Quantitative paleoclimate reconstruction based on a 130 ka pollen record from the C9001C core off NE Japan
Autor: | Masaaki Okuda, Manami Sugaya, Makoto Okada |
---|---|
Rok vydání: | 2016 |
Předmět: |
Palynology
010506 paleontology Milankovitch cycles biology 010502 geochemistry & geophysics Pollen core biology.organism_classification medicine.disease_cause 01 natural sciences Subarctic climate Climatology Pollen Interglacial medicine Glacial period Beech Geology 0105 earth and related environmental sciences Earth-Surface Processes |
Zdroj: | Quaternary International. 397:404-416 |
ISSN: | 1040-6182 |
DOI: | 10.1016/j.quaint.2015.11.124 |
Popis: | Although monsoons are an important climatic factor in the Indo-Pacific region, the mechanism responsible for monsoon variations is not fully understood, particularly at the 10 5 year-scale, which includes the Milankovitch orbital cycles. Here, we provide a palynological result from the C9001C marine core drilled in the NW Pacific off the Shimokita Peninsula, eastern Japan. Based on the parallel δ 18 O record, the pollen record covers the past 130,000 years. During the interglacial periods (MIS1 and 5e), the C9001C core is dominated by cool temperate pollen of Fagus (beech) and Quercus subgenus Lepidobalanus (deciduous oak) that is similar to the present-day Shimokita vegetation. However, during the glacial periods (MIS2-4), the pollen spectra are dominated by subarctic elements of Betula (birch) and Picea (spruce), similar to the vegetation of Sakhalin and northern Hokkaido. These fossil pollen data are converted into quantitative climate variables by using the modern analog technique. Of the reconstructed paleoclimate variables, the mean annual temperature (Tann) correlates with the parallel δ 18 O record. By contrast, reconstructed precipitation in the summer (Psum) shows a similar pattern to the northern insolation variations particularly during MIS5, though the phase relation between the two curves requires further studies. |
Databáze: | OpenAIRE |
Externí odkaz: |