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Sir Harry Godwin looks back over sixty years of life at Clare
College, the University of Cambridge and its very distinguished
school of Botany. He came to Clare in 1919 as an undergraduate,
became an early research student and was a Fellow from 1925. A
botanist, he was virtual founder of the science of Quaternary
Research in England, using the technique of pollen analysis to show
the age of plant remains and their distribution, especially in the
Fens and peat bogs of Eastern England. His History of the British
Flora (CUP 1956) is a classic. Sir Harry contemplates his threefold
life, as a deeply loyal college man, as a Cambridge researcher and
professor, as a member of the wider scientific world. He remembers
the long-past Cambridge of small college societies, still in touch
with the Victorian world, and tells of its characters and
conventions. He explains his own scientific work in terms that any
reader can understand. The whole story is a microcosm of Cambridge
and English life: the time and the world of Snow's The Masters, but
made more real and a great deal more genial.
Sir Harry Godwin has written a companion volume to his widely
acclaimed Fenland: its ancient past and uncertain future. He
follows the same historical approach that made Fenland so
interesting. Vast rain-fed peat bogs still cover the landscape of
northern and western Britain, their ecology, vegetation and flora
unfamiliar to most of our population. Yet, through the millennia
since last Ice Age, they have accumulated ever-deepening acidic
peat, whose plant remains are a precious archive of the events of
the past. Upon investigation, the reconstructed bog vegetation gave
clues to former climatic history, pollen analysis provided a
chronological scale dependent upon changes in upland forest
composition and archaeological objects from the Mesolithic to the
Roman period were recovered by peat-diggers from observed horizons
in the bogs. The Archives of Peat Bogs will be of great interest to
a wide readership comprising both amateur and professional
biologists, geologists, geographers, archaeologists, naturalists
and antiquarians.
The features so characteristic of the Fenland, its flatness, its
flooding, its vast stretches of silt land and black peat, its
drainage channels, meres, buried forests, abundant water fowl and
aquatic plants, its special crops, all relate to the special
conditions in which the Fenland was formed and ultimately was taken
over by man. This is the story, by one of the active participants,
of how the researches of natural scientists, biologists,
geologists, geographers, historians and archaeologists, over the
last fifty years have, by active co-operation and the use of modern
techniques, reconstructed Fenland history through the last 10,000
years and have provided fresh understanding both of its ancient
past and its uncertain future. It is the only such synthesis for
either specialist or general reader in a hundred years and it is
written in simple non-technical language and fully illustrated both
by photographs and drawings.
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