Bryozoa from the Maastrichtian Korojon Formation, Western Australia - Fossils & Strata vol. 70 (ebok) av Eckart Håkansson
Eckart Håkansson , Dennis P. Gordon , Paul D. Taylor

Bryozoa from the Maastrichtian Korojon Formation, Western Australia ebok

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The taxonomically difficult ellipsocephalid trilobites from upper lower Cambrian (unnamed Stage 4) strata in Scandinavia are reviewed and revised. The suggested generic identities illustrate the diversification of the Ellipsocephalinae and advocate a modified correlation of the late to latest early Cambrian strata in Scandinavia and Baltica. The study is based primarily on material from the Gislö…
The taxonomically difficult ellipsocephalid trilobites from upper lower Cambrian (unnamed Stage 4) strata in Scandinavia are reviewed and revised. The suggested generic identities illustrate the diversification of the Ellipsocephalinae and advocate a modified correlation of the late to latest early Cambrian strata in Scandinavia and Baltica. The study is based primarily on material from the Gislöv Formation in Scania, southern Sweden, from which several species were originally known only from sparse and poorly preserved material. These are now described in more completeness and partly based on material that allows characterisation of ontogenetic developments.
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Undertittel Fossils & Strata vol. 70
Forfattere Eckart Håkansson (forfatter), Dennis P. Gordon (forfatter), Paul D. Taylor (forfatter)
Utgitt 29.04.2026
Sjanger
Språk English
Format epub
DRM-beskyttelse LCP
ISBN 9788215078144

The taxonomically difficult ellipsocephalid trilobites from upper lower Cambrian (unnamed Stage 4) strata in Scandinavia are reviewed and revised. The suggested generic identities illustrate the diversification of the Ellipsocephalinae and advocate a modified correlation of the late to latest early Cambrian strata in Scandinavia and Baltica. The study is based primarily on material from the Gislöv Formation in Scania, southern Sweden, from which several species were originally known only from sparse and poorly preserved material. These are now described in more completeness and partly based on material that allows characterisation of ontogenetic developments.
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