Physical factors contributing to the benthic dominance of the alga Caulerpa sertularioides (Caulerpaceae, Chlorophyta) in the upwelling Bahía Culebra, north Pacific of Costa Rica


Cindy Fernández-García¹*,²*,³*, Jorge Cortés¹,², Juan José Alvarado¹,³  & Jaime Nivia-Ruiz¹

*^{Dirección para correspondencia}
Abstract

Caulerpa sertularioides has been spreading in Bahía Culebra, a seasonal upwelling bay in the north Pacific of Costa Rica, since 2001. The survey was carried out from December 2003 to March 2005, in several locations around Bahía Culebra, located inside the Gulf of Papagayo. This study investigated spatial and temporal patterns, percent coverage, monthly growth rate, reproductive adaptations, and morphological variations of frond length and stolon diameter of Caulerpa sertularioides, at different environmental physical and chemical factors at the bay. The alga extended to depths of 23 m on a variety of substrates. The stolons extended quickly, with a maximum growth rate of 31.2 cm month^-1. This alga grows mainly by fragmentation of its fronds and stolons; nevertheless it can also reproduce sexually by releasing gametes in the water column. These two modes of spreading promote the adaptation of this opportunistic  species to environmental, chemical, and physical changes at this bay. At the same time the alga showed variations in the length of its fronds and stolons, adapting to conditions such as depth and season. Average percent cover and frond density increased during the dry season when the upwelling of nutrients and cold water occurs. In the rainy season the average percent cover and frond density decreased; however there was a peak in September, when high precipitation resulted in runoff into the bay of nutrient-rich waters. The morphological and physiological plasticity of C. sertularioides, in synergy with its predominant clonal propagation and sexual reproduction provided this species with a great adaptability to changes in temperature and nutrient concentration at Bahía Culebra.

Key words: Caulerpa sertularioides, Bryopsidales, Central America, growth rates, nutrients, seasonal upwelling.

Resumen

Desde el 2001 se ha observado una propagación del alga verdeCaulerpa sertularioidesen Bahía Culebra, zona de afloramiento costero, en el Pacífico norte de Costa Rica. El muestreo se llevó acabo entre Diciembre 2003 a marzo 2005, en varias localidades de Bahía Culebra. En este estudio se presentan los patrones de distribución, cobertura, tasa mensual de crecimiento, adaptaciones reproductivas y variaciones morfológicas del largo de la fronda y diámetro del estolón deCaulerpa sertularioides, a diferentes factores ambientales físico-químicos en Bahía Culebra. Esta alga se extiende hasta profundidades de 23 m, en una gran variedad de sustratos. Los estolones se extienden rápidamente, con un crecimiento máximo de 31.2 cm mes^-1. Esta alga se propaga principalmente por la fragmentación de sus frondas y estolones, así mismo se reproduce sexualmente liberando gametos a la columna de agua. Estos modos de reproducción promueven la adaptación de esta especie oportunista, a los cambios ambientales, tanto químicos, como físicos, de la bahía. Al mismo tiempo esta alga presenta variaciones en el largo de sus frondas y el diámetro del rizoma, adaptándose a diferentes profundidades y condiciones de la época del año. El porcentaje de cobertura y densidad de frondas aumentan durante la época seca, cuando emergen aguas frías y nutrientes por el afloramiento costero. Por otro lado, en la época lluviosa estas medidas decrecen, sin embargo se presenta un pico en setiembre, cuando la precipitación aumenta y llega una carga extra de nutrientes a la bahía por escorrentía. La plasticidad morfológica y fisiológica deC. sertularioides, en sinergia con su propagación clonal, proveen a esta alga con una gran adaptabilidad a los cambios en temperatura y nutrientes de Bahía Culebra.

