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Equations of motion for post-mortem sinking of cephalopod shells and the sinking of Nautilus

Published online by Cambridge University Press:  08 April 2016

J. Scott Weaver
Affiliation:
Department of Physics, Queens College of the City University of New York; Flushing, New York 11367
John A. Chamberlain Jr.
Affiliation:
Department of Geology, Brooklyn College of the City University of New York; Brooklyn, New York 11210

Abstract

Consideration of the physics of sinking of hollow, rigid bodies leads to equations of motion for sinking cephalopod shells. We have derived equations of motion for three post-mortem sinking situations: sinking with a fixed amount of water in the phragmocone; rapid phragmocone filling (no siphuncular tube); and slow phragmocone filling (siphuncular tube intact). In all three cases sinking speed can be closely approximated by the terminal velocity calculated from the total weight, buoyancy, and drag parameters of the shell.

Experiments on modern Nautilus shells yield sinking velocities in agreement with calculated values. The experiments also show that orientation of a sinking Nautilus shell varies as the phragmocone fills with water. With small negative buoyancy the shell sinks with its plane of symmetry upright, but as it fills, it begins to rock from side to side and leans over and sinks with its plane of symmetry horizontal when the camerae are about 55% full.

The maximum sinking speed of upright adult Nautilus shells is approximately 30 cm/sec, which appears to be too small for embedding in the bottom upon impact. The maximum depth to which Nautilus sinks in the upright position ranges from about 7 m for rapidly filling shells to as much as 600 m for slowly filling shells. In the latter case, the shell will continue to fill after coming to rest on the bottom, and the stability of the vertical orientation will be removed within 1 or 2 days. Thus, primary vertical preservation of cephalopod shells indicates water depths less than about 10 m.

Type
Research Article
Copyright
Copyright © The Paleontological Society 

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References

Literature Cited

Chamberlain, J. A. Jr. 1969. Technique for scale modelling of cephalopod shells. Palaeontology. 12:4855.Google Scholar
Chamberlain, J. A. Jr. 1971a. Fluid Mechanics of the Ectocochliate Cephalopod Shell: an Experimental Study. 312 pp. Unpubl. Ph.D. thesis, Univ. of Rochester; Rochester, N.Y.Google Scholar
Chamberlain, J. A. Jr. 1971b. Shell morphology and the dynamics of streamlining in ectocochliate cephalopods. Geol. Soc. Am., Abstr. with Program Annu. Meet. 3:523524.Google Scholar
Chamberlain, J. A. Jr. 1973. Phyletic improvements in hydromechanical design and swimming ability in fossil nautiloids. Geol. Soc. Am. Abstr. with Program Annu. Meet. 5:571572.Google Scholar
Chamberlain, J. A. Jr. and Weaver, J. S. 1974. Sinking kinematics of nekroplanktonic cephalopod shells. Geol. Soc. Am. Abstr. with Program Annu. Meet. 6:685686.Google Scholar
Collins, D. H. and Minton, P. 1967. Siphuncular tube of Nautilus. Nature. 216:916917.Google Scholar
Hertel, H. 1966. Structure, Form and Movement. 251 pp. Reinhold; New York, N.Y.Google Scholar
Hildebrand, F. B. 1974. Introduction to Numerical Analysis. 2nd ed.669 pp. McGraw-Hill; New York, N.Y.Google Scholar
Hoerner, S. F. 1965. Fluid Dynamic Drag. 454 pp. Publ. by author; Midland Park, N.J.Google Scholar
Kummel, B. and Lloyd, R. M. 1955. Experiments on the relative streamlining of coiled cephalopod shells. J. Paleontol. 29:159170.Google Scholar
Mutvei, H. and Reyment, R. A. 1973. Buoyancy control and siphuncle function in ammonoids. Palaeontology. 16:623636.Google Scholar
Page, L. 1935. Introduction to Theoretical Physics. 653 pp. Van Nostrand; New York, N.Y.Google Scholar
Raup, D. M. 1967. Geometric analysis of shell coiling: coiling in ammonoids. J. Paleontol. 41:4365.Google Scholar
Raup, D. M. 1973. Depth inferences from vertically imbedded cephalopods. Lethaia 6:217226.CrossRefGoogle Scholar
Raup, D. M. and Chamberlain, J. A. Jr. 1967. Equations for volume and center of gravity in ammonoid shells. J. Paleontol. 41:566574.Google Scholar
Raup, D. M. and Takahashi, T. 1966. Experiments on strength of cephalopod shells. Geol. Soc. Am., Program Annu. Meet. pp. 172173. (Abstract.)Google Scholar
Relf, E. F. and Powell, C. H. 1917. Rep. Mem. Aeronaut. Res. Comm. Lond. No. 307.Google Scholar
Reyment, R. A. 1957. Some factors in the distribution of fossil cephalopods. Stockh. Contrib. Geol. 1:97184.Google Scholar
Reyment, R. A. 1968. Orthoconic nautiloids as indicators of shoreline surface currents. J. Sed. Petrol. 38:13871389.CrossRefGoogle Scholar
Reyment, R. A. 1970. Vertically inbedded cephalopod shells. Some factors in the distribution of fossil cephalopods, 2. Palaeogeogr., Palaeoclimatol., Palaeoecol. 7:103111.Google Scholar
Reyment, R. A. 1973. Factors in the distribution of fossil cephalopods. 3. Experiments with exact shell models of certain shell types. Bull. Geol. Inst. Univ. Upps. N.S. 4, Part 2:741.Google Scholar
Trueman, A. E. 1941. The ammonite body-chamber, with special reference to the buoyancy and mode of life of the living ammonite. Q. J. Geol. Soc. Lond. 96:339383.CrossRefGoogle Scholar
Westermann, G. E. G. 1973. Strength of concave septa and depth limits of fossil cephalopods. Lethaia. 6:383403.Google Scholar