首页> 外文期刊>Palynology >High-resolution multi-proxy reconstruction of environmental changes in coastal waters of the Java Sea, Indonesia, during the late Holocene
【24h】

High-resolution multi-proxy reconstruction of environmental changes in coastal waters of the Java Sea, Indonesia, during the late Holocene

机译:在全新时期,印度尼西亚沿海水域环境变化的高分辨率多代理重建环境变化

获取原文
获取原文并翻译 | 示例
           

摘要

To obtain insight into the natural variability of the coastal ecosystems off southern Kalimantan, late Holocene environmental conditions between ca. 2850 and 990 cal yr BP in the Java Sea were investigated. A 134-cm-long sediment core collected approximate to 50 km off the Pembuang River mouth was analysed for organic-walled dinoflagellate cysts, pollen/spores and biogeochemical parameters, e.g. organic carbon (C-org), total nitrogen (N) and calcium carbonate (CaCO3) as well as carbon and nitrogen stable isotope composition (C-13, N-15). Sediments consist of mixed terrestrial as well as marine organic matter, are characterised by low nutrient uptake and suggest generally low river discharge that is supported by very low pollen and spore concentrations (256 pollen grains cm(-3) and 20 spores cm(-3) at maximum, respectively). Foraminifera and coccolithophores dominated the plankton over cyst-producing dinoflagellates and diatoms. Dinoflagellate cyst assemblages are composed mainly of oxidation-resistant species of the genera Operculodinium and Spiniferites with a minor contribution of Impagidinium (mainly I. strialatum). The percentages of round brown and peridinioid cysts are low and decrease from the bottom of the core to the top. Palynological and biogeochemical data appear well correlated and synchronously reflect changes in the marine environment. It is reconstructed that after ca. 2480 cal yr BP, bottom waters became increasingly ventilated. A typical open-water dinoflagellate cyst association is gradually replaced by a more coastal association between ca. 2480 and 1530 cal yr BP that is most likely attributed to El Nino-induced seasonal differences between dry and wet periods of the year. After 1530 cal yr BP, a more pronounced influence of the Pembuang River is indicated by an increase in N-15 and decreased C-13 which is supported by the occurrence of nutrient-sensitive Lingulodinium machaerophorum and Nematosphaeropsis labyrinthus. The overall results indicat
机译:从CA之间的全新世环境条件下期全新世环境条件下沿海生态系统的自然变异,以了解沿海生态系统的自然变异。 Java Sea中的2850和990 Cal YR BP进行了调查。为有机壁围绕的Dinoflagelate囊肿,花粉/孢子和生物地球化学参数分析了134厘米长的沉积物核心近似于Pembuang河口50公里。有机碳(C-ORG),总氮(N)和碳酸钙(CaCO 3)以及碳和氮稳定同位素组合物(C-13,N-15)。沉积物由混合的陆地和海洋有机物组成,其特征在于低营养吸收,并提出了由非常低的花粉和孢子浓度(256花粉晶粒Cm(-3)和20孢子Cm(-3)支撑的低河流放电)最大值)。 Foraminifera和Coccolithophores将浮游生物的浮游生物占据在囊肿的甲藻和硅藻土中。 Dinoflagelate囊肿组合主要由白葡聚糖杆菌和纺丝物种的抗氧化物种组成,具有轻微贡献的偶发性(主要是I. strialatum)。圆形棕色和赤素蛋白酶囊肿的百分比低,从芯的底部到顶部的底部较低。 Palynologic和BioEdochemical数据看起来很好地相关,并同步地反映了海洋环境的变化。在加利福之后重建它。 2480 Cal Yr BP,底部水域变得越来越通风。典型的开阔含Dinoflagellate囊肿关联逐渐被CA之间更沿海相关联的替代。 2480和1530 CAL YR BP最有可能归因于EL Nino-诱导的季节性差异,在今年的干燥和潮湿时期之间。在1530年CAL YR BP之后,Pembuang River的更明显的影响是通过N-15增加和降低的C-13,这是由营养敏感的鳞翅杆菌Machaerophoruphoruphoruphorum和Nematospheropsis迷宫的出现来支持的。整体结果指示

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号