Palabras clave: Caulerpa sertularioides, afloramiento costero, América Central, Bryopsidales, nutrientes, tasa de crecimiento.
The genus Caulerpa has 86 current accepted species (Guiry & Guiry 2011) distributed throughout the world oceans, and in Central America 8 species have been reported (Fernández-Garcíaet al. 2011). It is a common inhabitant of intertidal and subtidal tropical and semitropical marine waters. These algae have a creeping green stolon with root-like colorless rhizoids and erect uprights called fronds (Lee 2008). Propagation of Caulerpa is mainly clonal, and its phenotypic plasticity provides an opportunity to adapt to different changes in physical environments (Sernerpontet al. 2003). Most species in the genus have been studied, mainly due to its invasive capacity and the consequent economical impact on coastal communities (Knowlton 2000, Westet al. 2009).

The species Caulerpa sertularioides(S.G. Gmelin) Howe, 1905, is characterized by feather-like fronds, sometimes branched, with cylindrical and needle shaped branchlets 20 cm length and 1-2 cm wide (Howe 1905). This species is distributed within tropical and subtropical waters and is most commonly observed forming patches in benthic sandy habitats and growing within the seagrasses to a depth of 10 m (Schnetter & Bula-Meyer 1982, Littler &Littler 2000). Despite its broad distribution, studies on this species are scarce in comparison with otherCaulerpaspecies (Scrosati 2001).

In the Eastern Tropical Pacific (ETP),Caulerpa sertularioidesis distributed from the Gulf of California, Mexico (Dawson 1944) to a reported southern limit of Gorgona Island, Colombia (Schnetter & Bula-Meyer 1982). It has been reported for Mexico (Taylor 1945, Scrosati 2001), Nicaragua (Dawson 1962), Costa Rica (Fernández & Cortés 2005), Panama (Wysor 2004, Smithet al. 2010) and Colombia (Schnetter & Bula-Meyer 1982).

In the Pacific coast of Costa Rica, at Bahía Culebra, a coastal upwelling zone, this green alga has been spreading around the bay since 2001 (Fernández & Cortés 2005). As a result,C. sertularioideshas become dominant with the subsequent replacement of native algae species and overgrowth on coral colonies. This has caused changes on the local diversity and abundance of benthic flora and fauna (Fernández & Cortés 2005). In other regions of the Eastern Pacific,C. sertularioideshas exhibited similar bloom patterns, some of them ephemeral such in Panama (Glynn & Maté 1997) and Gulf of California (Scrosati 2001), while in Costa Rica and other localities of Panama (Fernández & Cortés 2005, Smithet al. 2010) the alga has maintained high densities over several years.

Under specific conditionsCaulerpaspecies can easily spread and cover high percentages of the substrate (Withgott 2002). Is well-known, that the spreading of some species ofCaulerpais triggered by changes in environmental conditions such as: water temperature, an increase in nutrient concentrations and light intensity (Raven & Geider 1988, Bell 1992, Lapointe 1997, Scrosati 2001, Maltaet al. 2005). Furthermore, this factors, combined with water motion and depth, can induce variations in the morphology, which is an advantage in adapting to different environments (Ohbaet al.1992, Collado-vides & Robledo 1999, De Senerpont Domiset al.2003, Malta et al. 2005).

In addition the spreading ofCaulerpaspecies is favored by intrinsic characteristics of this genus, such as toxins to avoid herbivory, morphological and physiological plasticity, asexual reproduction by fragmentation (Grahamet al.2009), rapid nutrient uptake, rapid lateral growth of stolons and fragments, and associations with unpalatable species (Tyleret al.2010).

In the Gulf of California, Scrosati (2001) found that water temperature is one of the most important abiotic factors that affect growth rates ofC. sertularioides. However there are few studies to date on other factors favoring the spreading of this species and how these factors influence the morphology of this species. This is why the objectives of the present study were to describe the spreading of this alga in an upwelling region and to determine those factors that influence the spreading ofC. sertularioides, by analyzing the spatial and temporal coverage, density and growth rates patterns. Also to determine, if there are morphological adaptations, of fronds and stolons, in relation to environmental conditions.

