Abstract

Predicted warmer temperatures and more frequent extreme climatic events in the southern Andes may affect the dynamics of the Patagonian forests. These environmental changes may differentially alter the probability of Nothofagus pumilio establishment across its altitudinal range of distribution. We monitored fruit fall, seedling emergence and survival at altitudinal distribution range of N. pumilio forests in Santa Cruz (49°22′ S—72°56′ W), Argentina. Fruit fall, seedling emergence and survival were tested in relation to drought, based on the SPEI (Standardized Precipitation Evapotranspiration Index), interacting with elevation. Fruit fall was consistently higher at low elevation and the abundance of fruits was not affected by drought intensity. Density of new-born seedlings was ~ 9 to 24 times lower at low- than at high-elevation plots in our first observations (2014 and 2016), characterized by warm-dry climatic conditions in spring-early summers. In contrast, seedling abundance was ~ 1.5 times larger at low elevations during relatively cold-wet growing seasons. Survival probability was explained by the interaction between SPEI and elevation. At low elevation and in dry periods, survival probability was lower (CI 54–72%) than in wet periods (CI 68–84%) but at high elevation similar survival was registered even with positive or negative SPEI values. Our results show interacting effects of elevation and drought on tree establishment at the elevation limits, with positive and negative drought effects at high and low elevations, respectively. Predicted increase of extreme drought events during the XXI century could be detrimental for N. pumilio establishment at dry, low-elevation forests.

Highlights

  • Understanding the consequences of climate change on mountains forests requires a comprehensive view of tree life stages and species-specific processes along their ranges of distribution

  • Seedling emergence was explained by elevation interacting with Standardized Precipitation Evapotranspiration Index (SPEI), reflecting the importance of water deficit in spring-summer during the previous year for regeneration

  • Under spring-summer seedling emergence was larger at the upper forest during but on the wet cold period abundance of emerged seedlings was similar at both elevation boundaries (Fig. 4)

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Summary

Introduction

Understanding the consequences of climate change on mountains forests requires a comprehensive view of tree life stages and species-specific processes along their ranges of distribution. The consequences of climate warming on plant vital rates are expected to differ spatially for tree species with wide elevation ranges. Empirical knowledge on the performance of montane at elevation boundaries could help us to understand plant responses to climate changes before the potential expansion or contraction of their range occurs (Harsch et al 2009, Harsch and Bader 2011, Cagnacci et al 2020). Seedling emergence and survival are the stages in the trees’ life cycle most vulnerable to climatic change (Hampe and Petit 2005, Engelbrecht 2007, Tercero Bucardo et al 2007, Peter et al 1996, Grubb 1977)

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