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Mineralogy of cheilostome bryozoans across the Eocene–Oligocene boundary in Mississippi, USA

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Abstract

Different cheilostome bryozoan species construct their skeletons from calcite, aragonite, or a combination of these two minerals. Calcite is the primitive biomineral in cheilostomes, but an increasing number of clades since the Late Cretaceous have evolved the ability to biomineralize aragonite. This change in bryozoan mineralogy paralleled the switchover from calcite to aragonite seas. Here, we provide a first test of whether changing bryozoan biomineralogy can be correlated with a particular calcite to aragonite sea transition by comparing the mineralogical composition of bryozoan assemblages from the Eocene with those from the Early Oligocene, a time of major climatic and oceanographical changes that many believe to be a time of transition. Bryozoan assemblages from deposits in Mississippi and western Alabama preserving skeletal aragonite (as indicated by the occurrence of aragonitic molluscs) were sampled, cleaned, and sorted by species for XRD analysis to determine their mineralogy. The hypothesis that the proportion of species employing aragonite increases from the Eocene into the Oligocene through the transition to aragonite seas is not supported by our data. Among 23 Eocene species, 14 (61 %) were found to be calcitic, 7 (30 %) aragonitic and 2 (9 %) bimineralic, whereas among 28 Oligocene species 19 (68 %) were calcitic, 5 (18 %) aragonitic and 4 (14 %) bimineralic. Possible reasons why the expected mineralogical change is lacking include incorrect dating of the calcite to aragonite sea switchover at the Eocene–Oligocene boundary, the compensating effects of cooling at this time favouring calcite over aragonite biomineralization, or high levels of biological control over their mineralogy by the bryozoans.

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References

  • Berggren WA, Prothero DR (1992) Eocene-Oligocene climatic and biotic evolution; an overview. In: Prothero DR, Berggren WA (eds) Eocene–Oligocene Climatic and Biotic Evolution. Princeton University Press, Princeton, pp 1–28

    Google Scholar 

  • Bicker AR Jr (1969) Geologic map of Mississippi (1:500,000). Mississippi Office of Geology, Jackson, Mississippi

    Google Scholar 

  • Canu F, Bassler RS (1920) North American Early Tertiary Bryozoa. Bull US Natl Mus 106:1–879

    Google Scholar 

  • Cheetham AH (1963) Late Eocene zoogeography of the eastern Gulf Coast region. Mem Geol Soc Am 91:1–113

    Article  Google Scholar 

  • Cheetham AH, Sanner J, Jackson JBC (2007) Metrarabdotos and related genera (Bryozoa: Cheilostomata) in the Late Palaeogene and Neogene of Tropical America. J Paleont 81(Supplement 1):1–91

    Article  Google Scholar 

  • Cherns L, Wright VP (2000) Missing molluscs as evidence of large-scale, early aragonite dissolution in a Silurian sea. Geology 28:791–794

    Article  Google Scholar 

  • Cook PL, Chimonides PJ (1986) Recent and fossil Lunulitidae (Bryozoa, Cheilostomata) 6. Lunulites sensu lato and the genus Lunularia from Australasia. J Nat Hist 20:681–705

    Article  Google Scholar 

  • Conrad TA (1847) Observations on the Eocene formation, and descriptions of one hundred and five new fossils of that period, from the vicinity of Vicksburg, Mississippi, with an appendix. Proc Acad Natl Sci Philadelphia 3:280–299

    Google Scholar 

  • Defliese W, Hren MT, Lohmann KC, Van Tongeren JA (2011) Paleoclimate cooling in Eocene-Oligocene New Zealand revealed by clumped isotope thermometry. Am Geophys Union, Fall Meeting 2011:abstract #PP23C-02

  • Dockery DT III (1977) Mollusca of the Moodys Branch Formation. Mississippi: Miss Bur Geol Bull 120:1–212

    Google Scholar 

  • Dockery DT III (1980) The invertebrate micropaleontology of the Clarke County, Mississippi. Miss Bur Geol Bull 122:1–387

    Google Scholar 

  • Dockery DT III (1986a) Dobys Bluff tongue of the Kosciusko Formation and the Archusa Marl Member of the Cook Mountain Formation at Dobys Bluff on the Chickasawhay River, Clarke County, Mississippi. Geol Soc Am Cent Field Guide—Southeastern Sect, 14 p

  • Dockery DT III (1986b)The Cockfield (Claiborne Group), Moodys Branch and Yazoo (Jackson Group) Formations at the Riverside Park locality in Jackson, Mississippi; Geol Soc Am Cent Field Guide—Southeastern Sect, 26 p

  • Dockery DT III (1986c) Punctuated succession of Paleogene mollusks in the northern Gulf Coastal Plain. Palaios 6:582–589

    Google Scholar 

  • Dockery DT III (1996) Toward a revision of the generalized stratigraphic column of Mississippi. Miss Geol 17(1):1–9

