Studies of the post-glacial history of British vegetation - III. Fenland polen diagrams - IV. Post-glacial changes of relative land- and sea-level in the English Fenland
Studies of the post-glacial history of British vegetation - III. Fenland polen diagrams - IV. Post-glacial changes of relative land- and sea-level in the English Fenland
复制标题
英国植被冰期后历史的研究 - III。
DOI：
--
复制
发表时间：
1940
期刊：
影响因子：
--
通讯作者：
H. Godwin
中科院分区：
文献类型：
--
作者：
H. Godwin
自1932年以来，剑桥芬兰研究委员会一直致力于解决芬兰盆地沉积物的历史问题，采用了许多适合于组成该机构的考古学家、地质学家、地理学家和植物学家的方法。由于芬兰盆地的很大一部分都充满了泥炭或泥炭或淤泥的交替层，对该地区植被发展的研究不可避免地意味着植物学工作与其他学科专家的工作相协调，并导致了芬兰地层学的研究。在本系列的前两篇论文中，已经对芬兰南部的地层进行了描述，因为这是通过研究泥炭层和其他层的横向连续性，通过观察其中的生物遗迹，并通过与考古学指标的相关性（戈德温和克利福德，1938年）来确定的。在这些论文中，相对较少提及花粉分析的结果，本文所关注的正是这种方法在芬兰沉积物研究中的应用。它的目的是增加另一种类型的证据，沼泽床的相关性，并表明，这一证据既证实和扩展的结果，以前描述。
Since 1932 the Cambridge Fenland Research Committee has been engaged in solving the problem of the history of the deposits of the Fenland basin, by the many methods appropriate to the archaeologists, geologists, geographers and botanists who make up that body. Since so large a part of the Fenland basin is filled with peat or with alternating beds of peat or silt, a study of vegetational development in the area has inevitably meant co-ordination of botanical work with that of specialists in other subjects, and has led, in itself, to a study of Fenland stratigraphy. In the two preceding papers of this series an account has been given of the stratigraphy of the southern part of the Fenlands, so far as this has been determinable by study of the lateral continuity of peat and other beds, by observations on the remains of organisms in them, and by correlation with archaeological indices (Godwin and Clifford 1938). In these papers comparatively little reference has been made to the results of pollen analysis, and it is with the application of this method to studies of Fenland deposits that the present paper is concerned. It purposes to add another type of evidence for the correlation of fen beds, and to show that this evidence both confirms and extends the results previously described.