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日本花粉学会 | 論文
- 496 A 60,000 year record of vegetation change from Lake Towuti, central Sulawesi, Indonesia
- 119 Biomineralizations in extant mosses : a key to finding unrecognized fossils?
- 578 30 000-year vegetation and climate change around the East China Sea Shelf inferred from a high resolution pollen record
- 425 Justification, validation, and implication of aridity index for paleoclimate
- 562 Fertile organs and in situ spores of a dipteridaceous fern (Clathropteris obovata Oishi) from the Upper Triassic in Sichuan, China
- 294 Vegetation change across the Eocene-Oligocene Transition (EOT) : a case study from southern China
- 293 Cenozoic vegetation and climate changes in the subtropical East Asia : a case study from Guangxi, south China
- 455 Dinoflagellate stratigraphy around the Cenomanian/Turonian boundary in New Zealand
- 563 The Early Jurassic plants from the Shenzhen area of Guangdong Province, southern China and their significance
- 298 Modern pollen distributions in Qinghai-Tibetan Plateau and development of transfer functions for reconstructing Holocene environmental changes
- 575 Phytolith evidence of millet agriculture during about 6000-2100 cal. aBP. in the Guanzhong Basin, China
- 569 Cretaceous angiosperm woods and APG III : What orders and families are represented?
- 219 Occurrence of Sciadopitys-like fossil wood (Coniferales) in China
- 567 Understanding the early terrestrial palynological record : decay experiments and their taphonomic implications
- 606 Phytolith analysis for differentiating between foxtail millet (Setaria italica) and green foxtail (Setaria viridis)
- 398 Late Quaternary climate on the basis of pollen and diaspores from Kathmandu Basin, Nepal
- 192 Miocene-Pliocene vegetation changes of west southern Africa (Namibia)
- 540 A marine palynological study from off north-western Africa as a tool for land-sea correlation in the Late Pliocene
- 552 How plants conquered the land : An EvoDevo analysis of the spore wall
- 043 Eocene petrified wood from Parnell Draw : towards a more complete understanding of the diversity and paleoenvironment of the Green River Formation in southwestern Wyoming, USA
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