Zobrazeno 1 - 10
of 133
pro vyhledávání: '"S. Conway Morris"'
Publikováno v:
Palaeontology. 48:395-410
The supposed polychaete annelid Protonympha salicifolia, from the Upper Devonian (Frasnian) of New York State, USA, is redescribed. P. salicifolia has a bilateral and segmented body, but appears to have a ‘mattress-like’ construction with blade-l
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::5b3afc58535febcc54f90dca9c7e7d4b
https://doi.org/10.1111/j.1475-4983.2005.00449.x
https://doi.org/10.1111/j.1475-4983.2005.00449.x
Publikováno v:
Nature. 430:422-428
Deuterostomes are a remarkably diverse super-phylum, including not only the chordates (to which we belong) but groups as disparate as the echinoderms and the hemichordates. The phylogeny of deuterostomes is now achieving some degree of stability, esp
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::96f1a97ffbc260be633beea0736a35ca
https://doi.org/10.1038/nature02648
https://doi.org/10.1038/nature02648
Akademický článek
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Autor:
S. Conway Morris
Publikováno v:
Geological Magazine. 137:97-106
Despite the dynamism of living organisms, and we may assume their fossil counterparts, the study of their functional morphology has had a curiously static feel, most notably with its formulaic inclusion of Seilacher’s now famous triangle of constru
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::70d787cc903e48b5f72152cf57eeeb3a
https://doi.org/10.1017/s0016756800263668
https://doi.org/10.1017/s0016756800263668
Autor:
S. Conway Morris
Publikováno v:
Geological Magazine. 136:697-711
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::f920e99ad9f7bea0f70820dceb691442
https://doi.org/10.1017/s0016756899373325
https://doi.org/10.1017/s0016756899373325
Autor:
L. Chen, Jian Han, S. X. Hu, H. L. Luo, Min Zhu, Xingliang Zhang, Yong Li, Lei Chen, S. Conway Morris, Degan Shu
Publikováno v:
Nature. 402:42-46
The first fossil chordates are found in deposits from the Cambrian period (545–490 million years ago), but their earliest record is exceptionally sporadic and is often controversial. Accordingly, it has been difficult to construct a coherent phylog
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::875612893f2d29affd98a218143a1269
https://doi.org/10.1038/46965
https://doi.org/10.1038/46965
Publikováno v:
Nature. 400:746-749
Exceptional fossil preservation is critical to our understanding of early metazoan evolution. A key source of information is the Burgess Shale-type faunas1,2,3,4,5. Fossils from these deposits provide important insights into metazoan phylogeny, notab
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::f81051c2ef9b31d063c5396e4527237e
https://doi.org/10.1038/23445
https://doi.org/10.1038/23445
Publikováno v:
Scopus-Elsevier
Two new fossil worms are described from the Lower Cambrian Kinzers Formation of southeast Pennsylvania. Both are unique specimens.Kinzeria crinitanew genus and species has a body divided into three regions. The head bears a prominent set of elongate
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::0aa1e1bdb0441b55bd9a709e2b61d294
https://doi.org/10.1017/s0022336000027918
https://doi.org/10.1017/s0022336000027918
Autor:
S. Conway Morris
Publikováno v:
Geological Magazine. 136:331-340
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::90622bca0fa7983556433e765798f3d5
https://doi.org/10.1017/s0016756899312644
https://doi.org/10.1017/s0016756899312644
Autor:
S. Conway Morris
Publikováno v:
Geobios. 32:165-174
The overall pattern of ancient diversifications was apparent more than a century ago, and since thenhas shown no basic change. This suggests that the fossil record is both robust and reliable. Yet many questions remain to be answered. The recent surg
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::e7b4d92bed10211787c2348bd1572ec5
https://doi.org/10.1016/s0016-6995(99)80028-x
https://doi.org/10.1016/s0016-6995(99)80028-x