Cited by 99Paleontology and Stratigraphy of FossilsEvolution and Paleontology StudiesPaleontology and Evolutionary Biology

The DOI matches its Crossref record, with a small difference in title or year; 7 of the 7 references it cites were found in a registry or an index.

Ichnodiversity and ichnodisparity: significance and caveats

Buatois, Luis A., Mángano, M. Gabriela·2013·Lethaia

Abstract

Ichnodiversity has been used as a proxy for environmental stress and stability in facies interpretations and to reconstruct evolutionary radiations and colonization histories in evolutionary palaeoecology. The three components of global diversity are exported from ecology and adapted for ichnology. Alpha ichnodiversity is used for palaeoenvironmental characterization, being assessed for individual facies. Beta ichnodiversity is commonly overlooked, although it may provide information about degree of similarity between ichnofaunas formed along environmental gradients. Gamma ichnodiversity may provide clues to detect ichnofossil provincialism. The concept of disparity may also prove to be significant in ichnological studies. Whereas ichnodiversity refers to ichnotaxonomic richness, ichnodisparity provides a measure of the variability of morphological plans in biogenic structures. Changes in global ichnodiversity do not necessarily parallel changes in ichnodisparity. For example, while the Cambrian explosion involved a dramatic increase in both, the Ordovician radiation essentially reflects an increase only in the former. Ichnodiversity and ichnodisparity should be used with caution because they are both affected by taphonomic processes. High diversity of superficial to shallow-tier trace fossils may result from enhanced preservation due a poorly developed mixed layer, rather than a true reflection of ecosystem performance, as shown by underexploited infaunal ecospace after biot…

Overview

Integrity signals

Registry

Crossref · 10.1111/let.12018

Cites

7 of 7 references verified0 citation errors · 0 not checkable

Statistics

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

Verification

Claims the paper makes

This paper’s full text isn’t openly available, 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?

  • Ichnodisparity provides a measure of the variability of basic morphological plans in biogenic structures, and consequently best records innovations in body plan, locomotory system and behavioural programme.

    “Although ichnodiversity simply refers to trace-fossil richness, ichnodisparity (i.e. number of trace-fossil architectural designs) provides a measure of the variability of basic morphological plans in biogenic structures, and consequently best records innovations in body plan, locomotory system and behavioural programme [20].”

