Late-glacial pollen and diatom changes in response to two different environmental perturbations: volcanic eruption and Younger Dryas cooling-Reference-Cited by-同舟云学术

Late-glacial pollen and diatom changes in response to two different environmental perturbations: volcanic eruption and Younger Dryas cooling

Published:1995-07 Issue:1 Volume:14 Page:23-47
ISSN:0921-2728
Container-title:Journal of Paleolimnology
language:en
Short-container-title:J Paleolimnol

Author:

Lotter A. F.,Birks H. J. B.,Zolitschka B.

Publisher

Springer Science and Business Media LLC

Subject

Earth-Surface Processes,Aquatic Science

Link

http://link.springer.com/content/pdf/10.1007/BF00682592.pdf

Reference100 articles.

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2. Alley, R. B.et al. 1993. Abrupt increase in Greenland snow accumulation at the end of the Younger Dryas event. Nature 362: 527?529.

3. Ammann, B., 1989. Response times in bio- and isotope-stratigraphies to Late-Glacial climatic shifts ? an example from lake deposits. Ecologae geologica Helvetica 82: 183?190.

4. Ammann, B. & K. Tobolski, 1983. Vegetational development during the late-Würm at Lobsigensee (Swiss Plateau). Revue de Paléobiologie 2: 163?180.

5. Ammann, B. & A. F. Lotter, 1989. Late-Glacial radiocarbon- and palynostratigraphy on the Swiss Plateau. Boreas 18: 109?120.

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