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南黄海西北部SYS-0803孔第四纪晚期底栖有孔虫群落特征及其古环境意义

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王飞飞, 王红, 刘健, 宫少军. 南黄海西北部SYS-0803孔第四纪晚期底栖有孔虫群落特征及其古环境意义[J]. 海洋地质与第四纪地质, 2011, 31(4): 113-123. doi: 10.3724/SP.J.1140.2011.04113
引用本文: 王飞飞, 王红, 刘健, 宫少军. 南黄海西北部SYS-0803孔第四纪晚期底栖有孔虫群落特征及其古环境意义[J]. 海洋地质与第四纪地质, 2011, 31(4): 113-123. doi: 10.3724/SP.J.1140.2011.04113
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WANG Feifei, WANG Hong, LIU Jian, GONG Shaojun. LATE QUATERNARY BENTHIC FORAMINIFERA OF CORE SYS-0803 FROM THE NORTHWESTERN SOUTH YELLOW SEA AND THEIR PALEOENVIROMENTAL SIGNIFICANCE[J]. Marine Geology & Quaternary Geology, 2011, 31(4): 113-123. doi: 10.3724/SP.J.1140.2011.04113
Citation: WANG Feifei, WANG Hong, LIU Jian, GONG Shaojun. LATE QUATERNARY BENTHIC FORAMINIFERA OF CORE SYS-0803 FROM THE NORTHWESTERN SOUTH YELLOW SEA AND THEIR PALEOENVIROMENTAL SIGNIFICANCE[J]. Marine Geology & Quaternary Geology, 2011, 31(4): 113-123. doi: 10.3724/SP.J.1140.2011.04113
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南黄海西北部SYS-0803孔第四纪晚期底栖有孔虫群落特征及其古环境意义

  • 1 国土资源部 海洋油气资源与环境地质重点实验室, 青岛 266071;

  • 2 青岛海洋地质研究所, 青岛 266071;

  • 3 天津华北地质勘查局 地质研究所, 天津 300171;

  • 4 天津市海洋地质勘查中心, 天津 300171

  • 基金项目:

    国土资源部地质调查项目(1212010611401)

    国家自然科学基金项目(40876034)

详细信息
    作者简介: 王飞飞(1984-),男,硕士,从事海洋地质微体古生物研究,E-mail:ffwang123@163.com

  • 中图分类号: P736.2

LATE QUATERNARY BENTHIC FORAMINIFERA OF CORE SYS-0803 FROM THE NORTHWESTERN SOUTH YELLOW SEA AND THEIR PALEOENVIROMENTAL SIGNIFICANCE

  • 1 Key Laboratory of Marine Hydrocarbon Resources and Environmental Geology, Ministry of Land and Resources, Qingdao 266071, China;

  • 2 Qingdao Institute of Marine Geology, Qingdao 266071, China;

  • 3 Tianjin North China Geological Exploration Bureau, Institute Of Geology, Tianjin 300171, China;

  • 4 Tianjin Exploration Center Of Marine Geology, Tianjin 300171, China

    摘要
  • SYS-0803孔取于南黄海西北部(35°02'N、121°45'E,水深49.00 m),其60.30 m长的柱状样记录了约140 ka以来的沉积环境演变。对248个样品中25个底栖有孔虫变量的Q型因子分析得到4个主因子,累计方差贡献为93.0%。通过底栖有孔虫组合分析,在140 ka以来的沉积中共发现4个海相层和4个陆相层,其中MIS 6晚期海侵层(孔深53.06~50.28 m)中以含典型暖水底栖有孔虫为特征,推测该时期可能存在有暖流;MIS 5e期高海面海相层(孔深33.76~30.55 m)中的微体化石群以典型的冷水底栖有孔虫和介形虫占优势,推断当时的黄海与现代一样,发育有强盛的冷水团。在冰后期海侵层位中发现了以短期海退为特征的YD事件(孔深13.80~12.91 m,12 460~11 572 cal.aBP)。
    The Core SYS-0803 was taken from the northwestern South Yellow Sea (35°02' N,121°45' E,water depth 49.00 m, core length 60.30 m), and it recorded the paleoenvironmental changes of the past~140 ka. Q-mode factor analysis was carried out for 248 samples and 25 benthic foraminiferal species, and 4 varimax factors were selected, which account for more than 93.0% of the total variance. Based on the benthic foraminiferal assemblages, four marine and four terrestrial strata were recognized in this core. The late MIS 6 marine layer (depth 53.06~50.28 m) contains typical warm-water benthic foraminifera, implying the occurrence of a warm current. The MIS 5e (depth 33.76~30.55 m) marine layer was remarked by the abundant cold-water benthic foraminifera and ostracods, indicating the development of a strong cold-water mass similar to the modern Cold-water Mass of the Yellow Sea. A short regression (depth 13.80~12.91 m, 12 460~11 572 cal.aBP)was found in the postglacial transgression layer, probably responding to the Younger Dryas event.
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收稿日期:  2011-04-18
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