Pollen floras were obtained from Miocene sediments recovered at four sites drilled during Ocean Drilling Program Leg 127. The local pollen floras of each site were correlated to the standard pollen zones of northeast Japan by using the concept of the essential members for each pollen zone. At Site 797, the complete floral range was obtained for recognition of the NP2 zone and the pollen components of the NP1 zone were also clarified continuously. The ages of the boundaries between pollen zones NP4/NP3, NP3/NP2, and NP2/NP1 are estimated to be about 7 Ma, 13 Ma, and 17-18.5 Ma, respectively. Even in the same pollen zone, the ratios of major pollen taxa vary with the location. This variation is expressed on maps representing two different tim...
More than 70 dinoflagellate cyst taxa have been encountered in a palynological study of 34 samples f...
International audiencePalynology contributes for long to stratigraphy, based on presence-absence of ...
The Jigokudani formation, considered to be late Miocene to early Pliocene in age, developed in the N...
This initial survey of pollen from 192 samples from Hole 794A, supplemented by 189 samples from Hole...
In this paper, the author has summarized almost all the Neogene pollenfloras of Japan. As a result o...
The analysis of 104 core-catcher samples from Site 603 resulted in a continuous palynological record...
A biomization method, which objectively assigns individual pollen assemblages to biomes (Prentice et...
A palynological study of samples from Ocean Drilling Program Site 767 in the Celebes Sea indicates t...
Stratigraphical and palynological studies on the Cenozoic deposits of the hilly area southeast of Ic...
A biomization method, which objectively assigns individual pollen assemblages to biomes ( Prentice e...
Middle Miocene to Holocene pollen assemblages reveal a history of environmental change in northern A...
Results of preliminary pollen analyses of 280 samples from selected intervals of cores from Hole 798...
In order to identify the northern latitudinal limit between mangroves composed of Avicennia only and...
Fifty-three sidewall samples of the boring well (Tsu-Ko-1) on the western slope of the Tsushima Trou...
Thermally altered and carbonised palynomorphs from the Omichidani Formation in the Tetori area of we...
More than 70 dinoflagellate cyst taxa have been encountered in a palynological study of 34 samples f...
International audiencePalynology contributes for long to stratigraphy, based on presence-absence of ...
The Jigokudani formation, considered to be late Miocene to early Pliocene in age, developed in the N...
This initial survey of pollen from 192 samples from Hole 794A, supplemented by 189 samples from Hole...
In this paper, the author has summarized almost all the Neogene pollenfloras of Japan. As a result o...
The analysis of 104 core-catcher samples from Site 603 resulted in a continuous palynological record...
A biomization method, which objectively assigns individual pollen assemblages to biomes (Prentice et...
A palynological study of samples from Ocean Drilling Program Site 767 in the Celebes Sea indicates t...
Stratigraphical and palynological studies on the Cenozoic deposits of the hilly area southeast of Ic...
A biomization method, which objectively assigns individual pollen assemblages to biomes ( Prentice e...
Middle Miocene to Holocene pollen assemblages reveal a history of environmental change in northern A...
Results of preliminary pollen analyses of 280 samples from selected intervals of cores from Hole 798...
In order to identify the northern latitudinal limit between mangroves composed of Avicennia only and...
Fifty-three sidewall samples of the boring well (Tsu-Ko-1) on the western slope of the Tsushima Trou...
Thermally altered and carbonised palynomorphs from the Omichidani Formation in the Tetori area of we...
More than 70 dinoflagellate cyst taxa have been encountered in a palynological study of 34 samples f...
International audiencePalynology contributes for long to stratigraphy, based on presence-absence of ...
The Jigokudani formation, considered to be late Miocene to early Pliocene in age, developed in the N...