Abstract

The alarming decline of amphibians around the world calls for complementary studies to better understand their responses to climate change. In mountain environments, water resources linked to snowmelt play a major role in allowing amphibians to complete tadpole metamorphosis. As snow cover duration has significantly decreased since the 1970s, amphibian populations could be strongly impacted by climate warming, and even more in high elevation sites where air temperatures are increasing at a higher rate than at low elevation. In this context, we investigated common frog (Rana temporaria) breeding phenology at two different elevations and explored the threats that this species faces in a climate change context. Our objectives were to understand how environmental variables influence the timing of breeding phenology of the common frog, and explore the threats that amphibians face in the context of climate change in mountain areas. To address these questions, we collected 11 years (2009–2019) of data on egg-spawning date, tadpole development stages, snowmelt date, air temperature, rainfall and drying up of wetland pools at ∼1,300 and ∼1,900 m a.s.l. in the French Alps. We found an advancement of the egg-spawning date and snowmelt date at low elevation but a delay at high elevations for both variables. Our results demonstrated a strong positive relationship between egg-spawning date and snowmelt date at both elevations. We also observed that the risk of frost exposure increased faster at high elevation as egg-spawning date advanced than at low elevation, and that drying up of wetland pools led to tadpole mortality at the high elevation site. Within the context of climate change, egg-spawning date is expected to happen earlier in the future and eggs and tadpoles of common frogs may face higher risk of frost exposure, while wetland drying may lead to higher larval mortality. However, population dynamics studies are needed to test these hypotheses and to assess impacts at the population level. Our results highlight climate-related threats to common frog populations in mountain environments, but additional research should be conducted to forecast how climate change may benefit or harm amphibian populations, and inform conservation and land management plans in the future.

Highlights

  • In mountain environments, species living at high elevation face strong constraints such as seasonal snow cover and low temperatures during the breeding season (Körner, 2007)

  • Growth, and reproduction of ectotherms such as amphibians are strongly influenced by environmental temperature, and given that water resources influenced by snowpack are essential for amphibians to complete metamorphosis, amphibian populations in mountain environments should be strongly impacted by climate warming, with pathways of impacts that may vary along elevation gradients

  • Over the 11-year period (2009–2019), year as a continuous variable was a significant predictor of egg-spawning date at high elevation, revealing an advancement of 1.4 days per year of the first spawning date at low elevation [β = −1.4, CI 95% (−3.1; 0.3), P = 0.10], and a delay of 1.7 days per year at high elevation [β = 1.7, CI 95% (0.3; 3.1), P = 0.02] (Figure 2B)

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Summary

Introduction

Species living at high elevation face strong constraints such as seasonal snow cover and low temperatures during the breeding season (Körner, 2007). Numerous studies have shown that climate change affects amphibian phenology at low elevation sites (Alford and Richards, 1999; Blaustein and Kiesecker, 2002; Beebee and Griffiths, 2005; Parmesan, 2006; Blaustein et al, 2010), but results indicate high heterogeneity in phenological responses across species and populations (Todd et al, 2010). In regard to temporal trends, Prodon et al (2019) emphasized non-linear phenological shifts over time related to the North Atlantic Oscillation (NAO) index, with earlier dates of Mediterranean amphibian breeding phenology in

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