Materials and methods

Study site:The survey was carried out in Bahía Culebra (10º35’N-85º40’W), located in the Gulf of Papagayo, north Pacific coast of Costa Rica, from December 2003 to March 2005. This bay extends from Islas Huevos to Islas Pelonas, including the inner part of the bay, Puerto Culebra and the Iguanita mangrove (Jiménez 2001) (Fig. 1). The Gulf of Papagayo is highly influenced by trade winds that move southward during the dry season (December to April). These winds displace surface waters away from the coast. This results in the upwelling of cold and nutrient rich water (Breneset al. 1995, Jiménez & Cortés 2003). During the dry season, when upwelling occurs, the mean water temperature is 22.9 + 0.3ºC, while during the wet, non-upwelling season (May-November) the temperature rises to a mean of 27.0 + 0.1ºC (Jiménez & Cortés 2003).



Environmental conditions:The following environmental factors were measured monthly at five sites: Islas Huevos, Playa Blanca, Punta Flor, La Penca and Isla Pelonas (Fig. 1): Salinity (‰), using a manual refractometer (ATAGO, model S/Mill-E). Temperature (ºC), measured at 30 min intervals with in situ continuous logging sensors (Stow Away XTI) located at each site, converted to monthly mean averages for the analysis. As an indirect measurement of primary productivity, we measured the concentration of chlorophyll a (μg l^-1) according to Lorenzen and Jeffrey (1978). Also we calcu-lated the concentration of suspended sediments (mg l^-1), collected with a 3.8 l bottle, filtered with fiberglass filters (Whatman GF/C) that were dried and weighted, and sedimentation rate (mg cm^-2 day^-1) measured with three sedi-ment traps at each sampling site, following the methodology of Cintrónet al. (1994) and Rog erset al. (1994). These two last factors were measured as an indirect measurement of runoff.

Nutrients were analyzed from water samples collected with a Niskin bottle at 15 m deep, at five sites in the bay (Fig. 1). Each sample was transferred to 1 L dark bottles, which were placed in a cooler with ice. We estimated the concentration (µM) of: phosphate (PO₄^-3), nitrite (NO₂^-),  nitrate  (NO₃^-), ammonium (NH4+) and silicate (SiO₄). These nutrients were measured following Strickland & Parsons (1972) and the protocol of the Chemical Oceanography Laboratory of the Centro de Investigación en Ciencias del Mar y Limnología (CIMAR).

To determine climatic changes, precipitation (mm), solar intensity (sun hours day^-1) and wind velocity (km h^-1) data were obtained from the National Meteorological Institute of Costa Rica, at the Daniel Oduber Quirós International Airport Station (10º35’ N-85º32’ W, 80 m above sea level); the closest station to Bahía Culebra.

To determine the most important marine environmental factors influencing Bahía Culebra, we applied a principal component analysis (PCA) based on a correlation matrix (Clarke & Warwick 1994) using the mean value per month of each environmental variable. Once we determined the most important environmental factors, graphed the average per month and we applied a Kruskal-Wallis non parametric analysis to determinate whether or not these factors vary between the dry and wet season. All the statistical analyses were performed using the software Systat 8.0 and JMP IN 4.0.4.

Ecology and morphology of Caulerpasertularioides:With a manta tow method (Rogerset al. 1994), we identified the mainC. sertularioidespatches in Bahía Culebra. At each site we recorded the maximum and minimum depth where the alga was growing.

In order to determine morphological variations of the fronds and stolons ofC. sertularioidesat different depths and seasons, we collected thalli of the green alga, in March 2004 (dry season) and in October 2004 (rainy season), at three depths and from three different sites as replicates: 2 m (Playa La Penca, Islas Huevos and Punta Flor), 5 m (Playa La Penca and Playa Blanca) and 10 m (Playa La Penca, Islas Huevos and Islas Pelonas). According to Meineszet  al. 1995, Dumayet al. 2002 and De Senerpont Domiset al. (2003), who found that fronds and stolons vary with physical conditions, we chose frond length and stolon diameter as morphological measurements. Therefore, we randomly chose 50 fronds and 50 stolons from each sample. We photographed each section of the thallus and digitized frond length and stolon diameter (UTHSCSA software Image Tool version 3.0). For each parameter, we took 3-5 measurements and we calculated an average per thallus. To determine if morphological characteristics varied between depths, we applied an analysis of variance (ANOvA) and an a posteriori test (Tukey), for each factor. Frond length data were log₁₀(x+1) transformed, while stolon diameter data fit a normal distribution.

