Using bog archives to reconstruct paleopollution and vegetation change during the late Holocene

Tim Mighall, Simon Timberlake, D. A. Jenkins, John Grattan

Allbwn ymchwil: Pennod mewn Llyfr/Adroddiad/Trafodion CynhadleddPennod

Crynodeb

'In the past two decades there has been considerable work on global climatic change and its effect on the ecosphere, as well as on local and global environmental changes triggered by human activities. From the tropics to the Arctic, peatlands have developed under various geological conditions, and they provide good records of global and local changes since the Late Pleistocene. The objectives of the book are to analyze topics such as geological evolution of major peatlands basins; peatlands as self sustaining ecosystems; chemical environment of peatlands: water and peat chemistry; peatlands as archives of environmental changes; influence of peatlands on atmosphere: circular complex interactions; remote sensing studies of peatlands; peatlands as a resource; peatlands degradation, restoration, plus more.' * Presents an interdisciplinary approach, with an emphasis on Earth Science, and addresses the need for intergration between subdisciplines and the developing of new approaches * Synthesizes the evolutionary, ecological, and chemical characteristics of major peatlands, as well as focuses on the environmental changes, from climate changes to surface ares changes due to human activities * Covers topical studies of worldwide interest and provides examples from many different countries
Iaith wreiddiolSaesneg
TeitlPeatlands
Is-deitlEvolution and Records of Environmental and Climatic Changes
GolygyddionI. P. Martini, A. Martinez Cortizas, W. Chesworth
CyhoeddwrElsevier
Tudalennau413-434
Nifer y tudalennau22
ISBN (Argraffiad)978-0-444-52883-4, 0444528830
StatwsCyhoeddwyd - 01 Ebr 2007

Cyfres gyhoeddiadau

EnwDevelopments in Earth Surface Processes
CyhoeddwrElsevier

Ôl bys

Gweld gwybodaeth am bynciau ymchwil 'Using bog archives to reconstruct paleopollution and vegetation change during the late Holocene'. Gyda’i gilydd, maen nhw’n ffurfio ôl bys unigryw.

Dyfynnu hyn