Oarai plant bed was discovered by Ozaki and Saito in 1954 on the shore of the river Naka in the vicinity of Iwai, Oarai Town situated on the east of Mito City (text-fig. 1). In the cliff on the river bank it is intercalated in thick conglomerate beds (1300m. thick) which have been thought Cretaceous in age and nominated by them the Oarai Formation. There the last is conformably overlain by the Nakaminato formation, 1800m. in thickness. Last year, Zamiophyllum Sequoia and a fragment probably of Dicotyledonous plant were collected by them from this plant bed, and Late Cretaceous was suggested by the writer for the age of the plants. Ozaki and Saito, on the other hand, reported Cfr. Didymoceras ? sp. and Bostrychoceras sp. from the Nakaminato ...
Abstract: A new collection of plant fossils from the Derevyannye Gory Formation of the New Siberia I...
Based upon the abundant fossil plants collected from the Tsukabara Formation of the third of the fiv...
The sample employed in this study is a piece of blue-grayish mudstone, dredged by the Hakusan-Maru o...
The Oarai flora involves 63 species in the 50 genera, and consist of the Hepaticae 1.6% ; Filicales ...
The present author has described in his previous paper (1959) the list of fossil plants from Oarai d...
Supplemental note of the previous paper entitled An Inspection of the Oarai Flora of Upper Gretaceou...
Supplemental note of the previous paper intitled Addition to the Oarai Flora of the Upper Cretaceous...
Supplemental note of the previous paper entitled The Second Addition to the Oarai Flora of the Upper...
The fossil plants treated with in this paper were obtained from Kamakuradate, Kamikanazawa and belon...
From the Byobugaura member, plant fossils have long been known to occur in silty or ligneous beds. T...
Our knowledge on the Nymphaeaccan plants of the Cretaceous age of our coun-try is limited. and the o...
Geological and paleontological studies of the Nakaminato area in Ibaraki Prefecture and of the Futab...
A new assemblage of Late Cretaceous fossil plants (the Kamikitaba assemblage) was discovered from th...
Erect fossil stumps were found from the outcrop of the Upper Triassic Hinabata Formation, the upperm...
金沢大学理工研究域自然システム学系The Middle Jurassic (Bathonian to Callovian) Kaizara flora is proposed herein for t...
Abstract: A new collection of plant fossils from the Derevyannye Gory Formation of the New Siberia I...
Based upon the abundant fossil plants collected from the Tsukabara Formation of the third of the fiv...
The sample employed in this study is a piece of blue-grayish mudstone, dredged by the Hakusan-Maru o...
The Oarai flora involves 63 species in the 50 genera, and consist of the Hepaticae 1.6% ; Filicales ...
The present author has described in his previous paper (1959) the list of fossil plants from Oarai d...
Supplemental note of the previous paper entitled An Inspection of the Oarai Flora of Upper Gretaceou...
Supplemental note of the previous paper intitled Addition to the Oarai Flora of the Upper Cretaceous...
Supplemental note of the previous paper entitled The Second Addition to the Oarai Flora of the Upper...
The fossil plants treated with in this paper were obtained from Kamakuradate, Kamikanazawa and belon...
From the Byobugaura member, plant fossils have long been known to occur in silty or ligneous beds. T...
Our knowledge on the Nymphaeaccan plants of the Cretaceous age of our coun-try is limited. and the o...
Geological and paleontological studies of the Nakaminato area in Ibaraki Prefecture and of the Futab...
A new assemblage of Late Cretaceous fossil plants (the Kamikitaba assemblage) was discovered from th...
Erect fossil stumps were found from the outcrop of the Upper Triassic Hinabata Formation, the upperm...
金沢大学理工研究域自然システム学系The Middle Jurassic (Bathonian to Callovian) Kaizara flora is proposed herein for t...
Abstract: A new collection of plant fossils from the Derevyannye Gory Formation of the New Siberia I...
Based upon the abundant fossil plants collected from the Tsukabara Formation of the third of the fiv...
The sample employed in this study is a piece of blue-grayish mudstone, dredged by the Hakusan-Maru o...