Citations

Cites

Flagged first, then by citations

Research works printed but not linked: 99

  1. Bak, R.P.M. 1994: Sea urchin bioerosion on coral reefs: place in the carbonate budget and relevant variables. Coral Reefs 13, 99–103. · DOI
  2. Beatty, T.W., Zonnenveld, J.-P. & Henderson, C.M. 2008: Anomalously diverse Early Triassic ichnofossil assemblages in Northwest Pangea: a case for a shallow-marine habitable zone. Geology 36, 771–774. · DOI
  3. Briggs, D.E.G. & Fortey, R.A. 1989: The Early radiation and relationships of the major arthropod groups. Science 246, 241–243. · DOI · Paper page
  4. Briggs D.E.G. & Fortey R.A.. 2005: Wonderful strife: systematics stem groups and the phylogenetic signal of the Cambrian radiation. In Vrba E.S. Eldredge N. (eds): Macroevolution: Diversity Disparity Contingency: Supplement to Paleobiology volume 31 94–123. · DOI
  5. Briggs, D.E.G., Fortey, R.A. & Wills, M.A. 1992: Morphologic disparity in the Cambrian. Science 256, 1670–1673. · DOI · Paper page
  6. Bromley R.G. 1992: Bioerosion: eating rocks for fun and profit. In Maples C.G. West R.R. (eds): Trace Fossils: Paleontological Society Short Course volume 5 121–129. · DOI
  7. Bromley R.G. 1996. Trace fossils. Biology Taphonomy and Applications 361. pp.Chapman & Hall London. · DOI
  8. Bromley, R.G. & Asgaard, U. 1991: Ichnofacies: a mixture of taphofacies and biofacies. Lethaia 24, 15–163. · DOI
  9. Bromley, R.G. & Ekdale, A.A. 1986: Composite ichnofabrics and tiering of burrows. Geological Magazine 123, 59–65. · DOI
  10. Buatois, L.A. & Mangano, M.G. 1993: Ecospace utilization, paleoenvironmental trends and the evolution of early nonmarine biotas. Geology 21, 595–598. · DOI
  11. Buatois, L.A. & Mángano, M.G. 1998: Trace fossil analysis of lacustrine facies and basins. Palaeogeography, Palaeoclimatology, Palaeoecology 140, 367–382. · DOI
  12. Buatois, L.A. & Mángano, M.G. 2011b: The Déjà vu effect: recurrent patterns in exploitation of ecospace, establishment of the mixed layer, and distribution of matgrounds. Geology 39, 1163–1166. · DOI
  13. Buatois, L.A., Mángano, M.G., Maples, C.G. & Lanier, W.P. 1997: The paradox of nonmarine ichnofaunas in tidal rhythmites: integrating sedimentologic and ichnologic data from the Late Carboniferous of eastern Kansas, USA. Palaios 12, 467–481. · DOI
  14. Buatois, L.A., Mángano, M.G., Genise, J.F. & Taylor, T.N. 1998a: The ichnologic record of the invertebrate invasion of nonmarine ecosystems: evolutionary trends in ecospace utilization, environmental expansion, and behavioral complexity. Palaios 13, 217–240. · DOI
  15. Buatois, L.A., Mángano, M.G., Maples, C.G. & Lanier, W.P. 1998b: Ichnology of an upper carboniferous fluvio–estuarine paleovalley: the Tonganoxie Sandstone, Buildex Quarry, eastern Kansas. Journal of Paleontology 71, 152–180. · DOI
  16. Buatois, L.A., Mángano, M.G. & Sylvester, Z. 2001: A diverse deep marine ichnofauna from the Eocene Tarcau Sandstone of the Eastern Carpathians, Romania. Ichnos 8, 23–62. · DOI
  17. 10.2110/palo.2004.p04-32 · DOI
  18. Chamberlain, C.K. 1971: Morphology and ethology of trace fossils from the Ouachita Mountains, southeast Oklahoma. Journal of Paleontology 45, 212–246.
  19. Chen, Z.-Q. & Benton, M.J. 2012: The timing and pattern of biotic recovery following the end-Permian mass extinction. Nature Geoscience 5, 375–381. · DOI
  20. 10.1016/j.palaeo.2010.11.023 · DOI
  21. 10.1016/j.gr.2011.08.015 · DOI
  22. Crimes, T.P. 1970: Trilobite tracks and other trace fossils from the Upper Cambrian of North Wales. Geological Journal 7, 47–68. · DOI
  23. Crimes, T.P. 1974: Colonisation of the early ocean floor. Nature 248, 328–330. · DOI
  24. Crimes T.P. 1992. The record of trace fossils across the Proterozoic-Cambrian boundary. In Lipps J.H. & Signor P.W. (eds): Origin and Early Evolution of the Metazoa pp. 177–199. Plenus Press New York. · DOI
  25. Crimes T.P.. 1994: The period of early evolutionary failure and the dawn of evolutionary success. In Donovan S.K. (ed.) The Palaeobiology of Trace Fossils. John Wiley & Sons Chichester volume 105–133.
  26. Crimes, T.P. & Crossley, J.D. 1991: A diverse ichnofauna from Silurian flysch of the Aberystwyth Grits Formation, Wales. Geological Journal 26, 27–64. · DOI
