Metazooplankton communities in the Ahe atoll lagoon (Tuamotu Archipelago, French Polynesia): Spatiotemporal variations and trophic relationships

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Abstract

Metazooplankton abundance, biomass (<80 μm, 200–500 μm and >500 μm) and community structure in the Ahe atoll were studied together with their relationships with environmental factors (temperature, salinity, wind) and trophic factors (phytoplankton, bacteria, heterotrophic nanoflagellates (HNF) and ciliates) during three periods in 2008–2009. Meroplankton, mainly bivalve and gastropod larvae, was dominant. Holoplankton was dominated by copepods, the main species being Oithona spp., Paracalanus parvus, Clausocalanus spp., Corycaeus spp., Acartia fossae and Undinula vulgaris. The results suggest a clear wind influence on the structure and horizontal distribution of the zooplankton communities. The metazooplankton appeared to be controlled mainly by food resources, suggesting a bottom-up control. The low nanophytoplankton biomass in contrast to the high abundance of picophytoplankton, HNF and nano-particle grazers (mainly Oithona spp., Paracalanus and bivalve larvae) highlighted the importance of the microbial loop in the food web.

Introduction

Metazooplankton plays a major role in the functioning and productivity of aquatic ecosystems through its impact on nutrient dynamics and its key position in food webs. Most mesozooplanktonic organisms exert a strong grazing impact on the phytoplankon and on the microzooplankton (Pont, 1995, Calbet, 2008). They are also a food source for organisms of the upper trophic levels such as planktivorous fish and carnivorous invertebrates (Pinel-Alloul, 1995). In coral reef and atoll lagoon environments, they are important contributors to the benthic and pelagic food webs (Bozec et al., 2004, Alldredge and King, 2009). Zooplankton organisms can also be used as biological indicators for pollution, water quality and eutrophication (Attayde and Bozelli, 1998, Webber et al., 2005). Their generation times may be short enough to respond quickly to acute stress but long enough to integrate the effects of chronic problems. These attributes can be useful to design a community ecosystem health indicator (Cairns et al., 1993). However, very few studies have dealt with zooplankton in atoll lagoons (Gerber, 1981) and only a few have concerned the Tuamotu Archipelago (Michel et al., 1971, Ricard et al., 1979, Le Borgne et al., 1989, Carleton and Doherty, 1998).

Coral reef and atoll lagoons are productive ecosystems, compared to surrounding ocean (Hatcher, 1997). They have been frequently exploited for aquaculture, as in the Tuamotu Archipelago (French Polynesia) where pearl oyster farming is a major driver of the local economy (Andrefouët et al., 2012). The planktonic pearl-oyster larvae mainly feed on nanophytoplankton with high ingestion rates (Doroudi et al., 2003). The adults, cultivated in sub-surface pelagic nets, are also important passive consumers of nanoparticles (Yukuhira et al., 1998, Fournier et al., 2012). Farmed pearl-oyster populations can be considered as components of the pelagic ecosystem in pearl farming lagoons. In these ecosystems, they share (and may compete for) food resources with several pelagic components (including zooplankton) and may serve as food for other ones. Studying the different communities of the pelagic ecosystem and evaluating their stocks and their inter-relationships are required to define the optimal conditions for the recruitment and development of oysters. This information is also necessary to determine the load capacity for cultivation (Niquil et al., 1998).

A multidisciplinary research program was funded by the European Development Fund (EDF) in 2007 to describe, among other goals, the ecological environment of the pearl-oyster Pinctada margaritifera (Linnaeus, 1758) and its relationship with the pelagic trophic network.

Our study is part of this multidisciplinary study on the trophic environment of P. margaritifera. It aimed at analyzing within a farmed lagoon the spatiotemporal variations of metazooplankton standing stock and community composition according to the main environmental and trophic parameters.

Section snippets

Study site and sampling strategy

The Ahe atoll (14°29′S; 146°18′S) to the north west of the Tuamotu Archipelago in the Pacific Ocean is 23.5 km long and a maximum of 12.2 km wide (Fig. 1). The lagoon is 142 km2 in area with maximum depth of 70 m in the central zone. The atoll rim which surrounds the lagoon is not completely closed: there is a passage (300 m long and about 20 m deep) to the northwest between the lagoon and the ocean, and several spillways mostly in the southern part of the rim. The climate is wet tropical with one

Environmental and trophic variables

Different meteorological conditions were observed during the 3 sampling periods (Fig. 2). Rainfall were high in February 2009 (70 mm month−1) compared to May and October 2008 (52 and 23 mm month−1, respectively). Wind speed was lower during the May 2008 survey (0–7.7 m s−1 during the sampling period) than for the other surveys (6.1–11.5 m s−1 and 3.0–11.5 m s−1 in October 2008 and February 2009, respectively). Water temperature and salinity showed significant variations between sampling seasons (Fig. 3).

Hydrobiological context

The phytoplanktonic biomass, as inferred from Chl a, measured in the Ahe lagoon was comparable to that in other oligotrophic ecosystems and similar to that in other lagoons of the Tuamotu Archipelago (Rancher and Rougerie, 1995). The proportion of picoplankton was close to that recorded in other atoll lagoons and in agreement with additional measurements in Ahe made in 2009 and 2010 (Charpy, 1996, Charpy et al., 2012).

High spatio-temporal variations of chlorophyll, autotrophic (picoeukaryotes,

Conclusion

Our results showed the predominance of meroplankton and bivalve larvae in Ahe as compared to other coral reef and atoll lagoons. while the dominance of bivalve larvae suggests potentially major community change arising from aquaculture activities (pearl oyster farming), it is probably mainly due to the importance of wild populations. Our study also suggests that tide-flushing and wind driven circulation of the lagoon, as evidenced in the study by Dumas et al. (2012), plays an important role in

Acknowledgements

This study was funded by the 9th European Development Fund (EDF) (grant POF/001/002 N°1 to Serge Andréfouët and Loic Charpy, IRD). The authors express their gratitude to the EDF and Service de la Perliculture staff, especially Alain Lo-Yat, for their efficient help during sample collection on Ahe atoll. They also thank two anonymous reviewers for helpful criticisms and comments on the first version of the manuscript.

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