    Google Scholar 

  • Dockery DT III, Lozouet P (2003) Molluscan faunas across the Eocene/Oligocene boundary in the North American Gulf coastal plain, with comparisons to those of the Eocene and Oligocene of France. In: Prothero DR, Ivany LC, Nesbitt EA (eds) From Greenhouse to Icehouse. The Marine Eocene-Oligocene Transition. Columbia University Press, New York, pp 303–340

  • Dockery DT III, Thompson DE (2011) The geology of Mississippi. Kickapoo, Clinton

    Google Scholar 

  • Echols RJ, Armentrout JM, Root SA, Fearn LB, Cooke JC, Rogers BK, Thompson PR (2003) Sequence stratigraphy of the Eocene/Oligocene boundary interval, southeastern Mississippi. In: Prothero DR, Ivany LC, Nesbitt EA (eds) From Greenhouse to Icehouse. The Marine Eocene-Oligocene Transition. Columbia University Press, New York, pp 189–222

    Google Scholar 

  • Frost SH (1977) Cenozoic reef systems in the Caribbean – prospects for ecological synthesis. Am Assoc Petroleum Geologists Stud Geol 4:93–110

    Google Scholar 

  • Hallock P, Premoli-Silva I, Boersma A (1991) Similarities between planktonic and larger formaminiferal evolutionary trends through Paleogene paleoceanographic changes. Paleaogeogr Palaeoclimatol Palaeoecol 83:49–64

    Article  Google Scholar 

  • Hardie LA (1996) Secular variation in seawater chemistry: an explanation for the coupled secular variation in the mineralogies of marine limestones and potash evaporates over the past 600 m.y. Geology 24:279–283

    Article  Google Scholar 

  • Ivany LC, Lohmann KC, Patterson WP (2003a) Paleogene temperature history of the U.S Gulf Coastal Plain inferred from d18O of fossil otoliths. In: Prothero DR, Ivany LC, Nesbitt EA (eds) From Greenhouse to Icehouse. The Marine Eocene-Oligocene Transition. Columbia University Press, New York, pp 232–251

    Google Scholar 

  • Ivany LC, Nesbitt EA, Prothero DR (2003b) The marine Eocene/Oligocene transition: a synthesis. In: Prothero DR, Ivany LC, Nesbitt EA (eds) From Greenhouse to Icehouse. The Marine Eocene-Oligocene Transition. Columbia University Press, New York, pp 522–534

    Google Scholar 

  • Lea I (1833) Contributions to Geology. Carey, Lea and Blanchard, Philadelphia

    Book  Google Scholar 

  • Lear CH, Bailey TR, Pearson PN, Coxall HK, Rosenthal Y (2008) Cooling and ice growth across the Eocene–Oligocene transition. Geology 36:251–254

    Article  Google Scholar 

  • Lowenstam HA, Weiner S (1989) On biomineralization. Oxford University Press, Oxford

    Google Scholar 

  • Lowenstein TK, Timofeef MN, Brennan ST, Hardie LA, Demicco RV (2001) Oscillations in Phanerozoic seawater chemistry: evidence from fluid inclusions. Science 294:1086–1088

    Article  Google Scholar 

  • Lui Z, Pagani M, Zinniker D, DeConto R, Huber M, Brinkhuis H, Shah SS, Lecki RM, Pearson A (2009) Global cooling during the Eocene–Oligocene climate transition. Science 323:1187–1190

    Article  Google Scholar 

  • Mancini EA, Tew BH (1991) Relationships of Paleogene stage and planktonic foraminiferal zone boundaries to lithostratigraphic and allostratigraphic contacts in the eastern Gulf Coast plain. J Foram Res 21:48–66

    Article  Google Scholar 

  • May JH (1974) Wayne County geology and mineral resources. Miss Geol Surv Bull 117:64–107

    Google Scholar 

  • Miller KG (1992) Middle Eocene to Oligocene stable isotopes, climate, and deep-water history: The Terminal Eocene Event? In: Prothero DR, Berggren WA (eds) Eocene –Oligocene Climatic and Biotic Evolution. Princeton University Press, Princeton, pp 160–177

    Google Scholar 

  • Miller KG, Thompson PR, Kent DV (1993) Integrated stratigraphy of the Alabama coastal plain: Relationship of upper Eocene to Oligocene unconformities to glacioeustatic change. Paleoceanography 8:313–331

    Article  Google Scholar 

  • Milliman JD (1974) Marine carbonates. Springer, Berlin

    Google Scholar 

  • Norman AM (1864) On undescribed British Hydrozoa, Actinozoa and Polyzoa. Ann Mag nat Hist (3)13: 82–90

  • Porter SM (2010) Calcite and aragonite seas and the de novo acquisition of carbonate skeletons. Geobiol 8:256–277

    Google Scholar 

  • Prothero DR, Berggren WA (1992) Eocene–Oligocene Climatic and Biotic Evolution. Princeton University Press, Princeton

