Diagenesis and Crystal Caskets: Echinoderm Mg Calcite Transformation, Dry Canyon, New Mexico, U.S.A.

ABSTRACT The stereom of living Echinus esculentus skeletons is composed of Mg calcite (interambulacral plates 6 mole % MgCO3; spines 4 mole % MgCO3) and is compared with the stereom of Pennsylvanian echinoderms from the Holder Formation, Dry Canyon. Some Dry Canyon echinoderms had their pore system (55% volume) filled by magnesian ferroan calcite cement before the stereom transformed (type 1) into small ( 20 µm diameter in ossicles that underwent type 2 transformation indicates ionic transfer over tens of microns. The margins of some (type 2) ossicles set in a clay matrix are Fe-rich and contain barite crystals; the Fe2+ and Ba2+ were transferred from the surrounding clay hundreds of microns into these ossicles. Type 1 transformation was catalyzed by internal water from the stereom; the presence of a ferroan calcite crystal casket confined alteration to the skeletal Mg calcite. Type 2 transformation involved both stereom and pore-filling Mg calcite cement. The unstable dolomite crystals formed by both transformation processes were protected from further change by the crystal caskets in which they are encased. The transformation of Dry Canyon echinoderms was probably triggered, or accelerated, by rising temperature caused by burial. The bulk composition of stereom that has undergone type 1 transformation can be used as a proxy for the original, major-element chemistry of echinoderm skeletons. Minor amounts of Mg calcite cement that occur in Dry Canon (type 1) ossicles indicate the chemistry of porewater close to the sediment-water interface. Fossil echinoderms are preserved in many ways, and it is suggested that their textural variations can be used to map the distribution of diagenetic reactions. The stereom is destroyed in most fossil echinoderms, and even in those where the stereom shape is preserved its internal structure is changed. Echinoderm Mg calcite does not transform with perfect textural preservation.

[1]  J. Dickson Transformation of echinoid Mg calcite skeletons by heating , 2001 .

[2]  Sang-Tae Kim,et al.  Equilibrium and nonequilibrium oxygen isotope effects in synthetic carbonates , 1997 .

[3]  N. Pingitore,et al.  Discrimination of sulfate from sulfide in carbonates by electron probe microanalysis , 1997, Carbonates and Evaporites.

[4]  J. Dickson,et al.  Exceptional preservation of the sponge Fissispongia tortacloaca from the Pennsylvanian Holder Formation, New Mexico , 1996 .

[5]  T. Frank,et al.  Diagenesis of fibrous magnesian calcite marine cement: Implications for the interpretation of δ18O and δ13C values of ancient equivalents , 1996 .

[6]  S. Burns,et al.  Recrystallization of dolomite: An experimental study from , 1996 .

[7]  J. Dodd,et al.  Taphonomic and sedimentologic implications of crinoid intraskeletal porosity , 1996 .

[8]  S. Gaffey H2O and OH in echinoid calcite: A spectroscopic study , 1995 .

[9]  J. Dickson Paleozoic Mg calcite preserved: Implications for the Carboniferous ocean , 1995 .

[10]  P. Buseck,et al.  Structure of magnesian calcite from sea urchins , 1993 .

[11]  E. Hiatt,et al.  Mineralogical Stabilization of High-magnesium Calcite: Geochemical Evidence for Intracrystal Recrystallization Within Holocene Porcellaneous Foraminifera , 1993 .

[12]  C. H. Moore,et al.  Well preserved, aragonitic phylloid algae (Eugonophyllum, Udoteaceae) from the Pennsylvanian Holder Formation, Sacramento Mountains, New Mexico , 1993 .

[13]  K. C. Lohmann,et al.  Sr/Mg ratios of modern marine calcite: Empirical indicators of ocean chemistry and precipitation rate , 1992 .

[14]  S. Mazzullo Geochemical and neomorphic alteration of dolomite: A review , 1992, Carbonates and Evaporites.

[15]  D. Budd Dissolution of high-Mg calcite fossils and the formation of biomolds during mineralogical stabilization , 1992, Carbonates and Evaporites.

