Journal of Tropical Ecology a Longterm Evaluation of Fruiting Phenology: Importance of Climate Change

Journal of Tropical Ecology http://journals.cambridge.org/TRO Additional services for Journal of Tropical Ecology: Email alerts: Click here Subscriptions: Click here Commercial reprints: Click here Terms of use : Click here A longterm evaluation of fruiting phenology: importance of climate change Colin A. Chapman, Lauren J. Chapman, Thomas T. Struhsaker, Amy E. Zanne, Connie J. Clark and John R. Poulsen Journal of Tropical Ecology / Volume 21 / Issue 01 / January 2005, pp 31 45 DOI: 10.1017/S0266467404001993, Published online: 10 January 2005 Link to this article: http://journals.cambridge.org/abstract_S0266467404001993 How to cite this article: Colin A. Chapman, Lauren J. Chapman, Thomas T. Struhsaker, Amy E. Zanne, Connie J. Clark and John R. Poulsen (2005). A longterm evaluation of fruiting phenology: importance of climate change. Journal of Tropical Ecology, 21, pp 3145 doi:10.1017/S0266467404001993 Request Permissions : Click here Downloaded from http://journals.cambridge.org/TRO, IP address: 128.164.247.189 on 09 Apr 2013 Journal of Tropical Ecology (2005) 21:31–45. Copyright © 2005 Cambridge University Press DOI: 10.1017/S0266467404001993 Printed in the United Kingdom A long-term evaluation of fruiting phenology: importance of climate change Colin A. Chapman∗†1, Lauren J. Chapman∗†, Thomas T. Struhsaker‡, Amy E. Zanne§, Connie J. Clark∗ and John R. Poulsen∗ ∗ Department of Zoology, University of Florida, Gainesville, Florida 32611, USA † Wildlife Conservation Society, 2300 Southern Boulevard, Bronx, New York 10460, USA ‡ Department of Biological Anthropology and Anatomy, Duke University, Durham, North Carolina 27708, USA § Department of Biology, Tufts University, Medford, Massachusetts, 02155, USA (Accepted 20 April 2004) Abstract: Within the last decade the study of phenology has taken on new importance because of its contribution to climate-change research. However, phenology data sets spanning many years are rare in the tropics, making it difficult to evaluate possible responses of tropical communities to climate change. Here we use two data sets (1970–1983 and 1990–2002) to describe the fruiting patterns of the tropical tree community in Kibale National Park, Uganda. To address variation in spatial patterns, we describe fruiting over 2–3 y among four sites each separated by 12–15 km. Presently, the Kibale region is receiving c. 300 mm more rain than it did at the start of the century, droughts are less frequent, the onset of the rainy season is earlier, and the average maximum monthly temperature is 3.5 ◦C hotter than it was 25 y ago. The 1990–2002 phenology data illustrated high temporal variability in the proportion of the populations fruiting. Interannual variation in community-wide fruit availability was also high; however, the proportion of trees that fruited has increased over the past 12+ y. At the species level a variety of patterns were exhibited; however, a number of the most common species currently rarely fruit, and when they do, typically < 4% of the individuals take part in fruiting events. Combining the data set from 1990 to 2002 with that from 1970 to 1983 for specific species again reveals an increase in the proportion of trees fruiting between 1990 and 2002; however, the proportion of the populations fruiting decreased during the earlier period. When one examines particular species over this whole period a variety of patterns are evident. For example, Pouteria altissima exhibited a relatively regular pattern of fruiting during the 1970s; however, it rarely fruited in the 1990s. Contrasting phenological patterns at four sites revealed that at the community level the fruiting patterns of only one of the six pair-wise site combinations were correlated. Relationships between rainfall and fruiting were variable among sites. Contrasting changes in fruiting patterns over the 30 y with differences among the four sites varying in rainfall, suggests that the changes observed in fruiting may be due to climate change. Responses to this climate change are likely complex and will vary among species. However, for some species, current conditions appear unsuitable for fruiting. Key Words: climate change, flowering, fruiting, Kibale National Park, phenology, seasonality, seed dispersal, tropical trees, Uganda INTRODUCTION van Schaik et al. 1993); mode of seed dispersal (Charles- Dominique et al. 1981, Smythe 1970, Wheelwright A variety of factors have been proposed to drive 1985); activity of pollinators or seed dispersers (Frankie phenological patterns of tropical rain forests. These et al. 1974, Rathke & Lacey 1985, Snow 1965); factors include: abiotic characters such as rainfall, day variation in germination conditions (Frankie et al. 1974, length, irradiance and temperature (Ashton et al. 1988, Janzen 1967); life history traits (Davies & Ashton 1999, Newbery et al. 1998, Opler et al. 1976, van Schaik 1986, Newstrom et al. 1994a); and relative abundance of the trees themselves (van Schaik et al. 1993). For example, itisthoughtthatfruitripeningmayoccuratatime whenconditionsfordispersalareoptimal.Wind-dispersed 1Corresponding author. Current address: Anthropology Department and McGill School of Environment, 855 Sherbrooke St West, seeds may ripen during the dry season when winds McGill University, Montreal, Quebec, Canada H3A 217. Email: are stronger and leaves are often absent, allowing for [email protected] greater dispersal distance (Newstrom et al. 1994a). In 32 COLIN A. CHAPMAN ET AL. contrast, peak fruiting periods for some animal-dispersed facilitating the evaluation of the effect of climate. For fleshy-fruited species occur during the rainy season, example, the disperser community (Chapman et al. 2000) perhaps as a result of increased moisture levels necessary and wind patterns are similar among years and sites. for fruit production (Lieberman 1982, Rathke & Lacey Having a spatially and temporally extensive data set 1985). Fruiting can be directly responsive to climatic allows us to verify whether patterns documented at one conditions (e.g. fleshy fruits are produced when the water site or at one time have general applicability. needed to produce them is abundant), or fruiting can be triggered by climatic changes which act as cues (Tutin & Fernandez 1993). METHODS Regardless of the mechanism driving fruiting, climatic patterns are likely to be critical in setting the timing of Study sites fruiting events. Given this dependence, and the current endangered status of tropical forests and the animals Kibale National Park (795 km2) is located in western dependent on them for fruit, current projections of climate Uganda (0 13–0 41N, 30 19–30 32E) near the foothills change are alarming. The earth’s climate has warmed by of the Ruwenzori Mountains (Chapman et al. 1997, approximately 0.6 ◦C over the past 100 y, with two main Skorupa 1988, Struhsaker 1975, 1997). The park periods of warming (1910–1945 and 1976–present), and consists of mature, mid-altitude, moist, semi-deciduous the 1990s are the warmest decade on record (Walther and evergreen forest (57%), grassland (15%), woodland et al. 2002). (4%), lakes and wetlands (2%), colonizing forest (19%) Within the last decade the scientific community and plantations of exotic trees (1%; Chapman & Lambert has begun to quantify ecological responses to recent 2000). Mean annual rainfall in the region is 1749 mm climate change and has realized that some communities (1990–2001, or 1547 mm from 1903–2001); mean experience marked changes with slight shifts in daily minimum temperature is 14.9 ◦C; and mean daily temperature or growing-season length (Spark & Menzel maximum temperature is 20.2 ◦C (1990–2001). There 2002, van Vliet & Schwartz 2002, Walther et al. 2002). are distinct wet and dry seasons that are bimodal in For example, the average first flowering date of 385 distribution. May–August and December–February tend British plant species has advanced by 4.5 d over the past to be drier than other months (Chapman et al. 1999a). decade compared with the previous four decades (Fitter & This study was conducted at four sites within Kibale. Fitter 2002). Such changes can modify the composition For the temporal study, two long-term phenological of communities. Stachowicz et al. (2002) demonstrated data sets come from Kanyawara; the site established by that increased ocean surface temperatures gave an intro- TTS in 1970. For the spatial study, to examine how duced sea squirt an earlier start after settlement than the consistent patterns were across space, and to evaluate native species and thus facilitated a shift in dominance whether environmental correlates shown to be predictive in a sessile marine invertebrate community. Potential at one site applied to others, we contrasted phenological impacts of global climate change, such as these, stress patterns at Kanyawara with three other sites that are the importance of understanding the determinants of each 12–15 km apart (Sebatoli, Dura River and Mainaro; phenological patterns to predict responses of specific com- Chapman et al. 1997). Within Kibale, there is a gradual munities to global climate change (van Vliet & Schwartz elevational gradient from north to south, which cor- 2002). Only with such an understanding can appropriate responds to a north to south increase in temperature, management practices be initiated to help preserve decrease in rainfall, and changes in forest composition vulnerable communities. While long-term phenological (Howard 1991, Struhsaker 1997; Table 1). Kibale re- records are available for some

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