The influence of climate on peatland extent in Western Siberia since the Last Glacial Maximum

por Alexandrov, G. A., Brovkin, V. A., Kleinen, T.
Publicado 2016

Mid-Pleistocene transition in glacial cycles explained by declining CO(2) and regolith removal

por Willeit, M., Ganopolski, A., Calov, R., Brovkin, V.
Publicado 2019

Subsea permafrost organic carbon stocks are large and of dominantly low reactivity

por Miesner, F., Overduin, P. P., Grosse, G., Strauss, J., Langer, M., Westermann, S., Schneider von Deimling, T., Brovkin, V., Arndt, S.
Publicado 2023