2006
DOI: 10.1080/00241160500409215
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Microreticulation in Cambrian Ostracoda and its relation to similar patterns in tertiary and Recent Ostracoda

Abstract: The Cambrian bradoriid ?Parahoulongdongella sp. is shown to have a microreticulate (2nd order) surface sculpture. A possible organic sheet-like origin is proposed for this reticulation. The relation between this second order pattern and those found in Tertiary to Recent Ostracoda is discussed.I Microreticulation, Ostracoda, Palaeozoic, surface tension.

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Cited by 3 publications
(2 citation statements)
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“…Ostracoda is one of the oldest crustacean groups; fossils of Ostracoda date back to the Cambrian age (Neil & Bell 2006). Because their carapace consists mainly of CaCO 3, fossilized forms can persist for long periods in sediments and soil.…”
Section: Introductionmentioning
confidence: 99%
“…Ostracoda is one of the oldest crustacean groups; fossils of Ostracoda date back to the Cambrian age (Neil & Bell 2006). Because their carapace consists mainly of CaCO 3, fossilized forms can persist for long periods in sediments and soil.…”
Section: Introductionmentioning
confidence: 99%
“…Various species here placed in Neohornibrookella have been previously placed in the genera Hermanites or Jugocythereis (Holden, 1976;Neil, 1994Neil, , 2000aNeil, , 2002Neil, , 2006Neil and Bell, 2006). Neohornibrookella species generally possess two rounded frontal muscles, the lower one often showing evidence of suturing and sometimes becoming fully divided to produce a frontal muscle scar pattern composed of three scars.…”
Section: Hermanites Jugocythereis and Thaerocythere Comparisonsmentioning
confidence: 99%