[16]  P. Smalley,et al.  Carbon and oxygen isotopes in Pennsylvanian biogenic and abiogenic aragonite (Otero County, New Mexico): A laser microprobe study , 1991 .

[17]  S. Noeth,et al.  Tempered microdolomites in crinoids: A new criterion for high-grade diagenesis , 1990, Carbonates and Evaporites.

[18]  P. Swart,et al.  New distribution coefficient for the incorporation of strontium into dolomite and its implications for the formation of ancient dolomites , 1990 .

[19]  R. Goldstein Cement Stratigraphy of Pennsylvanian Holder Formation, Sacramento Mountains, New Mexico , 1988 .

[20]  F. Mackenzie,et al.  Stabilities of synthetic magnesian calcites in aqueous solution: Comparison with biogenic materials , 1987 .

[21]  S. Dorobek Petrography, Geochemistry, and Origin of Burial Diagenetic Facies, Siluro-Devonian Helderberg Group (Carbonate Rocks), Central Appalachians , 1987 .

[22]  B. Wilkinson,et al.  Rock Composition, Dolomite Stoichiometry, and Rock/Water Reactions in Dolomitic Carbonate Rocks , 1984, The Journal of Geology.

[23]  W. J. Meyers,et al.  Regional Distribution of Microdolomite Inclusions in Mississippian Echinoderms from Southwestern New Mexico , 1984 .

[24]  Detlev Richter,et al.  Zur Anwendung der Kathodolumineszenz in der Karbonatpetrographie , 1981 .

[25]  J. Neugebauer Drei Probleme der Echinodermendiagenese: Innere Zementation, Mikroporenbildung und der übergang von Magnesiumcalcit zu Calcit , 1979 .

[26]  W. J. Meyers,et al.  Microdolomite-rich syntaxial cements; proposed meteoric-marine mixing zone phreatic cements from Mississippian limestones, New Mexico , 1979 .

[27]  J. Pearse,et al.  Growth Zones in the Echinoid Skeleton , 1975 .

[28]  J. N. Weber Temperature Dependence of Magnesium in Echinoid and Asteroid Skeletal Calcite: A Reinterpretation of its Significance , 1973, The Journal of Geology.

[29]  T. G. Dix Biology of evechinus chloroticus (Echinoidia: Echinometridae) from different localities , 1972 .

[30]  J. P. Riley,et al.  The Distribution of the Major and Some Minor Elements in Marine Animals Part II. Molluscs , 1971, Journal of the Marine Biological Association of the United Kingdom.

[31]  E. Ghent,et al.  Electron microprobe study of magnesium distribution in some Mississippian echinoderm limestones from western Canada , 1970 .

[32]  M. Jensen Breeding and growth of Psammechinus miliaris (Gmelin) , 1969 .

[33]  J. B. Pilkington The organization of skeletal tissues in the spines of Echinus esculentus , 1969, Journal of the Marine Biological Association of the United Kingdom.

[34]  E. Gavish,et al.  Progressive diagenesis in Quaternary to late Tertiary carbonate sediments; sequence and time scale , 1969 .

[35]  J. N. Weber The incorporation of magnesium into the skeletal calcites of echinoderms , 1969 .

[36]  S. Gould,et al.  Pleistocene History of Bermuda , 1967 .

[37]  J. Dickson,et al.  A Modified Staining Technique for Carbonates in Thin Section , 1965, Nature.

[38]  H. B. Moore A Comparison of the Biology of Echinus esculentus in different Habitats. Part III. , 1934, Journal of the Marine Biological Association of the United Kingdom.

[39]  R. Reid,et al.  Recrystallization in Living Porcelaneous Foraminifera (Archaias Angulatis): Textural Changes Without Mineralogic Alteration , 1998 .

[40]  E. Grossman The carbon and oxygen isotope record during the evolution of Pangea: Carboniferous to Triassic , 1994 .

[41]  P. Sandberg Aragonite Cements and their Occurrence in Ancient Limestones , 1985 .