  27. 10.1669/0883-1351(2002)017<0003:LCIFTC>2.0.CO;2 · DOI
  28. Droser, M.L., Jensen, S. & Gehling, J.G. 2002b: Trace fossils and substrates of the terminal Proterozoic–Cambrian transition: implications for the record of early bilaterians and sediment mixing. Proceedings of the National Academy of Sciences 99, 12572–12576. · DOI
  29. Droser M.L. Jensen S. & Gehling J.G.. 2004: Development of early Palaeozoic ichnofabrics: evidence from shallow marine siliciclastics. In McIlroy D. (ed.): The application of ichnology to palaeoenvironmental and stratigraphic analysis: Geological Society London Special Publication volume 228 383–396. · DOI · Paper page
  30. 10.1016/S0031-0182(85)80006-7 · DOI
  31. Ekdale, A.A. 1988: Pitfalls of paleobathymetric interpretations based on trace fossil assemblages. Palaios 3, 464–472. · DOI
  32. 10.1080/00241160152418410 · DOI
  33. Ekdale A.A. Bromley R.G. & Pemberton S.G. 1984: Ichnology Trace Fossils in Sedimentology and Stratigraphy: Society for Sedimentary Geology Short Course Notes 15 316 pp. SEPM Tulsa. · DOI
  34. Erwin D.H. 2006. Extinction.296pp. Princeton University Press Princeton
  35. Foote, M. 1993: Contributions of individual taxa to overall morphological disparity. Paleobiology 19, 403–419. · DOI
  36. Foote, M. 1997: The evolution of morphological diversity. Annual Review of Ecology and Systematics 28, 129–152. · DOI
  37. Fortey, R.A., Briggs, D.E.G. & Wills, M.A. 1996: The Cambrian evolutionary ‘explosion’: decoupling cladogenesis from morphological disparity. Biological Journal of the Linnean Society 57, 13–33.
  38. 10.1080/08120090903002656 · DOI
  39. Frey R.W. 1975: The realm of ichnology its strengths and limitations. In Frey R.W. (ed.): The study of trace fossils. A Synthesis of Principles Problems and Procedures in Ichnology. Springer–Verlag New York 13–38. · DOI
  40. Frey, R.W. & Howard, J.D. 1985: Trace fossils from the Panther Member, Star Point Formation (Upper Cretaceous), Coal Creek Canyon, Utah. Journal of Paleontology 59, 370–404.
  41. 10.1017/S0022336000019004 · DOI
  42. Frey R.W. & Pemberton S.G.. 1984: Trace fossils facies models. In Walker R.G. (ed.): Facies Models: Geoscience Canada Reprint Series volume 189–207.
  43. Frey, R.W. & Pemberton, S.G. 1985: Biogenic structures in outcrops and cores; I, Approaches to ichnology. Bulletin of Canadian Petroleum Geology 33, 72–115.
  44. 10.1111/j.1502-3931.1980.tb00632.x · DOI
  45. Genise, J.F. 2000: The ichnofamily Celliformidae for Celliforma and allied ichnogenera. Ichnos 7, 267–284. · DOI
  46. Genise J.F.. 2004: Ichnotaxonomy and ichnostratigraphy of chambered trace fossils in palaeosols attributed to coleopterans ants and termites. In: McIlroy D.. (ed.): The Application of Ichnology to Palaeoenvironmental and Stratigraphic Analysis: Geological Society Special Publication volume 228 419–453. · DOI
  47. Glynn P.W. 1997. Bioerosion and coral reef growth: a dynamic balance. In Birkeland C. (ed): Life and Death Of Coral Reefs pp. 69–98. Chapman and Hall New York. · DOI
  48. Gould, S.J. 1991: The disparity of the Burgess Shale arthropod fauna and the limits of cladistic analysis: why we must strive to quantify morphospace. Paleobiology 17, 411–423. · DOI
  49. Hallam A. & Wignall P.B. 1997. Mass Extinctions and Their Aftermath. 320. pp.Oxford University Press Oxford · DOI
  50. Hammer Ø. & Harper D.A.T. 2008. Paleontological Data Analysis. 351 pp. Blackwell Oxford.
  51. Hickman, C.S. 1993: Theoretical design space; a new program for the analysis of structural diversity; Progress in constructional morphology. Neues Jahrbuch fuer Geologie und Palaeontologie Abhandlungen 190, 169–182. · DOI
  52. 10.1016/j.palaeo.2011.07.014 · DOI
  53. Hutchings, P.A. 1986: Biological destruction of coral reefs A review. Coral Reefs 4, 239–252. · DOI
  54. Jensen S. Buatois L.A. & Mángano M.G. (in press): Palaeogeographical patterns in the distribution of Cambrian trace fossils. In Harper D. Servais T. (eds): Early Palaeozoic Palaeobiogeography and Palaeogeography: Geological Society of London Memoir volume .
  55. 10.1111/j.1365-3121.2010.00934.x · DOI
