| Literature DB >> 30937217 |
Abstract
PREMISE OF THE STUDY: A novel method of estimating phenology of herbarium specimens was developed to facilitate more precise determination of plant phenological responses to explanatory variables (e.g., climate). METHODS ANDEntities:
Keywords: climate change; digitization; herbarium specimens; phenology
Year: 2019 PMID: 30937217 PMCID: PMC6426155 DOI: 10.1002/aps3.1224
Source DB: PubMed Journal: Appl Plant Sci ISSN: 2168-0450 Impact factor: 1.936
Figure 1Graphical representation of how the binary (A), ≥50% (B), and estimated phenophase (C) methods estimate the relationship between the timing of a phenological event and an explanatory variable. The binary method (A) uses the collection date of all specimens in any phase within the longer phenological event (e.g., at least one flower present). Thus, the span of time within which the collection date can occur is potentially as long as the flowering season. When compounded, these imprecise phenological approximations can lead to erroneous estimates of the relationship between phenology and the explanatory variable or even preclude discovery of the relationship. Similarly, the range of possible dates for the ≥50% method (B) may be wide if the duration of peak flowering is long, and estimates of phenological relationships may be accordingly imprecise. In contrast, the estimated phenophase method (C) can theoretically provide a more precise estimate of the phenological relationship by enabling comparison of a specific point within the phenological event among values of the explanatory variable.
Default values for simulated specimen data sets. These values were chosen for their similarity to real‐world values calculated in a study of asteraceous species in the southeastern United States (Pearson, 2019)
| Parameter | Default value |
|---|---|
| Slope (i.e., relationship between phenology and explanatory variable) | 3.0 |
| Intercept mean | 268 |
| Intercept SD | 15 |
| Number of species ( | 50 |
| Specimens per species | 100 |
| Flowering season duration mean | 80 |
| Flowering season duration SD | 10 |
| Individual flowering duration mean | 20 |
| Individual flowering duration SD | 3 |
| Species slope (phenology/climate relationship) mean | 3 |
| Species slope (phenology/climate relationship) SD | 1 |
SD = standard deviation.
The slope and intercept values are arbitrary; changing their values did not affect subsequent results.
Figure 2Width of 95% confidence intervals (CIs) of slope (days/unit climate) estimated using the ≥50% (white triangles), binary (black squares), and estimated phenophase (gray circles) methods of specimen inclusion with changes in key simulation parameters. For simplicity, results from linear mixed effects (LME) models in which only species intercepts were allowed to vary are shown; variable intercept + slope model results are provided in Appendix S3. Each point represents the mean value of 100 iterations of the simulation. Standard errors of the mean (listed in Appendix S2) were very small and are not included in this figure for clarity. (A) The length of the individual flowering duration was changed between simulations. (B) The number of specimens per species was varied while keeping all other variables, including number of species, constant. (C) 95% CI widths are shown with increasing flowering season durations of species. Unless otherwise specified, default simulation parameters were as described in Table 1.