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    Volume 46 Issue 3
    Mar.  2021
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    Article Contents
    Zhang Lanlan, Hu Bangqi, Qiu Zhuoya, Guo Jianwei, Ding Xue, Lu Jun, Xiang Rong, 2021. Records of Polycystine Radiolaria in the Diatom Mats Sediments from the Western Philippine Sea and Their Environmental Significance. Earth Science, 46(3): 853-865. doi: 10.3799/dqkx.2020.341
    Citation: Zhang Lanlan, Hu Bangqi, Qiu Zhuoya, Guo Jianwei, Ding Xue, Lu Jun, Xiang Rong, 2021. Records of Polycystine Radiolaria in the Diatom Mats Sediments from the Western Philippine Sea and Their Environmental Significance. Earth Science, 46(3): 853-865. doi: 10.3799/dqkx.2020.341

    Records of Polycystine Radiolaria in the Diatom Mats Sediments from the Western Philippine Sea and Their Environmental Significance

    doi: 10.3799/dqkx.2020.341
    • Received Date: 2020-09-08
    • Publish Date: 2021-03-01
    • In order to understand the formation process of marine laminar sediments from multiple perspectives, this paper studied the changes of polycystine radiolarian assemblages and their environmental significance by using the XT47 core samples with laminar diatom mats collected in the western Philippine Sea. Results show that there were abundant radiolarians, generally higher than 2×104 inds. g-1in the upper 260 cm depth; five times of alternating deposition of maximum radiolarian abundances and red clay occurred at the middle 260-460 cm depth; radiolarians in the bottom 460-630 cm depth were rare. According to the early occurrence of radiolarian species, the sediment age of > 470 cm depth was older than 0.34 Ma, suggesting the diatom sediments in the western Philippine Sea were formed since the Middle Pleistocene. The relative abundances of Tetrapyle group and Didymocyrtis tetrathalamus tetrathalamus, which are controlled by warm currents, significantly decreased during the last glacial maximum (LGM) period, indicating that the influence of North Equatorial warm current on the studied areas weakened during the LGM period. Interestingly, the variation of radiolarian abundance shows a different pattern, compared to the change of biogenic silica content, suggesting that the four peaks of biogenic silica content may be caused by the rapid increase of diatom, that is to say, the bloom of Ethmodiscus rex in the western Philippine Sea had a strong-weak fluctuation during the LGM period. Furthermore, four strong blooms of Ethmodiscus rex were found to be good correspondence to the low relative abundances of collodarians, and the high relative abundances of mediate-deep cold species. The former indicates that the stratification of upper water became weakened, and the latter reflects the increase of nutrients in mediate-deep water. Therefore, we believe that four strong blooms of Ethmodiscus rex during the LGM period may be caused by the weak stratification in the upper water and the upwelling of lower water with the abundant nutrients. Our results may provide a possible explanation for the long-term occurrence of the large diatom bloom and the formation of diatom mats with thickness up to three meters on the seafloor in the Phillippine Sea.

       

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