Growth rate: Growth rate of C. sertularioideswas estimated from stolon growth rates per month.In situmeasurements of re-growth stolon length at three sites in the bay (Islas Huevos, Playa Blanca and Playa La Penca:Fig. 1) were collected at approximately 4 m deep. At each site, we removed all the thali from five permanent 50 cm²quadrats, marked with construction rods, located over a patch of C. sertularioides. After a month, we measured all the re-growth stolons inside the fixed quadrat using a caliper (±0.05 mm). Plots were cleared at the end of November 2003, February 2004 and August 2004 and were allowed to re-grow until the end of December 2003, March 2004, and September 2004. Finally, we applied an ANOvA and a posteriori Tukey test to determine differences between growth rates, at each month. The stolon length data were log₁₀(x+1) transformed.

Temporal algal percent coverage and frond density:Between March 2004 and March 2005 we measured the frond density and percent coverage of C. sertularioides monthly, at three sites in the bay: Islas Huevos, Playa Blanca and Playa La Penca (Fig. 1). At each site we calculated the percent coverage, as a visual estimation of how much substrate fronds and stolons cover the substrate, from five 50 x 50 cm²quadrats permanently located over a C. sertularioides patch. From these quadrats we choose six 10 cm2 subquadrats where we counted the fronds. Finally, to determine coverage and frond density differences between sites and seasons we applied an ANOvA. Data were tested for assumptions of normality and homogeneity and were transformed with Box-Cox.

Results

Environmental  factors:Bahía Culebra has high local seasonality, primarily related to precipitation, number of solar hours, and wind velocity (Table 1). The rainy season begins in May and ends in October, the rainiest months of this season are September and October. The dry season extends from December to April. Relative to the rainy season, the dry season had 212 mm less precipitation, an average of three more hours of sun light and an increase of 8.8 km h-1 in wind velocity (Table 1).

According to the Principal Component Analysis (PCA), five main environmental factors explained 65.2% of the variance of the environmental conditions in Bahía Culebra from March 2004 to March 2005. Nitrate, phosphate and suspended sediments (PC1) contributed 26.7% of the variance, while sedimentation rate contributed 22.5% (PC2) and temperature contributed 16.0% (PC3) (Fig. 2). Of these factors, only the mean temperature was significantly different between seasons (F_1,11= 12.099, P < 0.005).

Water temperature exhibited high season-ality, showing decreased temperatures in the dry season, when the wind velocity increased, producing a displacement of the thermocline to the surface and coastal upwelling (Table 1, Fig. 3A). The lowest temperature was recorded in  March  2004  (22.9°C,  dry  season),  while the highest was recorded in September 2004 (29.6°C, wet season). Salinity was higher during the dry season (34.3‰) and lowest (30.0‰) during the rainy season (Table 1). The highest chlorophyll  a  concentration  (3.8  µg l-1)  was recorded in October (wet season) (Table 1). Suspended sediments showed similar fluctuation patterns to precipitation during the wet season, when streams and rains carry sediments and nutrients into the sea (Table 1, Fig. 3A). Sedimentation rates were less variable than suspended sediments (Table 1, Fig. 3A).

Nutrient concentration differed between seasons. Average phosphate, nitrate and ammonium were higher in the dry season, while average silicate and nitrite were higher during the wet season (Table 1). However, nutrient concentrations were highly variable within seasons. phosphate increased in December 2004 (PO₄^-3=1.45) and September (PO₄^-3=0.69 µM), while  nitrate  was  higher  in  December  2004 (NO₃^-1=15.6 µM) (Fig. 3B)

Ecology and morphology of Caulerpa sertularioides: We found C. sertularioides ranged in Bahía Culebra from the intertidal zone to 23 m deep. It was present on different substrates (rocks, sand, and live and dead corals) forming patches that can cover 6 ha. The greatest coverage (~90%) was observed in sites between 3 to 6 m deep, where we found 108 fronds 10 cm^-2. However, at depths >12 m, the coverage and frond density decreased, and only isolated stolons were observed.

