Abstract
Secular variations in the proportion of Mg and Ca ions in seawater during the Phanerozoic have driven alternations between calcite seas (Mg:Ca < 2) and aragonite seas (Mg:Ca > 2). There is mounting evidence that these changes in seawater chemistry have impacted the evolution of marine organisms constructing calcareous skeletons, favouring calcite as the CaCO3 biomineral during times of calcite seas but aragonite during times of aragonite seas. It has been suggested that some organisms became hypercalcified when the mineralogy of their skeletons matched seawater type. This paper tests the proposal that calcitic trepostome bryozoans (‘stony bryozoans’) became hypercalcified in the calcite sea of the Ordovician. Data on two independent hypercalcification proxies—the diameter of branches, and exozonal wall thickness—have been compiled from the literature for ramose trepostome species from the Ordovician (calcite sea), Devonian (calcite sea) and Permian (aragonite sea). No significant difference was found in branch diameter between the calcite and aragonite sea periods, whereas wall thickness was found to be greater in the Permian than in the Ordovician and Devonian, counter to expectations. Either these two parameters are inadequate as proxies for hypercalcification or, more likely, trepostomes did not become hypercalcified in the calcite sea of the Early Palaeozoic, probably because they exerted a higher degree of control over their biomineralization than some other groups such as corals.
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References
Bartley JW, Anstey RL (1987) Growth of monilae in the Permian trepostome Tabulipora carbonaria: evidence for periodicity and a new model of stenolaemate wall calcification. In: Ross JRP (ed) Bryozoa: present and past. Western Washington University, Bellingham, pp 9–16
Berner RA (1975) The role of magnesium in the crystal growth of calcite and aragonite from sea water. Geochim Cosmochim Acta 39:489–494
Boardman RS (1960) Trepostomatous Bryozoa of the Hamilton Group of New York State. US Geol Surv Prof Pap 340:1–87
Brood K (1978) Upper Ordovician Bryozoa from Dalmanitina beds of Borenshult, Östergötland, Sweden. Geol Palaeont 12:53–72
Buttler CJ (1991a) Bryozoans from the Llanbedrog Mudstones (Caradoc), north Wales. Bull Br Mus (Nat Hist) (Geol) 47:153–168
Buttler CJ (1991b) A new Upper Ordovician bryozoan fauna from the Slade and Redhill Beds, South Wales. Palaeontology 34:77–108
Cuffey RJ, Fine RL (2005) The largest known fossil bryozoan reassembled from near Cincinnati. Ohio Geol 2005(1):1–4
Cuffey RJ, Cawley JJ, Lane JA, Bernarsky-Remington SM, Ansari SL, McClain MD, Ross-Phillips TL, Savill AC (2000) Bryozoan reefs and bryozoan-rich limestones in the Ordovician of Virginia. Proc 9th Int Coral Reef Symp, Bali 1:205–210
Ernst A (2001) Bryozoa of the Upper Permian Zechstein Formation of Germany. Senck leth 81:135–181
Ernst A, Key MM (2007) Upper Ordovician Bryozoa from the Montagne de Noire, southern France. J Syst Palaeontol 5:359–428
Gilmour EH, Snyder EM (2000) Bryozoa of the Mission Argillite (Permian), northeastern Washington. J Paleontol 74:545–570
Gilmour EH, McColloch ME, Wardlaw BR (1997) Bryozoa of the Murdock Mountain Formation (Wordian, Permian), Leach Mountains, northeastern Nevada. J Paleontol 71:214–236
Håkansson E, Madsen L (1991) Symbiosis - a plausible explanation of gigantism in Permian trepostome bryozoans. Bull Soc Sci Nat l'Ouest Fr Mém HS 1:151–159
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
Karklins OL (1984) Trepostome and cystoporate bryozoans from the Lexington Limestone and the Clays Ferry Formation (Middle and Upper Ordovician) of Kentucky. US Geol Surv Prof Pap 1066-I:1–105
Karklins OL (1985) Bryozoans from the Murfreesboro and Pierce Limestones (Early Blackriveran, Middle Ordovician), Stones River Group, of central Tennessee. Mem Paleontol Soc 15:1–42
Lowenstam HA, Weiner S (1989) On Biomineralization. Oxford University Press, New York, pp 1–324
Lowenstein TK, Timofeef MN, Brennan ST, Hardie LA, Demicco RV (2001) Oscillations in Phanerozoic seawater chemistry: evidence from fluid inclusions. Science 294:1086–1088
Madsen L, Håkansson E (1989) Upper Palaeozoic bryozoans from the Wandel Sea Basin, North Greenland. Rapp Grønlandsgeol Unders 144:43–52
McKinney FK (1971) Trepostomatous Ectoprocta (Bryozoa) from the lower Chickamauga Group (Middle Ordovician), Wills Valley, Alabama. Bull Am Paleontol 60:195–337
Morozova IP, Kruchinina ON (1986) Permskie mshanki Arktiki (Zapadnyĭ sektor). Akad Nauk SSSR Moscow, 1–144
Nakrem HA (1995) Bryozoans from the Lower Permian Voringen Member (Kapp Starostin Formation) Spitsbergen, Svalbard. Norsk Polarinst Skr 196:1–93
Perry TG (1962) Spechts Ferry (Middle Ordovician) bryozoan fauna from Illinois, Wisconsin, and Iowa. Circ Ill State Geol Surv 326:1–36
Porter SM (2007) Seawater chemistry and early carbonate biomineralization. Science 316:1302
