Using herbarium specimens to select indicator species for climate change monitoring

2018 ◽  
Vol 27 (6) ◽  
pp. 1487-1501 ◽  
Author(s):  
Rebecca A. Hufft ◽  
Michelle E. DePrenger-Levin ◽  
Richard A. Levy ◽  
Melissa B. Islam
2012 ◽  
Vol 99 (4) ◽  
pp. 751-756 ◽  
Author(s):  
Zoe A. Panchen ◽  
Richard B. Primack ◽  
Tomasz Aniśko ◽  
Robert E. Lyons

2017 ◽  
Vol 215 (1) ◽  
pp. 479-488 ◽  
Author(s):  
Charles G. Willis ◽  
Edith Law ◽  
Alex C. Williams ◽  
Brian F. Franzone ◽  
Rebecca Bernardos ◽  
...  

2017 ◽  
Author(s):  
Casey A Jones ◽  
Curtis C Daehler

Studies in plant phenology have provided some of the best evidence for large-scale responses to recent climate change. Over the last decade, more than thirty studies have used herbarium specimens to analyze changes in flowering phenology over time. In this review, we summarize the approaches and applications used to date. Reproductive plant phenology has primarily been analyzed using two summary statistics, the mean flowering day of year and first flowering day of year, but mean flowering day has proven to be a more robust statistic. Three types of regression models have been applied to test for changes in phenology; flowering day regressed on year, flowering day regressed on temperature, and temperature regressed on year. Most studies analyzed the effect of temperature by averaging temperatures from three months prior to the date of flowering, but other approaches may be suitable in some cases. On average, published studies have used 55 herbarium specimens per species to characterize changes in phenology over time, but in many cases fewer specimens were used. Geospatial grid data is increasingly being used for determining average temperatures at herbarium specimen collection locations, allowing testing for finer scale correspondence between phenology and climate. Multiple studies have shown that inferences from herbarium specimen data are comparable to findings from systematically collected field observations. Herbarium specimens are expected to become an increasingly important resource for analyzing plant responses to climate change. As temperatures continue to rise globally, there is a need to understand phenological rates of change in response to warming and implications of these changes, especially in tropical environments where phenological studies are thus far generally lacking.


2012 ◽  
Vol 8 (5) ◽  
pp. 882-886 ◽  
Author(s):  
Greg R. Guerin ◽  
Haixia Wen ◽  
Andrew J. Lowe

Climate change is driving adaptive shifts within species, but research on plants has been focused on phenology. Leaf morphology has demonstrated links with climate and varies within species along climate gradients. We predicted that, given within-species variation along a climate gradient, a morphological shift should have occurred over time due to climate change. We tested this prediction, taking advantage of latitudinal and altitudinal variations within the Adelaide Geosyncline region, South Australia, historical herbarium specimens ( n = 255) and field sampling ( n = 274). Leaf width in the study taxon, Dodonaea viscosa subsp. angustissima , was negatively correlated with latitude regionally, and leaf area was negatively correlated with altitude locally. Analysis of herbarium specimens revealed a 2 mm decrease in leaf width (total range 1–9 mm) over 127 years across the region. The results are consistent with a morphological response to contemporary climate change. We conclude that leaf width is linked to maximum temperature regionally (latitude gradient) and leaf area to minimum temperature locally (altitude gradient). These data indicate a morphological shift consistent with a direct response to climate change and could inform provenance selection for restoration with further investigation of the genetic basis and adaptive significance of observed variation.


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