Data from: Underlying geology and climate interactively shape climate change refugia in mountain streams
Data files
Dec 15, 2022 version files 81.54 KB
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Dataset_Ishiyama_etal_220506.xlsx
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README_datset_Ishiyama_etal_220506.docx
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Abstract
Identifying climate-change refugia is a key adaptation strategy for reducing global warming impacts. Knowledge of the effects of underlying geology on thermal regime along climate gradients and the ecological responses to the geology-controlled thermal regime is essential to plan appropriate climate adaptation strategies. In the present study, the dominance of volcanic rocks in the watershed is used as a landscape-scale surrogate for cold groundwater inputs to clarify the importance of underlying geology in stream ecosystems along climate gradients. First, using hundreds of monitoring stations distributed across multiple catchments, we explored the relationship between watershed geology and the mean summer water temperature of mountain streams along climate gradients in the Japanese archipelago. Mean summer water temperature was explained by the interaction between the watershed geology and climate in addition to independent effects. The cooling effect supported by volcanic rocks reached up to 3.3°C among study regions, which was more pronounced in streams with less summer precipitation or lower air temperatures. Next, we examined the function of volcanic streams as cold refugia under contemporary and future climatic conditions. Community composition analyses revealed that volcanic streams hosted distinct stream communities composed of more cold-water species compared with non-volcanic streams. Scenario analyses based on multiple GCMs and RCPs revealed a geology-related pattern of thermal habitat loss for cold-water species. Non-volcanic streams rapidly declined in thermally suitable habitats for lotic sculpins even under the lowest emission scenario (RCP 2.6). In contrast, most volcanic streams will be sustained below the thermal threshold, especially for low and mid-level emission scenarios (RCP 2.6, 4.5). However, the distinct stream community in volcanic streams and geology-dependent habitat loss for lotic sculpins was not uniform and was more pronounced in streams with less summer precipitation or lower air temperatures. These findings highlight that underlying geology, climate variability, and their interaction should be considered simultaneously for effective management of climate-change refugia in mountain streams.
Definitions of the variable headings
Variable | Explanation |
Site | Monitoring site |
Region | Monitoring region |
Basin | Monitoring basin |
Year | Monitoring year of water temperature |
WT_℃ | Mean summer water temperature (℃) |
Volcanic_% | Volcanic rocks in the watershed (%) |
Agri_% | Agricultural lands in the watershed (%) |
CA_km2 | Drainage area (km2) |
Slope_% | Stream slope (%) |
Elev_m | Site elevation (m) |
AT_℃ | Mean summer air temperature (℃) |
Pricipi_mm | Total summer precipitation (mm) |
Depth_cm | Mean water depth (cm) |
Velocity_cm/s | Mean current velocity (cm/s) |
Substrate | Substrate coarseness |
DO_mg/l | Dissolved oxygen (mg/l) |
NO3-_mg/l | NO3− (mg/l) |
*Other columns' names indicate species names (e.g., Potamanthus.formosus).