Middle Triassic megafossil plants from Long Gully, near Otematata, north Otago, New Zealand
Middle Triassic megafossil plants from Long Gully, near Otematata, north Otago, New Zealand
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DOI:
10.1080/03036758.1981.10421836
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发表时间:
1981-06
影响因子:
2.2
通讯作者:
G. Retallack
中科院分区:
文献类型:
--
作者:
G. Retallack
Abstract The Long Gully Formation of the Corbies Creek Group contains abundant remains of the low-diversity coastal vegetation characteristic of the Middle and Late Triassic Pacific margins of Gondwana. The plant-bearing rocks in Long Gully conformably overlie fossiliferous deltaic and marine Ladinian rocks (Kaihikuan local stage). A variety of fossil fructifications were found, allowing better understanding of the botanical affinities of the plants. Fertile remains referred to Todites maoricus sp. nov., indicate osmundalean affinities for one common kind of sphenopterid fern frond. Townrovia petasata gen. et sp. nov. is the likely microsporophyll and ? Peltaspermum sp. indet. the likely megasporophyll of seed fern leaves referred to Pachydermophyllum, represented at Long Gully by P. dubium (Burges) comb. nov. and P. praecordillerae (Frenguelli) comb. nov. The ovulate voltziacean conifer cone Telemachus lignosus sp. nov. and “unidentified cone B” may be fructifications of a species also producing leaves r...