首页> 外文期刊>Boreas >First discovery of cryptotephra in Holocene peat deposits of Estonia, eastern Baltic
【24h】

First discovery of cryptotephra in Holocene peat deposits of Estonia, eastern Baltic

机译:在波罗的海东部爱沙尼亚的全新世泥炭矿床中首次发现隐孢子虫

获取原文
获取原文并翻译 | 示例
       

摘要

This article reports the first discovery of middle Holocene cryptotephra from a peat sequence in Estonia, eastern Baltic. Two sequences, Mustjarve and Parika (located 110 km apart), were chosen for a pilot study aimed at finding traces of tephra fallout during the middle Holocene. Peat accumulation at both sites started in the early Holocene (c. 9500 - 9000 C-14 yr BP; c. 11 000 - 10 000 cal. yr BP) and continued throughout the whole Holocene. The radiocarbon-dated intervals between c. 2000 and 5000 C-14 yr BP (c. 2000 - 5500 cal. yr BP) were chosen from both sites for the study. Colourless tephra shards were identified at 312 - 316 cm below the peat surface in the Mustjarve peat sequence, while no tephra was found in peat of the same age at Parika. Electron microprobe analyses suggest a correlation with the initial phase of the Hekla-4 eruption (c. 4260 cal. yr BP), although the age - depth model indicated an age around 4900 cal. yr BP. Small concentrations of colourless to light brown tephra shards at 266 - 270 cm in the Mustjarve sequence indicate that the Kebister tephra (c. 3750 cal. yr BP) might also be present, but geochemical analyses were not possible. The low concentration and small size of the tephra particles indicate that Estonian bogs are probably on the verge of where tephrochronology is possible in northwestern Europe. Further studies of full Holocene sequences are required in order to discover traces of other ash plumes reaching as far east as the eastern Baltic area.
机译:本文报道了从波罗的海东部爱沙尼亚的一个泥炭序列中首次发现全新世的隐密码虫。选择了两个序列,分别为Mustjarve和Parika(相距110 km)进行初步研究,目的是发现全新世中期的特菲拉尘埃的痕迹。两个地点的泥炭堆积始于全新世早期(约9500-9000 C-14年BP;约11000-10000 cal.yr BP),并贯穿整个全新世。 c之间的放射性碳测年间隔。从两个地点选择2000和5000 C-14 yr BP(约2000-5500 cal.yr BP)进行研究。在Mustjarve泥炭序列中,在泥炭表面以下312-316 cm处发现了无色的特非拉碎片,而在Parika的相同年龄的泥炭中未发现特非拉碎片。电子微探针分析表明与Hekla-4爆发的初期有关(约4260 cal。yr BP),尽管年龄-深度模型表明年龄约为4900 cal。年BP。在Mustjarve序列中,在266-270 cm处少量的无色至浅褐色的特弗拉碎片表明,也可能存在Kebister特弗拉(约3750 cal.yr BP),但无法进行地球化学分析。特非拉粒子的低浓度和小尺寸表明爱沙尼亚沼泽可能处于欧洲西北部可能进行年代学的边缘。为了发现远东至波罗的海东部地区的其他烟灰羽的痕迹,需要对全新世序列进行进一步研究。

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