We also observed some algal patches simultaneously releasing gametes (Fig. 4A) at Punta Flor at 07:40 a.m., on January 3^rd2005 (Fig. 1). After gamete releases finished, all stolons and fronds turned white (Fig. 4B). This signal was later used to recognize other spawning events. Thus, most spawning events were observed in months when water temperature changes occured (February 2004, January 2005) and rain intensity was high (October 2004).

Caulerpa sertularioides showed different frond lengths at different depths (Fig. 5). The average stolon diameter of all the thalli measured was 0.18 mm (Min=0.04 mm, Max= 0.34 mm), while frond length average was 5.3 cm (Min=0.79 cm, Max= 15.9 cm). Stolon diameter was larger at 5 m than 2 m depth (F_2,1055 = 9.5, P < 0.000), while fronds were significantly longer at greater depths (F_2,985  = 116.8, P <0.000) (Fig. 5).

Growth rate: Mean stolon growth rate was 11.7 ± 6.2 cm month^-1, minimum in December 2004 (1.4 cm month-1) and maximum in September 2004 (33.2 cm month^-1, Fig. 5). Significant differences were found between   the   stolon   growth   rates   during the  three  sampling  months  (F_2,144  =  5.797 p<0.004), mainly between March and September 2004 (Fig. 6).

Temporal algal percent coverage and frond density: Average percent coverage and frond density had similar dynamic patterns throughout the sampling time (Fig. 7). During the wet season the values of cover percentage tended to be <40%, however in September 2004 we documented a peak of 46.3%, while the frond density during those months was <29.5 fronds 10 cm-2. After November bothparameters  increase  continuously  until  they reach the maximum values at February 2005, 70.7% cover and 50 fronds 10 cm^-2, dropping in March to less than 20% of cover and 20 fronds 10 cm^-2 (Fig. 7).

The  average  percent  cover  (F_5,183=7.9, p<0.0001)  and  frond  densities  (F_5,183=13.5, p<0.0001) were statistically different between seasons (Fig. 8), being higher during the dry season (Fig. 8A and ^8B Fig. 8 Fig. 8A 8B Fig. 8A Fig. 8B ). Also we found differences in coverage (F_5,183=12.1, p=0.02) and frond density (F_5,183=20.5, p<0.03) values, between sites. Playa Blanca exhibited the highest percent coverage and frond density values while Isla Huevos showed the lowest values (Fig. 8A). When comparing seasons, we found higher during the dry season (Fig. 8B).

Discussion

Caulerpa  sertularioides  is  a  native  alga from the Pacific coast of Costa Rica, but since 2001 its abundance and growth rate have increased, colonizing a wide range of substrates and depths at Bahía Culebra (Fig. 9). In fact, we documented the greatest depth (23 m) reported for the species. In the Pacific coast of Panama, C. sertularioides grows from the intertidal zone to 16 m (Wysor 2004), while in Colombia, it grows to 1 m deep (Schnetter & Bula-Meyer 1982). In the Caribbean and Central  Pacific,  C.  sertularioides  grows  in reef habitats to a depth of 10 m (Littler & Littler 2000, 2003). However, C. sertularioides has not been found as deep as other Caulerpa species, such as C. taxifolia in the Mediterranean that grows from 0-30 m deep, with highest densities between 5-15 m (Belsher & Meinesz 1995). C. sertularioides at Bahía Culebra grew faster (1.1 cm day^-1) than some other Caulerpa species. For example, Williams et al. (1985) reported that C. mexicana grew 1.0 cm day^-1, while C. cupressoides 0.8 cm day^-1, and C. prolifera 0.4 cm day-1. But slower than other Caulerpa species, such as C. taxifolia (8 cm day^-1) and C. racemosa (2 cm^-1day^-1) (Dalton 2000), the first being one of the most invasive species of the genus.



