首页> 外文期刊>Earth and environmental science transactions of the Royal Society of Edinburgh >Spore assemblages from the Lower Devonian 'Lower Old Red Sandstone' deposits of the Northern Highlands of Scotland: the Berriedale Outlier
【24h】

Spore assemblages from the Lower Devonian 'Lower Old Red Sandstone' deposits of the Northern Highlands of Scotland: the Berriedale Outlier

机译:来自苏格兰北部高地下泥盆纪“下层老红砂岩”矿床的孢子组合:Berriedale离群值

获取原文
获取原文并翻译 | 示例
           

摘要

Assemblages of well-preserved dispersed spores have been recovered from the 'Lower Old Red Sandstone' deposits of the Berriedale Outlier in the Northern Highlands of Scotland. They belong to the annulatus-sextantii Spore Assemblage Biozone (AS SAB), in the spore zonation of Richardson & McGregor (1986), indicating an Early Devonian Emsian (but not earliest Emsian or latest Emsian) age. Comparison with the spore zonation of Streel et al. (1987) suggests they may be confined to the annulatus-bellatulus Oppel Zone (AB OZ), further constraining the age to early Emsian. This new biostratigraphical datum provides an age constraint for the onset of 'Lower Old Red Sandstone' sedimentation in the Orcadian Basin and, in particular, northwest of the Great Glen Fault System on the Northern Highlands. In the Orcadian Basin, there is a gap between 'Lower Old Red Sandstone' and 'Middle Old Red Sandstone' sedimentation, represented by either unconformity or disconformity, which appears to be variable in duration. In the Berriedale Outlier, it is estimated to represent up to 16 million years, but with an unknown thickness of 'Lower Old Red Sandstone' sequence removed at the unconformity. However, this basin-wide unconformity/disconformity is likely due to minor, local rather than large-scale, regional tectonism, and the evidence suggests little, if any, syn-depositional strike-slip movement along the Great Glen Fault System during Devonian 'Old Red Sandstone' deposition. The described spore assemblage is the most diverse AS SAB/AB OZ assemblage described from the British Isles. However, compared to contemporary spore assemblages from elsewhere on the Old Red Sandstone continent, the Scottish material is rather depauperate, with certain key taxa absent. This probably reflects subtle ecological effects, with the Scottish material representing restricted floras of the inland intermontaine basins.
机译:从苏格兰北部高地Berriedale外围地区的“较低的旧红砂岩”矿床中回收了保存完好的孢子组合。它们属于Richardson&McGregor(1986)的孢子带中的环-sextantii孢子组合生物区(AS SAB),表明早泥盆世的埃姆斯时代(但不是最早的埃姆斯时代或最新的埃姆斯时代)。与Streel等人的孢子区带比较。 (1987年)表明它们可能被限制在环-共生的欧佩尔带(AB OZ)中,这进一步限制了该年龄至早期的Emsian。这种新的生物地层基准为奥卡德盆地,特别是北高地大格伦断层系统的西北“低层老红砂岩”沉积的开始提供了年龄限制。在奥卡迪亚盆地,“下老红砂岩”和“中老红砂岩”的沉积之间存在间隙,表现为不整合或不整合,其持续时间似乎是可变的。在Berriedale离群值中,估计可以代表1600万年,但是不整合时去除了厚度未知的“下老红砂岩”序列。但是,这种盆地范围的不整合/不整合可能是由于较小的,局部的而不是大规模的区域构造,而且证据表明泥盆纪“大格伦断层系统”沿大格伦断裂系统的同沉积走滑运动很少(如果有)。老红砂岩的沉积。所描述的孢子组合是从不列颠群岛描述的最多样的AS SAB / AB OZ组合。但是,与旧红砂岩大陆其他地方的当代孢子组合相比,苏格兰的物质更加腐烂,缺少某些关键的分类单元。这可能反映了微妙的生态影响,苏格兰的材料代表了内陆山间盆地的有限植物区系。

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