, GSA Today, 11, 4, 10.1130/1052-5173(2001)011<0004:TCBROT>2.0.CO;2 · DOI
  6. Baker, 1985, Occurrence and formation of dolomite in organic-rich continental margin sediments, AAPG Bull., 69, 1917
  7. Baker, 1981, Constraints on the formation of sedimentary dolomite, Science, 213, 213, 10.1126/science.213.4504.214 · DOI · Paper page
  8. Briggs, 1997, The taphonomy and affinities of the problematic fossil Myoscolex from the Lower Cambrian Emu Bay Shale of South Australia, J. Paleontol., 71, 22, 10.1017/S0022336000038919 · DOI
  9. Chafetz, 1986, Marine peloids: a product of bacterially induced precipitation of calcite, J. Sediment. Petrol., 56, 812
  10. Coleman, 1985, Geochemistry of diagenetic non-silicate minerals: kinetic considerations, Philos. Trans. R. Soc. Lond., A, 315, 39, 10.1098/rsta.1985.0028 · DOI
  11. Compton, 1988, Degree of supersaturation and precipitation of organogenic dolomite, Geology, 16, 318, 10.1130/0091-7613(1988)016<0318:DOSAPO>2.3.CO;2 · DOI · Paper page
  12. Conway Morris, 1989, The persistence of Burgess Shale-type faunas: implications for the evolution of deeper-water faunas, Trans. R. Soc. Edinb. Earth Sci., 80, 271, 10.1017/S0263593300028716 · DOI
  13. Droser, 1988, Trends in depth and extent of bioturbation in Cambrian carbonate marine environments, western United States, Geology, 16, 233, 10.1130/0091-7613(1988)016<0233:TIDAEO>2.3.CO;2 · DOI · Paper page
  14. Droser, 2002, Trace fossils and substrates of the terminal Proterozoic–Cambrian transition: implications for the record of early bilaterians and sediment mixing, Proc. Natl. Acad. Sci., 99, 12572, 10.1073/pnas.202322499 · DOI
  15. Gaines, 2002, Depositional environments, ichnology, and rare soft-bodied preservation in the lower Cambrian Latham Shale, East Mojave, SEPM Pac. Sect. Book, 93, 153
  16. Henrichs, 1987, Anaerobic mineralization of marine sediment organic matter: rates and the role of anaerobic processes in the oceanic carbon economy, Geomicrobiol. J., 5, 191, 10.1080/01490458709385971 · DOI
  17. Hintze, 1975, Middle Cambrian stratigraphy of the House, Wah Wah, and adjacent ranges in Western Utah, Geol. Soc. Amer. Bull., 86, 881, 10.1130/0016-7606(1975)86<881:MCSOTH>2.0.CO;2 · DOI
  18. Irwin, 1980, Early diagenetic carbonate precipitation and pore fluid migration in the Kimmeridge Clay of Dorset, England, Sedimentology, 27, 577, 10.1111/j.1365-3091.1980.tb01648.x · DOI
  19. Kraemer, 2000, Lithology of the upper gas hydrate zone, Blake Outer Ridge: a link between diatoms, porosity, and gas hydrate, Proc. Ocean Drill. Program Sci. Results, 164, 229
  20. Lee, 1992, Controls on organic carbon preservation: the use of stratified water bodies to compare intrinsic rates of decomposition in oxic and anoxic systems, Geochim. Cosmochim. Acta, 56, 3323, 10.1016/0016-7037(92)90308-6 · DOI
  21. Montañez, 2000, Evolution of the Sr and C isotope composition of Cambrian oceans, GSA Today, 10, 1
  22. Moon, 1984, Fabric of mud and shales: an overview, vol. 15, 579
  23. Müller, 1987, Morphology, ontogeny, and life-habit of Agnostus pisiformis from the Upper Cambrian of Sweden, Fossils Strata, 19, 1, 10.18261/8200075117-1987-01 · DOI
  24. Mullins, 1985, Authigenic dolomite in Bahamian peri-platform slope sediment, Geology, 13, 292, 10.1130/0091-7613(1985)13<292:ADIBPS>2.0.CO;2 · DOI
  25. Petrovich, 2001, Mechanisms of fossilization of the soft-bodied and lightly armored faunas of the Burgess Shale and of some other classical localities, Am. J. Sci., 3001, 683, 10.2475/ajs.301.8.683 · DOI
  26. Powell, 2003, Greenschist-facies metamorphism of the Burgess Shale and its implications for models of fossil formation and preservation, Can. J. Earth Sci., 40, 13, 10.1139/e02-103 · DOI
  27. Rees, 1986, A fault-controlled trough through a carbonate platform: the middle Cambrian House Range embayment, GSA Bull., 97, 1054, 10.1130/0016-7606(1986)97<1054:AFTTAC>2.0.CO;2 · DOI
  28. Savrda, 1984, Development of a comprehensive oxygen-deficient marine biofacies model: evidence from Santa Monica, San Pedro, and Santa Barbara Basins, California continental borderland, AAPG Bull., 68, 1179
  29. Srodon, 2001, Quantitative X-ray diffraction analysis of clay-bearing rocks from random preparations, Clays Clay Miner., 49, 514, 10.1346/CCMN.2001.0490604 · DOI
  30. Tolmacheva, 2001, Evidence for 15 m.y. of continuous deep sea biogenic siliceous sedimentation in early Paleozoic oceans, Geology, 29, 755, 10.1130/0091-7613(2001)029<0755:EFMYOC>2.0.CO;2 · DOI · Paper page
  31. Tucker, 1974, Sedimentology of Paleozoic pelagic limestones; the Devonian Griotte (southern France) and Cephalopodenkalk (Germany), Spec. Publ. Int. Assoc. Sedimentol., 1, 71
  32. Wollanke, 1990, Petrographic and geochemical aspects of fossil embedding in exceptionally well preserved fossil deposits, Mitt. Geol.-Paläontol. Inst. Univ. Hamb., 69, 57