Porter SM (2010) Calcite and aragonite seas and the de novo acquisition of carbonate skeletons. Geobiology 8:256–277
Reid CM (2003) Permian Bryozoa of Tasmania and New South Wales: systematics and their use in Tasmanian biostratigraphy. Mem Ass Austral Palaeontol 28:1–133
Ries JB (2010) Geological and experimental evidence for secular variation in seawater Mg/Ca (calcite- aragonite seas) and its effects on marine biological calcification. Biogeosciences 7:2795–2849
Ross JRP (1961) Ordovician, Silurian and Devonian Bryozoa of Australia. Bur Min Res Bull 50:1–172
Ross JRP (1967) Champlainian Ectoprocta (Bryozoa), New York State. J Paleontol 41:632–648
Ross JRP (1969) Champlainian (Ordovician) Ectoprocta (Bryozoa), New York State, Part II. J Paleontol 43:35–49
Ross JRP (1970) Distribution, paleoecology, and correlation of Champlainian Ectoprocta (Bryozoa), New York State, Part III. J Paleontol 44:346–382
Sandberg PA (1983) An oscillating trend in Phanerozoic non-skeletal carbonate mineralogy. Nature 205:19–22
Schäfer P, Bader B (2008) Geochemical composition and variability in the skeleton of the bryozoan Cellariasinuosa (Hassall): biological versus environmental control. Virginia Mus Nat Hist Spec Publ 15:269–279
Smith AM (2009) Bryozoans as southern sentinels of ocean acidification: a major role for a minor phylum. Mar Freshw Res 60:475–482
Smith AM, Key MM, Gordon DP (2006) Skeletal mineralogy of bryozoans: taxonomic and temporal patterns. Earth-Sci Rev 78:287–306
Stanley SM (2006) Influence of seawater chemistry on biomineralization throughout Phanerozoic time: paleontological and experimental evidence. Palaeogeogr Palaeoclimatol Palaeoecol 232:214–236
Stanley SM, Hardie LA (1998) Secular oscillations in the carbonate mineralogy of reef-building and sediment-producing organisms driven by tectonically forced shifts in sea-water chemistry. Palaeogeogr Palaeoclimatol Palaeoecol 144:3–19
Stanley SM, Hardie LA (1999) Hypercalcification; paleontology links plate tectonics and geochemistry to sedimentology. GSA Today 9:1–7
Stanley SM, Ries JB, Hardie LA (2002) Low-magnesium calcite produced by coralline algae in seawater of Late Cretaceous composition. Proc Natl Acad Sci USA 99:15323–15326
Stolarski J, Meibom A, Przenioslo R, Mazur M (2007) A Cretaceous scleractinian coral with a calcitic skeleton. Science 318:92–94
Suttner TJ, Ernst A (2007) Upper Ordovician bryozoans of the Pin Formation (Spiti Valley, Northern India). Palaeontology 50:1485–1518
Tavener-Smith R, Williams A (1972) The secretion and structure of the skeleton of living and fossil Bryozoa. Philos Trans R Soc Lond 264:97–159
Taylor PD (2008) Seawater chemistry, biomineralization and the fossil record of calcareous organisms. Pp. 21–29. In Okada H, Mawatari SF, Suzuki N, Gautam P (eds), Origin and Evolution of Natural Diversity, Proceedings of International Symposium "The Origin and Evolution of Natural Diversity", 1–5 October 2007, Sapporo:21–29
Taylor PD, Sendino C (2010) Latitudinal distribution of bryozoan-rich sediments in the Ordovician. Bull Geosci 85:565–572
Taylor PD, Wilson MA (1999) Dianulites: an unusual Ordovician bryozoan with a high-magnesium calcite skeleton. J Paleontol 73:38–48
Utgaard J, Perry TG (1964) Trepostomatous bryozoan fauna of the upper part of the Whitewater Formation (Cincinnatian) of eastern Indiana and western Ohio. Bull Indiana Dept Conser, Geol Surv 33:1–111
Xia Feng-sheng et al (1991) Early-Middle Permian bryozoans from Rutog region, Xizan (Tibet) [in Chinese]. In: Sun Dongli XuJuntao (ed) Papers for scientific co-expedition of the Nanjing Institute of Geology and Regional Geological Survey Team, Geological Bureau of Xizang Stratigraphy and Palaeontology of Permian, Jurassic and Cretaceous of the Rutog Region, Xizan (Tibet). Nanjing University Press, Nanjing, pp 166–214
Xia Feng-sheng (1997) Marine microfaunas (bryozoan, conodonts, and microvertebrate remains) from the Frasnian-Famennian interval in northwestern Junggar Basin of Xinjiang in China. Beitr Paläontol 22:91–207
Yang Jing-zhi, Hu Zhao-xun, Xia Feng-sheng (1988) Bryozoans from Late Devonian and Early Carboniferous of central Hunan. Palaeontol Sinica 174 (New Series B, 23):1–198
Acknowledgements
We are grateful to Dr. Andrej Ernst (Institut für Geowissenschaften, Kiel) and Dr. Abby Smith (University of Otago, Dunedin) for their comments on the manuscript. This study was commenced during a grant provided to PK by the Polish Ministry of Science and Higher Education (N N304 404038).
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Taylor, P.D., Kuklinski, P. Seawater chemistry and biomineralization: did trepostome bryozoans become hypercalcified in the ‘calcite sea’ of the Ordovician?. Palaeobio Palaeoenv 91, 185–195 (2011). https://doi.org/10.1007/s12549-011-0054-4
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DOI: https://doi.org/10.1007/s12549-011-0054-4