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Timing of high latitude peatland initiation since the Last Glacial Maximum. Pirita Oksanen, University of Bristol, School of Geographical Sciences . Introduction - PowerPoint PPT Presentation
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Timing of high latitude peatland initiation since the Last Glacial Maximum Pirita Oksanen, University of Bristol, School of Geographical Sciences
Contact [email protected]. Wetland data synthesis web site http://www.bridge.bris.ac.uk/projects/deglaciation/wetlands.html
AcknowledgementsEarlier databases by Gorham et al. (2005) and McDonald et al. (2006) are incorporated into this database. The ice sheets reconstructions are based on ICE-5G by Peltier (2004). Continental outlines are compiled by P. Bartlein.
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Europe % wetlands deglaciation 1 14,000 20,500 5 12,000 19,800 10 11,000 19,500 25 9500 17,000 50 8000 15,000 75 5000 12,000 90 3000 10,000
America wetlands deglaciation 17,000 16,000 15,000 15,000 13,500 14,000 12,000 13,000 9000 10,000 5500 8500 3000 8000
Siberia wetlands 14,000 12,000 11,000 10,000 8500 6000 3000
The study area and sites
Dates when percentage of total modern is reached for wetlands and deglaciation in three continents
Peatlands formed 21,000 – 15,750 cal BP
Peatlands formed at 13,000 cal BP +-250 yr
Peatlands formed at 12,000 cal BP +-250 yr
Peatlands formed at 9000 cal BP +-250 yr
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Methane concentration and mire initiationTemperature (Central Greenland core) and mire initiation
Cumulative mires and deglaciation
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Mire initiation as calculated 100 yr slices, and smoothed to 500 yr slices
IntroductionInformation from ca. 3000 late-Quaternary peat cores has been collected in a global wetland database within the QUEST-Deglaciation project. The data include modern wetland type, peat stratigraphy and dating. For the current study, 2500 basal dates from the northern latitudes above 39N are synthesised in order to establish the time of peatland initiation and to better understand the initiation patterns in different areas. Based on the collected data, a set of maps and time series is created, showing the change in peatland initiation and extent through time. These are compared with deglaciation and climate data. Relationships between some factors as age, peat depth and altitude, are tested. All dates are calibrated to calendar years BP using OxCal calibration programme. In future, extending the database to the southern latitudes, and adding stratigraphy and datings from the contributed sites would allow analyses on the evolution of different wetland types and changes in accumulation and methane emissions through time.
ResultsThere was no significant peat accumulation in the high-latitudes of the northern hemisphere during the Last Glacial Maximum. Deglaciation started in America at ca. 16,000 cal BP, and first peatlands appeared at the same time. In Europe, deglaciation started earlier, but first peatlands are recorded at around 15,000 cal BP. Most of the early peatlands in America are now buried. In non-glaciated Alaska the formation started at ca. 16,500 cal BP, but in Siberia considerably later, at ca. 14,500 cal BP. Latest mire initiation started in north-eastern Europe, Western Siberia (11,500) and the Hudson Bay area ( 9000 cal BP). A minor initiation peak at around 13,000 cal BP and the following trough at ca. 12,000 cal BP can be distinguished in most regions. In Alaska the 13,000 cal BP peak equals the later 10,500 cal BP peak. At its most active peatland initiation was between 11,000 and 9000 cal BP: the highest peak in America occurred at ca. 10,500 and across Eurasia at ca. 9000 cal BP. Half of the glaciers had melted from Europe by ca. 15,000 cal BP, and by ca. 10,000 cal BP from America. For peatlands, the half point was reached at 8000 and 9000 cal BP, respectively, and in Siberia, at 8500 cal BP. By around 7000 cal BP, when 60% of the modern peatlands existed, the distribution pattern was similar to today.
Region together with mire type predicts best the age of a peatland or peat layer, but the variability is large. Bogs show generally more constant accumulation rates than fens. Altitude makes little difference; most peatlands are located at lowlands, but peat of all ages is found at high altitudes too. Terrestrialisation was at its highest at the early stages, while during the most active time, the initiation was mainly of paludification type.
The cumulative initiation for all regions, including non-glaciated, correlate best with the northern hemisphere deglaciation. Initiation frequency and temperature reconstructions are in a good accordance from the LGM to ca. 8000 cal BP, after that small changes in temperature have little effect on peatland initiation. Rapid warming in America and enhanced continentality in Siberia likely affected the early peatland distribution patterns. Atmospheric CH4 concentration and initiation rates are strongly linked until ca. 5000 cal BP.
