Tree-ring-based methods are currently a frequently used tool for analyzing the spatial-temporal behavior of landslides, providing key data for predicting their future development or analyzing potential triggers. They use a spectrum of growth disturbances in tree-ring series to detect landslide events, one of the most common being abrupt growth suppression. Unlike other growth disturbances, however, this has not yet been studied in detail with regard to its frequency, intensity, or duration in different geomechanical zones of complex landslides. A deeper understanding of this issue would improve the efficiency of dendrogeomorphic sampling, as well as the overall spatial-temporal reconstruction of landslide movements. To obtain a more detailed insight, tree-ring series from 1322 disturbed individuals of Picea abies (L.) Karst. growing on 26 complex landslides with different geological structures were analyzed. The area of each landslide was divided into two contrasting zones with presumed different effects on tree growth (rotational slide zone and earthflow zone). The results showed that the highest incidence of abrupt growth suppression (both in absolute terms and per tree) was in the earthflow zone of landslides developed on rigid sandstone/conglomerate. Conversely, the highest intensity of abrupt growth suppression was found in the rotational slide zone on sandstone/conglomerate. Factors leading to this type of growth disturbance could possibly include root stretching in tension cracks or root shearing at the boundary of rock blocks in the rotational slide zone. In the case of the earthflow zone, root deformation and pinching during flow-like movement of weathered material may play a role. This effect is increased if pieces of rigid sandstone/conglomerate are present in the landslide material.
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