  56. MacEachern J.A. Pemberton S.G. Bann K.L. & Gingras M.K. 2007a: Departures from the archetypal Ichnofacies: effective recognition of environmental stress the rock record. In MacEachern J.A. Bann K.L. Gingras M.K. Pemberton S.G. (eds) Applied Ichnology: Society for Sedimentary Geology Short Course Notes volume 52 65–94. · DOI
  57. MacEachern J.A. Pemberton S.G. Bann K.L. & Gingras M.K. 2007b: The Ichnofacies paradigm: high-resolution paleoenvironmental interpretation of the rock record. In MacEachern J.A. Bann K.L. Gingras M.K. Pemberton S.G. (eds) Applied Ichnology: Society for Sedimentary Geology Short Course Notes volume 52 27–64. · DOI
  58. MacNaughton, R.B. & Zonneveld, J.P. 2010: Trace-fossil assemblages in the Lower Triassic Toad Formation, La Biche River map area, southeastern Yukon. Bulletin of Canadian Petroleum Geology 58, 100–114. · DOI
  59. Mángano M.G. & Buatois L.A. 2004: Ichnology of Carboniferous tide-influenced environments and tidal flat variability in the North American Midcontinent. In: McIlroy D.. (ed.): The application of ichnology to palaeoenvironmental and stratigraphic analysis: Geological Society Special Publication volume 228 157–178. · DOI
  60. Mángano M.G. & Droser M.L. 2004: The ichnologic record of the Ordovician radiation. In Webby B.D. Paris F. Droser M.L. Percival I.G. (eds): The great Ordovician biodiversification event. Columbia University Press New York 369–379. · DOI
  61. Mángano, M.G., Buatois, L.A., West, R.R. & Maples, C.G. 1998: Contrasting behavioral and feeding strategies recorded by tidal-flat bivalve trace fossils from the Upper Carboniferous of eastern Kansas. Palaios 13, 335–351. · DOI
  62. Mángano, M.G., Buatois, L.A., Maples, C.G. & West, R.R. 2000: A new ichnospecies of Nereites from Carboniferous tidal-flat facies of eastern Kansas, USA: implications for the Nereites-Neonereites debate. Journal of Paleontology 74, 149–157.
  63. Mángano, M.G., Buatois, L.A., West, R.R. & Maples, C.G. 2002: Ichnology of a Pennsylvanian equatorial tidal flat: the Stull shale member at Waverly, Eastern Kansas. Kansas Geological Survey 245, 1–133.
  64. Mángano, M.G., Buatois, L.A., Hofmann, R., Elicki, O. & Shinaq, R. (in press): Exploring the aftermath of the Cambrian Explosion: the evolutionary significance of marginal- to shallow-marine ichnofaunas of Jordan. Palaeogeography, Palaeoclimatology, Palaeoecology.
  65. McClain C.R. Rex M.A. & Etter R.J. 2009. Patterns in deep-sea macroecology. In Witman J.D. & Roy K. (eds): Marine Macroecology pp. 65–94. The University of Chicago Press London. · DOI
  66. Miller, A.I. 1997: Dissecting global diversity patterns: examples from the Ordovician radiations. Annual Review of Ecology and Systematics 28, 85–104. · DOI
  67. Orr, P.J. 1996: The ichnofauna of the Skiddaw Group (Early Ordovician) of the Lake District, England. Geological Magazine 133, 193–216. · DOI
  68. 10.1002/gj.891 · DOI
  69. Pruss, S. & Bottjer, D.J. 2004: Early Triassic trace fossils of the western United States and their implications for prolonged environmental stress from the end-Permian mass extinction. Palaios 19, 551–564. · DOI
  70. Pruss, S., Fraiser, M. & Bottjer, D.J. 2004: Proliferation of Early Triassic wrinkle structures: implications for environmental stress following the end-Permian mass extinction. Geology 32, 461–464. · DOI
  71. Pruss S.B. Corsetti F.A. & Bottjer D.J. 2005. Environmental trends of Early Triassic biofabrics: implications for understanding the aftermath of the end-Permian mass extinction. In Morrow J.D. Over D.J. & Wignall P.B. (eds): Understanding Late Devonian and Permian–Triassic Biotic and Climatic Events: Toward an Integrated Approach pp. 313–332. Elsevier Amsterdam. · DOI
  72. Raup, D.M. 1979: Size of the Permo-Triassic bottleneck and its evolutionary implications. Science 206, 217–218. · DOI
  73. Rindsberg, A.K. 1994: Ichnology of the upper Mississippian hartselle sandstone of Alabama, with notes on other Carboniferous Formations. Geological Survey of Alabama Bulletin 158, 1–107.
  74. Sanders, H.L. 1968: Marine benthic diversity: a comparative study. American Naturalist 102, 243–282. · DOI