We often observed floatingC. sertularioidesfronds and stolons during the study period, which suggest that local spreading is mainly driven by fragmentation of the thallus and dispersion around the bay by currents. As described by Benzieet al.(2000), C. sertularioidescan has the capacity to resist high solar radiation allows its thalli to float for several days without desiccation until it reaches a substrate to grow. Once a thallus has colonized a substrate, it can easily spread, due to intrinsic characteristics of the species, such as rapid and efficient growth (Collado-Vides & Robledo 1999). Thallus attachment is favored at sites with large coarse sediment. We found that coverage and density of the fronds was higher at sites with substrate composed mainly by Pocillopora spp. fragments (a common coral species at Playa La Penca, Ocotal and Playa Blanca). Most of these reefs develop over a structure of dead coral (Glynnet al.1983, Cortés 1997, Jiménez 1998) which provide an appropriate surface that favors the attachment of theC. sertularioidesstolons and rhizoids (Dumayet al. 2002). While substrates composed by fine sediments are less likely to be colonized byC. sertularioides. Sites with the highest coverage ofC. sertularioideswere located adjacent to coastal development, such as hotels, human communities, boat anchorage sites as well as complex coral reef structures. At sites, such as Playa Penca, Ocotal and Playa Blanca (Fig. 1), with coral reefs present, the bottom was composed of coarse sediments from fragments of dead coral (Pocillopora spp.), where the algae can attach easily.

In addition, frond and stolon morphology can adapt also to a combination of physical factors such as depth and substrate, as has been found for otherCaulerpaspecies (Meineszet al. 1995). When C. sertularioidesgrew on rocky substrates in shallow water the stolon was thicker, this adaptation allows the alga to hold to the substrate and resist the swell. Fronds in theses shallow depths (high solar radiation) tended to be smaller, and sometimes were not present. At greater depths and in finer sediments, stolons were thinner and more branched. This adaptation allows the alga to intercalate into fine sediments, and to easily obtain nutrients. This change in morphology with depth has been previously found to occur withCaulerpacupressoides, where fronds size decreased as the swell influence increased (Collado-vides & Robledo 1999). This adaptation provides (i) resistance to strong hydrodynamic forces (Collado-vides & Robledo 1999) in high energy coastal zones, and (ii) efficiency of nutrient uptake.

High genetic variability due to sexual reproduction of this opportunistic species at Bahía Culebra may promote adaptation to different environmental physical-chemical conditions (i.e depth, temperature, water motion, nutrients) (Allendorf & Lundquist 2003). This is evident at the bay, whereC. sertularioidesshowed morphological differences when growing on different substrates and depths, favoring local spreading of the green alga (Colladovides & Robledo 1999). As Clifton (1997) and Clifton and Clifton (1999) demonstrated for other species ofCaulerpa,C. sertularioidesin Bahía Culebra exhibit a synchronous release of sexual gametes and fertilization occurs in the water column. This green alga transforms all its vegetative inner content into gametes (holocarpic) that are released by papillae in the stolons and fronds (Dawes 1981, Bold & Wynne 1985, van den Hoeket al.1998), leaving the cell walls empty, which make the thallus turn white (van den Hoeket al.1998).

Bahía Culebra, as in Gulf of California (Mexico), percent coverage and frond density ofC. sertularioidesseasonally fluctuated in relation to environmental factors (Scrosati 2001). During the dry season, when upwelling occurs, percent coverage and frond density increased. Such high algal biomass is typically caused by the presence of high nutrients concentrations (Bell 1992, Lapointe 1997, Szmant 2002) as during upwelling events. These nutrients are rapidly taken up from the environment, and are consumed in relatively short time periods (Rodríguez-Sénz 2005, J. Acuña-González pers. comm.).

