PLANT MACROFOSSIL RECORDS | Late Glacial Multidisciplinary Studies

Ammann, Brigitta; Birks, H.H.; Walanus, A.; Wasylikowa, K. (2013). PLANT MACROFOSSIL RECORDS | Late Glacial Multidisciplinary Studies. In: Elias, Scott A. (ed.) Encyclopedia of Quaternary Science (pp. 785-793). Elsevier 10.1016/B978-0-444-53643-3.00217-X

Text 2013_EncyclQuatSci_2nd_785.pdf - Published Version Restricted to registered users only Available under License Publisher holds Copyright. Download (1MB) | Request a copy

Amplitudes and rates of climate changes and environmental responses were especially high during the Late Glacial (ca. 16 000–11 500 years BP). By applying several methods on the same material (if possible on the same core to avoid correlation problems), the uncertainties and weaknesses of single disciplines can be reduced. Case studies are summarized to illustrate three types of research questions: What were the qualitative changes in the Late Glacial? How large were the temperature changes quantitatively? and What were the biotic responses to an independently recorded temperature change? Plant macrofossils play an important role in answering these questions. When several biostratigraphies and isotope stratigraphies are combined in a multidisciplinary study, we may disentangle the changes in various ecological factors, such as temperature, effective moisture, salinity, pH, or nutrient availability.

Interest & Impact

Downloads

2 since deposited on 15 Jan 2018
0 in the past 12 months

Citations

5 Citations in Web of Science ®
6 Citations in Scopus

Search

in Google Scholar™

Services

Actions (login required)

Edit item

Actions (login required)

Edit item