Add to ORKGAnalyses of plant macrofossils can be used to reconstruct the development of the local vegetation on peatlands, and thus to elucidate successional processes. In the case of ombrotrophic peatlands, such analyses can also be used to generate palaeoclimate data. Identification of plant macrofossils in peat deposits is essential for accurate 14C dating. We present a brief overview of the sample pre-treatment procedure and available techniques for estimating macrofossil composition, and we recommend identification guides
Attributing the start of peat growth to an absolute timescale requires dating the bottom of peat dep...
Attributing the start of peat growth to an absolute timescale requires dating the bottom of peat dep...
Peat deposits are valuable archives for studying palaeoclimate, the history of local and regional ve...
Peatland vegetation from an ombrotrophic bog (Store Mosse bog) located in south-central Sweden. The ...
Plant macrofossils consist of reproductive and vegetative plant parts visible to the unaided eye. La...
ABSTRACT. The recently formed surface layers of peatlands are archives of past environmental conditi...
The analysis of plant macrofossils in peatland ecosystems has been widely used for the climatic and ...
In this article an attempt was made to explain some aspects of palaeoenvironmental studies. Analyses...
The chronologies of five northern European ombrotrophic peat bogs subjected to a large AMS 14C datin...
Detailed plant macrofossil analyses were performed on peat cores from an Allegan County, Michigan bo...
The need for Holocene peat-based palaeoclimatic records of increased temporal resolution has been wi...
Peat, especially from acidic mires (bogs), is a natural archive of past environmental change. Recons...
Peat deposits are valuable archives for studying palaeoclimate, the history of local and regional ve...
Peat molecular chemistry reflects a combination of plant input and decomposition. Both vegetation co...
The need for peat-based palaeoclimatic studies of increased temporal resolution has been identified ...
Attributing the start of peat growth to an absolute timescale requires dating the bottom of peat dep...
Attributing the start of peat growth to an absolute timescale requires dating the bottom of peat dep...
Peat deposits are valuable archives for studying palaeoclimate, the history of local and regional ve...
Peatland vegetation from an ombrotrophic bog (Store Mosse bog) located in south-central Sweden. The ...
Plant macrofossils consist of reproductive and vegetative plant parts visible to the unaided eye. La...
ABSTRACT. The recently formed surface layers of peatlands are archives of past environmental conditi...
The analysis of plant macrofossils in peatland ecosystems has been widely used for the climatic and ...
In this article an attempt was made to explain some aspects of palaeoenvironmental studies. Analyses...
The chronologies of five northern European ombrotrophic peat bogs subjected to a large AMS 14C datin...
Detailed plant macrofossil analyses were performed on peat cores from an Allegan County, Michigan bo...
The need for Holocene peat-based palaeoclimatic records of increased temporal resolution has been wi...
Peat, especially from acidic mires (bogs), is a natural archive of past environmental change. Recons...
Peat deposits are valuable archives for studying palaeoclimate, the history of local and regional ve...
Peat molecular chemistry reflects a combination of plant input and decomposition. Both vegetation co...
The need for peat-based palaeoclimatic studies of increased temporal resolution has been identified ...
Attributing the start of peat growth to an absolute timescale requires dating the bottom of peat dep...
Attributing the start of peat growth to an absolute timescale requires dating the bottom of peat dep...
Peat deposits are valuable archives for studying palaeoclimate, the history of local and regional ve...