  75. Sanders, H.L. 1969: Marine benthic diversity and the stability-time hypothesis. Brookhaven Symposia on Biology 22, 71–81.
  76. Schlirf, M. & Uchman, A. 2005: Revision of the ichnogenus Sabellarifex Richter, 1921 and its relationship to Skolithos Haldeman, 1840 and Polykladichnus Fürsich, 1981. Journal of Systematic Palaeontology 3, 115–131. · DOI
  77. Seilacher, A. 1974: Flysch trace fossils: evolution of behavioural diversity in the deep-sea. Neues Jahrbuch für Geologie und Palaontologie, Monatshefte 1974, 233–245.
  78. Seilacher A. 1977. Evolution of trace fossil communities. In Hallam A. (ed): Patterns of Evolution pp. 359–376. Elsevier Amsterdam. · DOI
  79. Seilacher, A. 1985: Trilobite paleobiology and substrate relationships. Transactions of the Royal Society of Edinburgh: Earth Sciences 76, 231–237. · DOI
  80. Seilacher A. 1992. An updated Cruziana stratigraphy of Gondwanan Palaeozoic sandstones. In Salem M.J. (ed): The Geology of Lybia 5 pp. 1565–1580. Elsevier Amsterdam.
  81. Seilacher, A. 1994: How valid is Cruziana stratigraphy? Geologische Rundschau 83, 752–758. · DOI
  82. Seilacher, A. & Seilacher, E. 1994: Bivalvian trace fossils: a lesson from actuopaleontology. Courier Forschungsinstitut Institut Senckenberg 169, 5–15.
  83. 10.1017/S0094837300011969 · DOI
  84. Systra, Y.J. & Jensen, S. 2006: Trace Fossils from the Dividalen Group of northern Finland with remarks on early Cambrian trace fossil provincialism. Geologiska Föreningens I Stockholm Förhandlingar 128, 321–325.
  85. Twitchett, R.J. 1999: Palaeoenvironments and the faunal recovery after the end-Permian mass extinction. Palaeogeography, Palaeoclimatology, Palaeoecology 154, 27–37. · DOI
  86. Twitchett R.J. & Barras C.G. 2004: Trace fossils in the aftermath of mass extinction events. In: McIlroy D.. (ed.): The Application of Ichnology to Palaeoenvironmental and Stratigraphic Analysis. Geological Society Special Publication volume 228 397–418. · DOI
  87. Twitchett, R.J. & Wignall, P.B. 1996: Trace fossils and the aftermath of the Permo-Triassic mass extinction: evidence from northern Italy. Palaeogeography, Palaeoclimatology, Palaeoecology 124, 137–151. · DOI
  88. Uchman, A. 1995: Taxonomy and paleoecology of flysch trace fossils: The Marnoso-arenacea Formation and associated facies (Miocene, Northern Apennines, Italy). Beringeria 15, 1–115.
  89. 10.1016/S0031-0182(02)00682-X · DOI
  90. Uchman A. 2004: Phanerozoic history of deep-sea trace fossils. In: McIlroy D.. (ed.): The Application of Ichnology to Palaeoenvironmental and Stratigraphic Analysis: Geological Society Special Publication volume 228 125–139. · DOI
  91. Valentine J.W. 1991. The sequence of body plans and locomotory systems during the Precambrian-Cambrian transition. In Schmidt-Kittler N. & Vogel K. (eds): Constructional morphology and evolution pp. 389–397. Springer-Verlag Berlin. · DOI
  92. Wetzel, A., Blechschmidt, I., Uchman, A. & Matter, A. 2007: A highly diverse ichnofauna in Late Triassic deep-sea fan deposits of Oman. Palaios 22, 567–576. · DOI
  93. Whittaker, R.H. 1960: Vegetation of the Siskiyou Mountains, Oregon and California. Ecological Monographs 30, 279–338. · DOI
  94. Whittaker, R.H. 1972: Evolution and measurement of species diversity. Taxon 21, 213–251. · DOI
  95. Wills, M.A. 1998: Cambrian and recent disparity: the picture from priapulids. Paleobiology 24, 177–199. · DOI
  96. 10.1111/j.1472-4669.2011.00299.x · DOI
  97. Zonneveld, J.P. 2011: Suspending the rules: unraveling the ichnological signature of the Lower Triassic post-extinction recovery interval. Palaios 26, 677–681. · DOI
  98. Zonneveld, J.P., Gingras, M.K. & Beatty, T.W. 2010a: Diverse ichnofossils assemblages following the P-T mass extinction, Lower Triassic, Alberta and British Columbia, Canada: Evidence for shallow marine refugia on the Northwestern coast of Pangea. Palaios 25, 368–392. · DOI
  99. Zonneveld, J.-P., MacNaughton, R.B., Utting, J., Beatty, S.G., Pemberton, S.G. & Henderson, C.M. 2010b: Sedimentology and ichnology of the Lower Triassic Montney Formation in the Pedigree-Ring/Border-Kahntah River area, northwestern Alberta and Northeastern British Columbia. Bulletin of Canadian Petroleum Geology 58, 115–140. · DOI