Coverage and frond density decreased 40% in March (2004, 2005), one month after the upwelling peak (Fig. 7). This is consistent with Rodríguez-Sáenz (2005) who found that phytoplankton concentration and zooplankton density decreased after upwelling in Bahía Culebra as evident with other algal biomasses (e.g.Ulva spp. and Dictyota spp., pers. observ.) that clearly decreased.

Although coverage and density ofC. sertularioidesdecreased during some months of the rainy months when nutrients decrease, it remained covering an average of 10% of the substrate (Fig.  7). In Uva Island, Panama, Smithet al. (2010) found that the maintenance ofC. sertularioidespatches, where there are no external nutrient inputs from the upwelling, is due to an association with epiphytic cyanobacteria, together with spatial refuges, suggesting mechanisms that maintainC. sertularioidesnear reef systems in the absence of high nutrients. Then from August to September the cover and frond density increased again when precipitation, organic material as well as phytoplankton biomass and zooplankton abundance increase in the bay (Rodríguez-Sáenz 2005).

Algal frond density and cover porcentage may be related to nutrient concentration in the environment, and our study suggests that a non-natural supply of nutrients during the wet season may trigger algae overgrowth, as has been reported in other areas (Lapointe 1997, Schaffelke & Klumpp 1997, Little 2000). This is of concern because in Bahía Culebra there is no infrastructure to treat water derived from human activities, such as golf courts, hotels and agriculture. Phosphate and nitrate are the most important nutrients influencing algal growth at the bay, that can come from upwelling and anthropogenic sources, spreading at Bahía Culebra mainly by currents (Jiménez 1998). Water quality near coastal communities is currently a global problem (PNUMA 2007) and nutrient overloading in the ocean is one of the factors influencing coastal water quality and can have effects on different ecosystem dynamics, such as those in coral reefs (Fabricius 2005). Thus, nutrient supply in Bahía Culebra must be better understood to determine non-natural sources and to improve coastal management.

Although decreasing and increasing nutrient concentrations may have an important role in driving algal patterns, it can act in synergy with the temperature, which is another of the main abiotic factors influencing the dynamic in the bay (Fig. 3). Coverage and frond density ofC. sertularioidescan increase with nutrient uploads, however there is a peak in the values of those measurements in February with lower temperatures, during the upwelling, than in September, during the rainy season (Fig. 7).

According to Terrados and Ros (1992) seasonal adaptations of macroalgae, are more common in temperate regions and in areas where upwelling occurs. These seasonal temperature variations can cause algal physiological adaptations in response to photosynthetic and growth requirements.At Bahía Culebra, we registered temperature differences of 10ºC between seasons, which increase probabilities of a synergic action with high nutrient concentration onC. sertularioidesabundance. OtherCaulerpaspecies, such as C. taxifolia, have demonstrated the capacity to adapt to low temperatures (Joussonet al.2000), providing the ability for growth at deeper depths and large temperature ranges (Belsher & Meinesz 1995), thus increasing its invasive capacity (Allendorf& Lundquist 2003). Another important factor may be the attenuation of herbivory in upwelling environments, as suggested by Floeteret al.(2005) and Smith (2008), however this factor was not measured in our study.

Acknowledgments

We are grateful to Davis Morera, Eva Salas, Bernadette Bezy, Eddy Gómez and Eleazar Ruiz for their collaboration in the field and in the laboratory. Specially thank to Bernadette Bezy for revising the English. We also want to thank the Costa Rican Institute of Tourism (ICT) by facilitating us the installations in Playa Panama and to the National Meteorological Institute of Costa Rica for providing meteorogical data. This manuscript was improved with the comments made by Ricardo Soto, Gerardo Ávalos and Javier Carrión. This work was supported through the Ecodesarrollo de Papagayo project and by project no. 808-98-013, of the vicerrectoría de Investigación, Universidad de Costa Rica.
References

Allendorf, F.W. & L.L. Lundquist. 2003. Introduction: population biology, evolution, and control of invasive species.

References

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