    Google Scholar 

  • Prothero DR, Ivany LC, Nesbitt EA (2003) From Greenhouse to Icehouse: The Marine Eocene–Oligocene Transition. Columbia University Press, New York

    Google Scholar 

  • Sandberg PA (1983) An oscillating trend in Phanerozoic non-skeletal carbonate mineralogy. Nature 205:19–22

    Article  Google Scholar 

  • Smith AM, Key MM, Gordon DP (2006) Skeletal mineralogy of bryozoans: taxonomic and temporal patterns. Earth-Sci Rev 78:287–306

    Article  Google Scholar 

  • Stanley SM (2006) Influence of seawater chemistry on biomineralization throughout Phanerozoic time: Paleontological and experimental evidence. Palaeogeogr Palaeoclimatol Palaeoecol 232:214–236

    Article  Google Scholar 

  • Stanley SM, Hardie LA (1998) Secular oscillations in the carbonate mineralogy of reef-building and sediment-producing organisms driven by tectonically forced shifts in seawater chemistry. Palaeogeogr Palaeoclimatol Palaeoecol 144:3–19

    Google Scholar 

  • Stanley SM, Hardie LA (1999) Hypercalcification; paleontology links plate tectonics and geochemistry to sedimentology. GSA Today 9:1–7

    Google Scholar 

  • Steuber T, Rauch M (2005) Evolution of the Mg/Ca ratio of Cretaceous seawater: Implication from the composition of biological low-Mg calcite. Mar Geol 217:199–213

    Article  Google Scholar 

  • Stolarski J, Meibom A, Przenioslo R, Mazur M (2007) A Cretaceous scleractinian coral with a calcitic skeleton. Science 318:92–94

    Google Scholar 

  • Swart PK, James NP, Mallinson D, Malone MJ, Matsuda H, Simo T (2002) Data Report: Carbonate mineralogy of sites drilled during Leg 182. In: Hines AC, Feary DA, Malone MJ(eds) Proc Ocean Drilling Prog, Sci Res 182:http://www-odp.tamu.edu/publications/182_SR/010/010.htm

  • Szabo MW, Osborne WE, Copeland CW, Jr, Neathery T L (1988) Geologic map of Alabama (1:250,000). Alabama Geological Survey Special Map 220

  • Taylor PD, Kuklinski P (2011) Seawater chemistry and biomineralization: did trepostome bryozoans become hypercalcified in the ‘calcite sea’ of the Ordovician? Palaeobio Palaeoenv 91:185–195

    Article  Google Scholar 

  • Taylor PD, James NP, Bone Y, Kuklinski P, Kyser TK (2009) Evolving mineralogy of cheilostome bryozoans. Palaios 24:440–452

    Article  Google Scholar 

  • Toulmin LD (1977) Stratigraphic distribution of Paleocene and Eocene fossils in the eastern Gulf Coast region. Monogr Geol Surv Alabama 13:1–602

    Google Scholar 

  • Tucker ME (1988) Techniques in Sedimentology. Blackwell, Palo Alto

    Google Scholar 

  • Wade BS, Houben AJP, Quaijtaal W, Schouten S, Rosenthal Y, Miller KG, Katz ME, Wright JD, Brinkhuls H (2012) Multiproxy record of abrupt sea-surface cooling across the Eocene-Oligocene transition in the Gulf Of Mexico. Geology 40:159–162

    Article  Google Scholar 

  • Zanazzi A, Kohn MJ, MacFadden BJ, Terry DO Jr (2007) Large temperature drop across the Eocene–Oligocene transition in central North America. Nature 445:639–642

    Article  Google Scholar 

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Acknowledgements

We thank MMNS volunteers Joy Rushing and Peter Kuchirka for help with specimen collection in the field, and landowner permissions are always appreciated. Isabelle Malcolm undertook the XRD analyses. NPJ's fieldwork and XRD analyses were supported by the Natural Sciences and Engineering Council of Canada. Andrej Ernst (Institut für Geowissenschaften, Kiel) and an anonymous reviewer provided useful comments. Consuelo Sendino registered the NHMUK samples.

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Authors and Affiliations

  1. Department of Earth Sciences, Natural History Museum, Cromwell Road, London, SW7 5BD, UK

    Paul D. Taylor

  2. Department of Geological Sciences, Queen’s University, Kingston, Ontario, Canada, K7L 3N6

    Noel P. James

  3. Mississippi Museum of Natural Science, Jackson, Mississippi, USA, 39202

    George Phillips

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  1. Paul D. Taylor
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  2. Noel P. James
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Correspondence to Paul D. Taylor.

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Taylor, P.D., James, N.P. & Phillips, G. Mineralogy of cheilostome bryozoans across the Eocene–Oligocene boundary in Mississippi, USA. Palaeobio Palaeoenv 94, 425–438 (2014). https://doi.org/10.1007/s12549-014-0153-0

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