Can subfossil insects complement pedoanthracology in reconstructing the past trajectories of old-growth forests? A study case from the Northern Central Pyrenees (France)

Abstract

The presence of insect remains preserved in soils has the potential to serve as a complementary proxy to charcoal, facilitating the reconstruction of Holocene forest trajectories at high spatial resolution. Six pits were dug at three old-growth forest sites (two per site) in the Central Pyrenees (France). Insect remains and charcoal were collected in each soil layer, following the pedoanthracological method usually conducted in similar mountain contexts. Radiocarbon dating was performed on a selection of both insects and charcoal, and a time-since-death index was developed to evaluate the degradation stage and relative age of the insect remains. Insect remains were present in most layers, but were more abundant in the upper ones, as with charcoal. Whereas radiocarbon dating did not work on individual insect remains, the time-since-death index showed a consistent relationship between increasing degradation and increasing depth. Saproxylic beetles, which are key indicators of the maturity of old-growth forests, were poorly preserved in the soils studied, but some of the other beetles identified at genus or species level provided useful information on past forest openness.