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GAO Yuan, ZHOU Ye-ze, QIN Tian, HOU Hong-xing, PEI Yang, KOU Fu-jian, YAN Bo. SPOROPOLLEN ASSEMBLAGE OF BLACK SOIL SECTION IN EASTERN LIAOHE PLAIN: Age and Paleoclimatic Implication[J]. Geology and Resources, 2024, 33(5): 617-625. doi: 10.13686/j.cnki.dzyzy.2024.05.001
Citation: GAO Yuan, ZHOU Ye-ze, QIN Tian, HOU Hong-xing, PEI Yang, KOU Fu-jian, YAN Bo. SPOROPOLLEN ASSEMBLAGE OF BLACK SOIL SECTION IN EASTERN LIAOHE PLAIN: Age and Paleoclimatic Implication[J]. Geology and Resources, 2024, 33(5): 617-625. doi: 10.13686/j.cnki.dzyzy.2024.05.001
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SPOROPOLLEN ASSEMBLAGE OF BLACK SOIL SECTION IN EASTERN LIAOHE PLAIN: Age and Paleoclimatic Implication

  • Langfang Natural Resources Comprehensive Survey Center, CGS, Langfang 065000, Hebei Province, China

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Received Date:  20 April 2023
Revised Date:  12 July 2023
Publish Date:  25 October 2024
    Abstract

  • By analysis of sporopollen in 0-1 m black soil profile PM25 in eastern Liaohe Plain, the fossils are divided into two sporopollen assemblages from bottom to top according to the sporopollen content change. The PM25-1 sporopollen assemblage is mainly Spiraea-Artemisia-Sanguisorba-Rosa-Echinate Asteraceae, with the climate changing from cold-dry to warm-wet; while the PM25-2 sporopollen assemblage is dominated by Pinus-Cyperaceae-Chenopodium, indicating the transition of climate from warm-wet to cold-dry. Combined with the 14C dating data, it is concluded that the black soil in eastern Liaohe Plain was mainly formed in Medieval Warm Period since 1335 a B.P.

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