Paleoclimate of Interglacial Marine Isotope Stage 11 (MIS 11) from Strata in the Japanese Isalands
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- Type
- article
- Published
- 2007-06-01
- Cited by
- 4
- References
- 17
- Access
- Open access
- OpenAlex
- https://openalex.org/W2580008456
- Semantic Scholar
- https://api.semanticscholar.org/CorpusID:128964752
Keywords
Interglacial, Paleoclimatology, Marine isotope stage, Geology, Milankovitch cycles
References
- 木更津-市原地域の瀬又,上泉および成田層の貝化石群とその産出層準
- Quaternary Geology of Osaka wiht Special Reference to Land Subsidence
- The Earth's Climate in the Next Hundred Thousand years (100 kyr)
- Gravelly spit deposits in a transgressive systems tract: the Pleistocene Higashikanbe Gravel, central Japan
- The Holocene CO2 rise: Anthropogenic or natural?
- Tephrochronological study on the middle Pleistocene deposits in the Kanto and Kinki districts, Japan
- Reconstruction of atmospheric CO2 from ice-core data and the deep-sea record of ontong Java plateau: the Milankovitch chron
- Contributions to Sequence Stratigraphy from the Quaternary Studies in Japan
- Marine hyperpycnal flows: initiation, behavior and related deposits. A review
- Compilation of the stratigraphy and molluscan fossil assemblages of the Pleistocene Shimosa Group, eastern part of Kwanto Plain, central Japan
- Characteristics of Hyperpycnal Flow and its Deposits as an Innovative Factor for the Turbidite Paradigm
- Pleistocene Gilbert-type coarse-grained delta, the Kamiizumi Formation, Shimosa Group, Japan.
- Sedimentary cycles and environments in the middle-late Pleistocene Shimosa Group, Boso Peninsula, central Japan.
- Middle Pleistocene depositional systems in the early paleo-Tokyo Bay, Japan.
- Faunal condensation in early phases of glacio-eustatic sea-level rise, found in the middle to late Pleistocene Shimosa Group, Boso Peninsula, central Japan
- Milankovitch and Climate
- Some Problems on the Middle Pleistocene deduced from Sediment Core Samples from Lake Biwa, Central Japan
Cited by
- Coastal staircase sequences reflecting sea-level oscillations and tectonic uplift during the Quaternary and Neogene
- Sea-level variation during MIS 11 constrained by stepwise Osaka Bay extensions and its relation with climatic evolution
- Relative sea-level fall since the last interglacial stage: Are coasts uplifting worldwide?
- Long-chain alkenones in the Shimosa Group reveal palaeotemperatures of the Pleistocene interglacial Palaeo-Tokyo Bays
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