Cited by

Sorted by citations

Metadata

Authors
Buatois, L. A., & Mángano, M. G.
Affiliations
  • Department of Geological Sciences, University of Saskatchewan, 114 Science Place, Saskatoon, SK S7N 5E2, Canada;
  • University of Saskatchewan (CA)
Venue
Lethaia
Published
2013-07
Volume
46
Issue
3
Pages
281-292
ISSN
  • 0024-1164 (ISSN-L)
  • 1502-3931
OpenAlex
W2129714803
Cited by
99
References
7
Citations by year
2026: 5 · 2025: 13 · 2024: 8 · 2023: 5 · 2022: 13 · 2021: 11 · 2020: 7 · 2019: 7 · 2018: 12 · 2017: 4 · 2016: 10 · 2015: 1 · 2014: 2 · 2013: 1
FWCI
3.17
Type
journal article
Language
en
Open access
closed
Locations
Lethaia (publishedVersion)
Funders
Natural Sciences and Engineering Research Council (311727-05/08, 311726-05/08)
Topics
  • Physical Sciences › Earth and Planetary Sciences › Paleontology › Paleontology and Stratigraphy of Fossils
  • Physical Sciences › Earth and Planetary Sciences › Paleontology › Evolution and Paleontology Studies
  • Physical Sciences › Earth and Planetary Sciences › Paleontology › Paleontology and Evolutionary Biology
Keywords
ichnodiversity, trace fossils, ichnotaxonomy, paleoenvironmental reconstruction, facies analysis, taphonomy, Cambrian explosion, Ordovician radiation, end-Permian mass extinction, biotic crises, environmental stress

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