CoChat
Sign Up
Cited by 830Paleontology and Stratigraphy of FossilsCalcium Carbonate Crystallization and InhibitionGeochemistry and Elemental Analysis

The DOI matches its Crossref record; 80 of the 81 references it cites were found in a registry or an index.

Secular oscillations in the carbonate mineralogy of reef-building and sediment-producing organisms driven by tectonically forced shifts in seawater chemistry

Open access
Stanley, Steven M, Hardie, Lawrence A·1998·Palaeogeography, Palaeoclimatology, Palaeoecology
DOI 10.1016/s0031-0182(98)00109-6
Open this paper in CoChat — free accountOpen PDF

Abstract

The primary mineralogy of oolites and early marine carbonate cements led Sandberg [Nature 305 (1983), 19–22] to divide the Phanerozoic Eon into three intervals of `aragonite seas' and two intervals of `calcite seas'. Hardie [Geology 24 (1996), 279–283] has shown that these oscillations, together with synchronous oscillations in the mineralogy of marine potash evaporites, can be explained by secular shifts in the Mg/Ca ratio of seawater driven by changes in spreading rates along mid-ocean ridges. The Hardie model also predicts that high-Mg calcite should precipitate along with aragonite, as it does in today's aragonite sea. We have uncovered oscillations in the carbonate mineralogy of hypercalcifying organisms (ones that have produced massive skeletons, large reefs, or voluminous bodies of sediment) that correspond to Sandberg's aragonite seas and calcite seas and that are predicted by the Hardie model. Particular groups of corals, sponges, and algae appear to have been dominant reef builders only when favored by an appropriate Mg/Ca ratio in seawater. In early and middle Paleozoic calcite seas (Calcite I), reefs were dominated by calcitic tabulate, heliolitid, and rugose corals and calcitic stromatoporoids. In contrast, during the period of late Paleozoic–early Mesozoic aragonite seas (Aragonite II), aragonitic groups of sponges, scleractinian corals, and phylloid algae, as well as high-Mg calcitic red algae, were principal reef builders. During Late Cretaceous time, at the acme of Calcite II, massive rudists displaced aragonitic hermatypic corals. In today's aragonite sea (Aragonite III) scleractinian corals are again dominant reef builders, along with high-Mg calcitic coralline algae. Major sediment-producing algae exhibit temporal patterns similar to those of reef builders. Calcitic receptaculitids flourished during Calcite I, whereas aragonitic dasycladaceans did not become dominant rock formers until Aragonite II. During Calcite II, calcitic nannoplankton formed massive coccolith chalks in warm shallow seas of the Late Cretaceous, after the Mg/Ca ratio of seawater had reached a very low value and calcium concentration, a very high value. As the Mg/Ca ratio of seawater rose and calcium concentration fell during the Cenozoic Era, individual coccoliths, on average, became less massive and encrusted cells less thickly. By Pliocene time, during Aragonite III, the prominent genus Discoaster secreted only narrow-rayed coccoliths that covered less than 25% of the cell surface. Also during Aragonite III, the aragonitic green alga Halimeda emerged as the dominant skeletal sediment producer in reef tracts. The influence of seawater chemistry on skeletal secretion appears to have been especially strong for morphologically simple taxa that exert relatively weak control over their own calcification. Such groups include algae, sponges, corals, and bryozoans. Morphological simplicity also permits these groups to adopt vegetative or colonial modes of growth that confer success in competition for space on reefs. This linkage, in addition to the basic chemical demands of hypercalcification, has given the Mg/Ca ratio of seawater strong control over the success of individual reef-building taxa. More generally, this ratio appears to have strongly influenced evolutionary changes in the skeletal mineralogy of sponges and cheilostome bryozoans throughout their history. We conclude that throughout Phanerozoic time a chain of causation has extended from mid-ocean ridge processes, via seawater chemistry, to the mineralogical and biological composition of reef communities and bioclastic carbonate deposits.

Overview

Integrity signals

Registry

Crossref · 10.1016/s0031-0182(98)00109-6

Cites

80 of 80 references verified0 citation errors · 0 not checkable

Statistics

Recomputing p-values needs the paper’s full text.

Verification

Claims the paper makes

We couldn’t retrieve this paper’s full text, so its claims and self-check weren’t run. The registry and citation checks still apply.

Claims other papers make about this one

Each is checked against this paper’s own text: does it say what the citing paper says it does?

