Abstract

The temporal variation in lake's phytoplankton is important to understand its general biodiversity. For tropical lakes, it has been hypothesized that they follow a similar pattern as temperate ones, on a much accelerated pace; nevertheless, few case studies have tried to elucidate this. Most studies in Costa Rica have used a monthly sampling scheme and failed in showing the expected changes. In this study, the phytoplankton of the small Barvas's crater lake was followed for more than three years, first with monthly and later with weekly samplings, that covered almost two years. Additional information on temperature and oxygen vertical profiles was obtained on a monthly basis, and surface temperature was measured during weekly samplings around noon. Results showed that in spite of its shallow condition (max. depth: 7m) and low surface temperature (11 to 19 degrees C), the lake stratifies at least for brief periods. The phytoplankton showed both, rapid change periods, and prolonged ones of relative stasis. The plankton composition fluctuated between three main phases, one characterized by the abundance of small sized desmids (Staurastrum paradoxum, Cosmarium asphaerosporum), a second phase dominated by equally small cryptomonads (Chryptochrysis minor, Chroomonas sp.) and a third phase dominated by the green alga Eutetramorus tetrasporus. Although data evidenced that monthly sampling could miss short term events, the temporal variation did not follow the typical dry and rainy seasons of the region, or any particular annual pattern. Year to year variation was high. As this small lake is located at the summit of Barva Volcano and receives the influence from both the Caribbean and the Pacific weather, seasonality at the lake is not clearly defined as in the rest of the country and short term variations in the local weather might have a stronger effect than broad seasonal trends. The occurrence of this short term changes in the phytoplankton of small tropical lakes in response to weather variations needs to be further explored in other lakes.

Highlights

  • Temporal variation of phytoplankton is one of the factors that explain the diversity of species of the plankton (Padisak 2003, Reynolds 2006), which was once considered as a paradox of theoretical ecology (Hutchinson 1961)

  • Lewis (1978) proposed that tropical lake phytoplankton follows the same basic sequence that occurs in temperate lakes: it starts with a community dominated by diatoms and Cryptophyta during the turn-over event which is the time of nutrient enrichment

  • Frequent circulation could be the main reason why changes in the plankton community in Costa Rican lakes do not seem to follow the pattern predicted by Lewis (1978)

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Summary

Introduction

Temporal variation of phytoplankton is one of the factors that explain the diversity of species of the plankton (Padisak 2003, Reynolds 2006), which was once considered as a paradox of theoretical ecology (Hutchinson 1961). Much smaller tropical lakes do not usually stratify in such a predictable and relatively long lasting pattern Their circulation is more dependent on weather conditions which vary more frequently, as has been noted by Lewis himself (Lewis 1996). Frequent circulation could be the main reason why changes in the plankton community in Costa Rican lakes do not seem to follow the pattern predicted by Lewis (1978). Research on plankton in Costa Rican lakes has been based generally on monthly or quarterly sampling designs (Camacho & Charpentier 1989, Umaña & Collado 1990, Umaña 1993,1997) This has always left in doubts whether these low frequency samplings are really ignoring valuable information about temporal changes in phytoplankton. The main objective of the present work is to record the changes in the water column condition and the plankton community in a small tropical crater lake, and test whether short term changes in the phytoplankton follow the predicted pattern as proposed by Lewis (1978)

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