Cited by 83

Pelagic palaeoecology: the importance of recent constraints on ammonoid palaeobiology and life history

Ritterbush, K. A., Hoffmann, R., Lukeneder, A., De Baets, K.·2014·Journal of Zoology

Abstract

A review of fossil evidence supports a pelagic mode of life (in the water column) of ammonoids, but they may have spent their life close to the seabottom (demersal), planktonically, or nektonically depending upon the ontogenetic stage and taxon. There are good indications for a planktonic mode of life of ammonoid hatchlings, but a broad range of reproductive strategies might have existed (egg‐laying, fecundity). Isotope and biogeographical studies indicate that some forms migrated or swam for considerable distances, whereas others may have been primarily transported by oceanic currents during early and/or late ontogeny. Diverse ammonoid habitats are also supported by evidence from predator–prey relationships derived from characteristic injuries and exceptional fossil finds, which indicate chiefly predatory or scavenging lifestyles. Sublethal injuries preserved in some ammonoid shells, as well as rare stomach and coprolite contents, provide evidence of predation by other cephalopods, arthropods and various jawed vertebrates. Various lines of evidence suggest that different groups of ammonoids had quite different ecologies, but shell shape alone can only give upper constraints on ammonoid capabilities, a matter that needs to be considered when interpreting their diversity and evolutionary history.

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  • In cephalopods, arms might perform the suction-feeding function, although arms have so far not been reported from fossil externally shelled cephalopods.

    “In cephalopods, arms might perform this function - although these have so far not been reported from fossil externally shelled cephalopods (Ritterbush et al. 2014, Clements et al. 2017).”

    From Palaeozoic evolution of animal mouthparts (2017) · cites this paper as Ritterbush et al. 2014

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Research works printed but not linked: 8

  1. Alegret, L., Thomas, E. & Lohmann, K.C. (2012). End- Cretaceous marine mass extinction not caused by produc- tivity collapse. Proc. Natl. Acad. Sci. USA 109, 728-732.
  2. House, M.R. (1989). Ammonoid extinction events. Philos. Trans. R. Soc. Lond. B. Biol. Sci. 325, 307-326.
  3. Hoving, H.J.T. & Robison, B.H. (2012). Vampire squid: detritivores in the oxygen minimum zone. Proc. Biol. Sci. 279, 4559-4567.
  4. Landman, N.H., Tanabe, K. & Davis, R.A. (1996). Ammo- noid paleobiology. New York: Plenum Press.
  5. Martill, D.M. (1990). Predation on Kosmoceras by semionotid fish in the middle Jurassic Lower Oxford Clay of England. Palaeontology 33, 739-742.
  6. Saunders, W.B. & Landman, N.H. (1987). Nautilus: the biology and paleobiology of a living fossil. New York: Plenum Press.
  7. Saunders, W.B. & Shapiro, E.A. (1986). Calculation and simulation of ammonoid hydrostatics. Paleobiology 12, 64-79.
  8. Saunders, W.B., Greenfest-Allen, E., Work, D.M. & Nikolaeva, S.V. (2008). Morphologic and taxonomic history of Paleozoic ammonoids in time and morphospace. Paleobiology 34, 128-154.

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Authors
Ritterbush, K. A., Hoffmann, R., Lukeneder, A., & De Baets, K.
Affiliations
  • Department of Earth Sciences University of Southern California Los Angeles CA USA
  • Institute for Geology, Mineralogy und Geophysics Ruhr University Bochum Bochum Germany
  • Department for Geology and Palaeontology Museum of Natural History Vienna Vienna Austria
  • Geozentrum Nordbayern Friedrich‐Alexander University Erlangen‐Nuremberg Erlangen Germany
Venue
Journal of Zoology
Publisher
Wiley
Published
2014-04
Volume
292
Issue
4
Pages
229-241
ISSN
  • 0952-8369
  • 1469-7998
Cited by
83
References
1
Language
en

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