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Metadata

Authors
Gaines, R. R., Kennedy, M. J., & Droser, M. L.
Affiliations
  • Pomona College (US)
  • University of California, Riverside (US)
Corresponding author
Gaines, Robert R.
Venue
Palaeogeography, Palaeoclimatology, Palaeoecology
Publisher
Elsevier BV
Published
2005-05
Volume
220
Issue
1-2
Pages
193-205
ISSN
0031-0182 (ISSN-L)
OpenAlex
W2078057631
Cited by
113
References
5
Citations by year
2026: 1 · 2025: 1 · 2024: 2 · 2023: 4 · 2022: 5 · 2021: 1 · 2020: 7 · 2019: 3 · 2018: 5 · 2017: 7 · 2016: 10 · 2015: 7 · 2014: 10 · 2013: 2 · 2012: 10
FWCI
4.18
Type
journal article
Language
en
Open access
closed
Locations
  • Palaeogeography Palaeoclimatology Palaeoecology (publishedVersion)
  • Scholarship - Claremont (Claremont Colleges) (submittedVersion)
  • Adelaide Research & Scholarship (AR&S) (University of Adelaide) (submittedVersion)
Topics
  • Physical Sciences › Earth and Planetary Sciences › Paleontology › Paleontology and Stratigraphy of Fossils
  • Physical Sciences › Earth and Planetary Sciences › Paleontology › Paleontology and Evolutionary Biology
  • Physical Sciences › Earth and Planetary Sciences › Earth-Surface Processes › Geological formations and processes
Keywords
Burgess Shale, Wheeler Formation, House Range, Cambrian, Konservat-Lagerstätten, organic preservation, taphonomy, taphofacies, bottom water anoxia, oxygen minimum, bioturbation, permeability, clay minerals, carbonate cement, diagenesis, early diagenesis, origin of life

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