Empirical 3D model of the conch of the Middle Jurassic ammonite microconch Normannites: its buoyancy, the physical effects of its mature modifications and speculations on their function

被引:43
作者
Tajika, Amane [1 ]
Naglik, Carole [1 ]
Morimoto, Naoki [2 ]
Pascual-Cebrian, Enric [3 ]
Hennhoefer, Dominik [3 ]
Klug, Christian [1 ]
机构
[1] Univ Zurich, Palaontol Inst & Museum, CH-8006 Zurich, Switzerland
[2] Kyoto Univ, Grad Sch Sci, Lab Phys Anthropol, Sakyo Ku, Kyoto 6068502, Japan
[3] Heidelberg Univ, Inst Geowissensch, D-69120 Heidelberg, Germany
基金
瑞士国家科学基金会;
关键词
grinding tomography; microconch ammonites; buoyancy; Jurassic; functional morphology; sexual dimorphism; SCAPHITID AMMONITES; POPULATION-DYNAMICS; DEVONIAN AMMONOIDS; HABITAT; PALEOBIOLOGY; TOMOGRAPHY; ISOTOPES; NAUTILUS; FOSSILS; CYCLES;
D O I
10.1080/08912963.2013.872097
中图分类号
Q [生物科学];
学科分类号
07 ; 0710 ; 09 ;
摘要
A 3D model of the Middle Jurassic ammonoid Normannites with an apertural modification from Thurnen, Switzerland, was constructed using physical-optical tomography. It was tested to determine whether the formation of the apertural modification affected shell orientation, to estimate buoyancy regulation and to reconstruct the mode of life of this ammonoid. No drastic postural changes occurred between the 3D models that excluded and included lappets, suggesting that the lappets were not formed to change the syn vivo shell orientation and, in turn, locomotion. We speculate that these adult shell modifications served to protect the soft parts during the reproduction period. Buoyancy calculations based on the model assume that ammonoids were positively buoyant when the phragmocone was devoid of liquid. When 31% of the entire phragmocone was filled with liquid, the living animal would have reached neutral buoyancy in contrast to 27% of cameral liquid filling when the weight of the aptychi is included. Provided that smaller ammonoids had more cameral liquid than bigger ammonoids, such as the modern Nautilus, Normannites examined in this study would have been able to maintain neutral buoyancy and might have had a demersal, nektobenthic or nektonic habitat somewhere in the water column.
引用
收藏
页码:181 / 191
页数:11
相关论文
共 75 条
  • [1] THE STABLE ISOTOPIC RECORDS OF FOSSILS FROM THE PETERBOROUGH MEMBER, OXFORD CLAY FORMATION (JURASSIC), UK - PALEOENVIRONMENTAL IMPLICATIONS
    ANDERSON, TF
    POPP, BN
    WILLIAMS, AC
    HO, LZ
    HUDSON, JD
    [J]. JOURNAL OF THE GEOLOGICAL SOCIETY, 1994, 151 : 125 - 138
  • [2] [Anonymous], PHILOS T ROYAL SOC L
  • [3] [Anonymous], 1996, AMMONOID PALEOBIOLOG
  • [4] [Anonymous], HDB PALAEONTOLOGICAL
  • [5] [Anonymous], 1840, SUPPLEMENT DICT SCI
  • [6] [Anonymous], 1962, Palaeontologia Polonica
  • [7] Antonov JI, 2009, NOAA ATLAS NESDIS, V2
  • [8] Bednarz M, 2009, PALAEONTOL ELECTRON, V12
  • [9] Callomon J. H., 1963, Transactions of the Leicester Literary and Philosophical Society, V57, P21
  • [10] Coemme S., 1917, Bulletin de la Societe Geologique Paris, V17