33 results on '"Kitaba, Ikuko"'
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2. Cryptotephra preserved in Lake Suigetsu (SG14 core) reveals the eruption timing and distribution of ash fall from Japanese volcanoes during the Late-glacial to early Holocene
3. The contemporary stable isotope hydrology of Lake Suigetsu and surrounding catchment (Japan) and its implications for sediment-derived palaeoclimate records
4. Reliable radiocarbon dating of fossil pollen grains: It is truly possible
5. Intermittent non-axial dipolar-field dominance of twin Laschamp excursions
6. Extraction method for fossil pollen grains using a cell sorter suitable for routine 14C dating
7. The spatio-temporal structure of the Lateglacial to early Holocene transition reconstructed from the pollen record of Lake Suigetsu and its precise correlation with other key global archives: Implications for palaeoclimatology and archaeology
8. Refining the eruptive history of Ulleungdo and Changbaishan volcanoes (East Asia) over the last 86 kyrs using distal sedimentary records
9. The contemporary stable isotope hydrology of Lake Suigetsu and surrounding catchment (Japan) and its implications for sediment-derived palaeoclimate records
10. Geochemical characterisation of the Late Quaternary widespread Japanese tephrostratigraphic markers and correlations to the Lake Suigetsu sedimentary archive (SG06 core)
11. High-resolution diatom record of paleoceanographic variations across the Early–Middle Pleistocene boundary in the Chiba Section, central Japan
12. Black ceramic spheres as marker grains for microfossil analyses, with improved chemical, physical, and optical properties
13. Understanding the human impact on Akita-sugi cedar (Cryptomeria japonica) forest in the late Holocene through pollen analysis of annually laminated sediments from Ichi-no-Megata, Akita, Japan
14. High resolution stratigraphy across the early–middle Pleistocene boundary from a core of the Kokumoto Formation at Tabuchi, Chiba Prefecture, Japan
15. High-Resolution Magneto–Climatostratigraphy of MIS 19 from the Osaka Group, Japan
16. Timing of the Matuyama–Brunhes geomagnetic reversal: Decoupled thermal maximum and sea-level highstand during Marine Isotope Stage 19
17. Midlatitude cooling caused by geomagnetic field minimum during polarity reversal
18. High-resolution record of the Matuyama—Brunhes transition constrains the age of Javanese Homo erectus in the Sangiran dome, Indonesia
19. High-resolution climate stratigraphy across the Matuyama–Brunhes transition from palynological data of Osaka Bay sediments in southwestern Japan
20. Refining the eruptive history of Ulleungdo and Changbaishan volcanoes (East \ud Asia) over the last 86 kyrs using distal sedimentary records
21. The Eurasian Modern Pollen Database (EMPD), version 2
22. Age control of the first appearance datum for Javanese Homo erectus in the Sangiran area
23. Integrating the Holocene tephrostratigraphy for East Asia using a high-resolution cryptotephra study from Lake Suigetsu (SG14 core), central Japan
24. Millennial-scale northern Hemisphere Atlantic-Pacific climate teleconnections in the earliest Middle Pleistocene
25. Geological support for the Umbrella Effect as a link between geomagnetic field and climate
26. Brief sea‐level fall event and centennial to millennial sea‐level variations during Marine Isotope Stage 19 in Osaka Bay, Japan
27. Geomagnetic field impact on paleoclimate: geological evidences during the Matuyama-Brunhes transition and Lower Jaramillo polarity reversal
28. Phase-lagged warming and the disruption of climatic rhythms during the Matuyama–Brunhes magnetic polarity transition
29. Late Pliocene magneto- and climatostratigraphic evolution toward the onset of the Quaternary in East Asia
30. Early Pleistocene plant fossil assemblages in the Ma2 Iayer of the Osaka Group from western Nara, Japan
31. MIS 21 and the Mid-Pleistocene climate transition: Climate and sea-level variation from a sediment core in Osaka Bay, Japan
32. The Eurasian Modern Pollen Database (EMPD), version 2
33. Age control of the first appearance datum for Javanese Homo erectus in the Sangiran area.
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