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
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DOI - Digital Object Identifier
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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
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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
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e-ISSN
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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
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