Citations

Cites

Show all 81 references

Research works printed but not linked: 19

  1. Berner, 1997, The rise of land plants and their effect on weathering and atmospheric CO2, Science, 291, 339
  2. Boardman, R S., Cheetham, A.H., 1987. Phylum Bryozoa. In: Boardman, R.S., Rowell, A.H. (Eds.), Fossil Invertebrates. Blackwell, Palo Alto, CA, pp. 497–549.
  3. Fischer, A.G., 1982. Long-term climatic oscillations recorded in stratigraphy. In: Berger, W. (Ed.), Climate in Earth History, National Research Council, Studies in Geophysics. National Academy Press, Washington, DC, pp. 97–104.
  4. Frost, S.H., 1977. Miocene to Holocene evolution of Caribbean Province reef-building corals. Proc., 3rd Int. Coral Reef Symposium, Miami, pp. 353–355.
  5. Füchtbauer, H., Hardie, L.A., 1980. Comparison of experimental and natural magnesian calcites (abstr.). International Association of Sedimentologists, Bochum, pp. 167–169.
  6. Hardie, 1997, Secular biotic trends in skeletal secretion and sedimentary carbonate production resulting from oscillations in seawater chemistry driven by plate tectonics, Eos, Trans. Am. Geophys. Union, 17, S179
  7. Kazmierczak, 1986, Calcium and the early eukaryotes, Mitt. Geol.-Paläontol. Inst., Univ. Hamburg, 61, 1
  8. Lippman, 1960, Versuche zur Aufklarung der Bildungsbedingungen von Calcit und Aragonit, Fortschr. Mineral., 38, 156
  9. Milliken, 1977, Variation of oceanic Mg/Ca ratio through time — implication of the calcite sea, Geol. Soc. Am., Abstr. Progr., 9, 64
  10. Mu, 1993, Late Cretaceous paleobiogeography of calcareous algae, Boll. Soc. Paleontol. Ital., 1, 333
  11. Oliver, W.A., Coates, A.G., 1987. Phylum Cnidaria. In: Boardman, R.S., Rowell, A.H. (Eds.), Fossil Invertebrates. Blackwell, Palo Alto, CA, pp. 140–193.
  12. Percival, 1977, Changes in calcareous nannoplankton in the Cretaceous–Tertiary biotic crisis at Zumaya, Spain, Evol. Theory, 2, 1
  13. Scott, 1984, Evolution of Early Cretaceous reefs in the Gulf of Mexico, Paleontogr. Am., 54, 406
  14. Senowbari-Daryan, B., Flügel, E., 1991. Tubiphytes Maslov, an enigmatic fossil: classification, fossil record and significance through time, Part I. Discussion of Late Paleozoic material. In: Barattolo, F., De Castro, P., Parente, M. (Eds.), Studies on Fossil Benthic Algae. Proc. 5th Int. Symp. Fossil Algae, Capri, 1991, pp. 353–382.
  15. Spencer, 1990, Control of seawater composition by mixing of river waters and mid-ocean ridge hydrothermal brines. In: Spencer, R.J., Chou, I.-M. (Eds.), Fluid–Mineral Interactions: A Tribute to H.P. Eugster, Geochem. Soc. Spec. Publ., 19, 409
  16. Stanley, 1997, Geobiology: studying the deep history of the earth-life system, Geol. Soc. Am., Abstr. Progr., 29, A21
  17. Van de Poel, 1994, Variations in Mesozoic–Cenozoic skeletal carbonate mineralogy, Geol. Mijnbouw, 73, 31
  18. Veizer, 1976, Mineralogy and chemical composition of recent and fossil skeletons of calcareous sponges, J. Archäol. Sci., 22, 558
  19. West, 1984, Palaeobiology and biological affinities of Palaeozoic chaetetids, Paleontogr. Am., 54, 337

Cited by

Sorted by citations

Items 501–600 of 825

Related

See all

Metadata

Authors
Stanley, S. M., & Hardie, L. A.
Affiliations
Johns Hopkins University (US)
Corresponding author
Stanley, Steven M
ORCID
Stanley, Steven M
Venue
Palaeogeography, Palaeoclimatology, Palaeoecology
Publisher
Elsevier BV
Published
1998-11
Volume
144
Issue
1-2
Pages
3-19
ISSN
0031-0182 (ISSN-L)
DOI
10.1016/s0031-0182(98)00109-6
OpenAlex
W2147427800
Cited by
830
References
81
Citations by year
2026: 33 · 2025: 26 · 2024: 29 · 2023: 24 · 2022: 28 · 2021: 24 · 2020: 36 · 2019: 34 · 2018: 22 · 2017: 29 · 2016: 38 · 2015: 26 · 2014: 37 · 2013: 38 · 2012: 47
FWCI
12.91
Type
journal article
Language
en
Open access
Licence
Locations
Palaeogeography Palaeoclimatology Palaeoecology (publishedVersion, cc-by-nc-nd)
Topics
  • Physical Sciences › Earth and Planetary Sciences › Paleontology › Paleontology and Stratigraphy of Fossils
  • Physical Sciences › Materials Science › Biomaterials › Calcium Carbonate Crystallization and Inhibition
  • Physical Sciences › Earth and Planetary Sciences › Geochemistry and Petrology › Geochemistry and Elemental Analysis
Keywords
calcite seas, carbonate mineralogy, Mg/Ca ratio, seawater chemistry, tectonic forcing, reef-building organisms, scleractinian corals, rudists, reef-building corals, red algae, coralline algae, nanoplankton, calcite precipitation, Phanerozoic

About these checks

Registry, retraction, Cites and statistics results are computed, not judged, with one exception: a printed reference that no index lists is read once by a model before it counts as a citation error. Claims are extracted by a model and kept only when their quote appears verbatim in the text; each cited source is then checked, with a model’s help, for whether it says what the claim relies on. Those verdicts can be wrong — read the claim’s quote and the cited source before relying on one.

Statistics and arithmetic are recomputed, not judged.

Confidence bands are shown only for fields calibrated on our annotated test set. None is calibrated yet, so no band is shown.

What counts as a claim ›How we measure confidence ›How we check this ›

Are you an author, or do you see a problem with this page? Request a review