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Phylogeny of Paleozoic gastropods and origin of larval planktotrophy

The result's identifiers

  • Result code in IS VaVaI

    <a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00025798%3A_____%2F04%3A00000212" target="_blank" >RIV/00025798:_____/04:00000212 - isvavai.cz</a>

  • Result on the web

  • DOI - Digital Object Identifier

Alternative languages

  • Result language

    angličtina

  • Original language name

    Phylogeny of Paleozoic gastropods and origin of larval planktotrophy

  • Original language description

    A characteristic feature of early Palaeozoic gastropods is the development of a large embryonic shell, reflecting their lecithotrophic larval strategy. The initial whorl of most early Palaeozoic gastropods was openly coiled. This morphology was changed dramatically during the Late Silurian and Early Devonian. The vast majority of those forms was replaced gradually by gastropods developing a relatively small embryonic shell and having tightly coiled initial whorls. This major macroevolutionary trend in larval shell morphology coincided with the inception of larval planktotrophy, and was followed by the late Paleozoic radiation of Neritimorpha, Caenogastropoda, and Heterostropha. The inception of larval planktotrophy also coincided with fundamental changes in the biogeochemical evolution of the Palaeozoic oceans, and seems to have been closely linked to a pronounced increase of nutrient input to sea-surface waters during the Palaeozoic eutrophication episodes.

  • Czech name

    Fylogeneze paleozoických gastropódů a vznik larvální planktotrofie

  • Czech description

    A characteristic feature of early Palaeozoic gastropods is the development of a large embryonic shell, reflecting their lecithotrophic larval strategy. The initial whorl of most early Palaeozoic gastropods was openly coiled. This morphology was changed dramatically during the Late Silurian and Early Devonian. The vast majority of those forms was replaced gradually by gastropods developing a relatively small embryonic shell and having tightly coiled initial whorls. This major macroevolutionary trend in larval shell morphology coincided with the inception of larval planktotrophy, and was followed by the late Paleozoic radiation of Neritimorpha, Caenogastropoda, and Heterostropha. The inception of larval planktotrophy also coincided with fundamental changes in the biogeochemical evolution of the Palaeozoic oceans, and seems to have been closely linked to a pronounced increase of nutrient input to sea-surface waters during the Palaeozoic eutrophication episodes.

Classification

  • Type

    D - Article in proceedings

  • CEP classification

    DB - Geology and mineralogy

  • OECD FORD branch

Result continuities

  • Project

    <a href="/en/project/GA206%2F04%2F0599" target="_blank" >GA206/04/0599: Evolutionary changes of Paleozoic marine communities: evolution of Devonian gastropod communities and their reaction to rapidenvironmental changes</a><br>

  • Continuities

    P - Projekt vyzkumu a vyvoje financovany z verejnych zdroju (s odkazem do CEP)

Others

  • Publication year

    2004

  • Confidentiality

    S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

Data specific for result type

  • Article name in the collection

    World Congress of Malacology, Perth 2004, Western Australia, F. E. Wells (ed.)

  • ISBN

    1920843124

  • ISSN

  • e-ISSN

  • Number of pages

    2

  • Pages from-to

    42-43

  • Publisher name

    Neuveden

  • Place of publication

    Perth

  • Event location

    2004

  • Event date

    Jan 1, 2004

  • Type of event by nationality

    WRD - Celosvětová akce

  • UT code for WoS article