Table 1 Explanatory variables used in this study and their hypothesised link to wood density

From: Variation in wood density across South American tropical forests

Variable

Potential effect on wood density

Source

Mean annual temperature (bio1)

Greater potential for drought stress at higher temperatures, so community-weighted mean wood density expected to increase with temperatures.

Worldclim V259

Mean annual precipitation (bio12)

Greater drought stress (and hence expectation for higher wood density) when precipitation lower.

Worldclim V259

Maximum cumulative water deficit (MCWD)

Higher wood density expected when moisture availability most limited.

Calculated using data from Worldclim V259 and TerraClimate.60

Mean wind speed in the windiest month

Proxy for potential for wind damage. High wind speeds could favour high wood-density species. Alternatively, frequent disturbances77 could favour low wood density pioneers.

Worldclim V263

Cloud frequency

Frequent cloud could reduce drought stress from evapotranspiration.

61

Lightning frequency

Potential to cause canopy gaps favouring pioneers.77 Trunk properties influence impacts of lightning strikes.78

TRIMM LIS Very High Resolution Gridded Climatology.79

Soil cation exchange capacity

A proxy for soil fertility (other metrics such as total exchangeable bases would be preferable but are not available in gridded form across the study area). More fertile soils are expected to favour faster life-history strategies, leading to lower average wood density.

SoilGrids62

Soil pH

Potential control on tree species distributions, with specialist communities in low or high pH environments.

SoilGrids62

Depth to rock

Shallower soils are potentially unstable, and frequent disturbances would be expected to favour pioneer species, which tend to have low wood density.

SoilGrids62

Soil texture

Relates to soil stability (more disturbances leads to more low wood density pioneers) and to soil moisture holding capacity.

SoilGrids62

Topography - rugosity

More disturbances likely on steeper slopes, which favours pioneers, which tend to have low wood density.

Calculated from SRTM V464

Topography - slope

More disturbances likely on steeper slopes, which favours pioneers, which tend to have low wood density.

Calculated from SRTM V464

Topography - HAND

Height above nearest drainage relates to soil drainage. Wood density may be lower in soils that retain moisture due to lower drought stress.

Donchyts et al.65

Spatial coordinates

Wood density is expected to vary independently of the environment due to biogeographic variation in species distributions. Additionally, spatial coordinates can capture variation in wood density caused by environmental factors not included in the analysis.