Surf zone zooplankton temporal dynamics and their environmental regulation in a southwestern Atlantic sandy beach (Pehuen Co, Argentina)
Introduction
The surf zone of sandy beaches is the transition area between the breaking zone of waves and the swash zone. It plays an essential role in the transport of materials and the exchange of organic matter and nutrients with adjacent habitats (McLachlan and Defeo, 2018). These productive ecosystems support a diverse coastal fauna (Schlacher et al., 2008; Dugan et al., 2015; Manning et al., 2013; McLachlan and Defeo, 2018) and are generally used by endemic species as well as by the transient taxa that arrive to take advantage of feeding conditions (McLachlan and Defeo, 2018). Despite the importance of the surf zone, current knowledge is mainly focused on variations in phytoplankton and benthic macrofauna there, with few studies focused on the zooplankton community (e.g., Dominguez-Granda et al., 2004; Odebrecht et al., 2010; Pinheiro et al., 2013; Odebrecht et al., 2014; Marin Jarrin et al., 2017).
Zooplankton communities play an essential role in the ecology of surf zones, serving as a connection with different trophic levels (Oliveira-Santos et al., 2016). In addition, the fauna of the lowest beach may extend its distribution seawards into the turbulent surf zone, where zooplankton can be abundant (Defeo et al., 2009). DeLancey (1989) stated that zooplankton represents the main food item for larvae and juveniles of fishes visiting the surf zone. Given that zooplankton is a primary food supply for fishes but also for suspension feeding macrofauna, changes in this community would have a relevant impact on sandy beach ecosystems (Defeo et al., 2009). The zooplankton community is the least studied one in surf zones worldwide, mainly due to the difficulty in sampling because of the dynamic physical conditions (McLachlan and Defeo, 2018). Moreover, most previous studies focused on tropical and subtropical sandy beaches (Avila et al., 2009; Da Costa et al., 2011; Pinheiro et al., 2011, Pinheiro et al., 2013; Aboul Ezz et al., 2014; Oliveira-Santos et al., 2016), whereas very few studies considered temperate systems (DeLancey, 1987; Stull et al., 2016; Menéndez et al., 2019).
It has been demonstrated that the effect of environmental variables on the spatio-temporal distribution of planktonic organisms in surf zones is substantial (Aboul Ezz et al., 2014; Stull et al., 2016; Menéndez et al., 2019). Constant temperatures and oligotrophic waters are factors influencing the zooplankton dynamics in subtropical sandy beaches such as Ajuruteua (Pinheiro et al., 2013) and Fortaleza (Oliveira-Santos et al., 2016) in northern Brazil. The effect of seasonality, principally in terms of changes in precipitation, and the associated changes in salinity have a substantial impact on local zooplankton dynamics in Ajuruteua beach (Da Costa et al., 2011). Thus, knowledge about the influence of environmental variables on surf zooplankton dynamics can contribute to an improved understanding of changes in the marine coastal function, potentially providing a useful tool for future samplings in similar coastal areas. Therefore, the specific aims of this study were: (i) to investigate the temporal dynamics of the composition and abundance of the surf zone zooplankton in a temperate sandy beach and (ii) to evaluate its association with environmental variables.
Section snippets
Study site
Pehuen Co beach (PC; 38°59′51” S; 61°33′16” W) is located in the southwest coast of Buenos Aires Province, Argentina, 80 km away from the innermost zone of the Bahía Blanca Estuary (BBE) (Fig. 1). It is a dissipative sandy beach, situated in an open bay with a straight E-W orientated shoreline. The area has a mesotidal regime with semidiurnal tides, with an amplitude range between 2.32 m and 3.35 m for neap and spring conditions, respectively (Servicio de Hidrografía Naval (SHN), 2009). In PC,
Environmental variables
During the study period, water temperature varied from 10 °C in August to 25 °C in February (Fig. 2A). Salinity showed a similar trend, with minimum values in August (31) and maximum ones in February (34) (Fig. 2A). Chl-a fluctuated between 2.5 μg L−1 (February) and 17 μg L−1 (November), being high in March (11.1 μg L−1), July (12 μg L−1), and September (12.3 μg L−1) (Fig. 2B). SPM and POM showed a clear seasonal pattern, with minimum concentrations in warmer months (SPM: 45.3 mg L−1, February;
Discussion
We observed strong seasonal variation in the zooplankton community structure in PC. Total zooplankton abundance was similar to that found by Morgan et al. (2016) for the surf zone of some sandy beaches in Monterey Bay, USA, but approximately an order of magnitude lower than those reported in similar studies in other temperate surf waters (Stull et al., 2016) and tropical areas (Da Costa et al., 2011; Pinheiro et al., 2013). The seasonal pattern in abundances of the dominant copepods was
Financial support
This work was supported by the Consejo Nacional de Investigaciones Científicas y Técnicas (CONICET, Argentina) through an internal doctoral scholarship-CONICET 2016-20120 (B. C. A., 2282016000116500).
Declaration of Competing Interest
The authors declare that they have no known competing financial interests or personal relationships that could have appeared to influence the work reported in this paper.
Acknowledgments
Partial support for this research was provided by grants from the Agencia Nacional de Promoción Científica y Tecnológica (ANPCYT, PICT2012-0356) and Consejo Nacional de Investigaciones Científicas y Técnicas (CONICET, PIP 1122030100467CO). We also thank Dr. Walter Melo for drawing the map of the study area and Dr. Martín Amodeo for his valuable contribution to the statistical analysis section of the manuscript.
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2022, Continental Shelf ResearchCitation Excerpt :The surf-zone is no exception: water temperature, precipitations -and their associated changes in salinity- and suspended sediments have been pointed up as the main structuring factors of zooplankton distribution (e.g. Menéndez et al., 2019; Stull et al., 2016). Other events like wind regime and tidal cycle also affect zooplankton dynamics on a shorter time-scale (Baleani et al., 2020, 2021). Research on macrobenthic organisms and fishes has suggested that the compositions of biological assemblages are highly variable, changing with fluctuations in physical parameters as water temperature, hydrodynamic factors such as wave height and turbidity, and the biomass of drifting algae or seagrass (Beyst et al., 2001a,b; Olds et al., 2018) and, as a consequence, they can affect the productivity of these environments (Janssen and Mulder, 2005; Marin Jarrin and Shanks, 2011; Sato et al., 2008).
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2021, Regional Studies in Marine ScienceCitation Excerpt :Studies on zooplankton biodiversity and population processes have been done in estuaries and other coastal areas (e.g. David et al., 2005; Gonçalves et al., 2015; Marques et al., 2014; Queiroga et al., 2005), but few focused on surf zones. Surf zone zooplanktonic communities are poorly known worldwide, with few studies carried out in Brazil (e.g. Avila et al., 2009; da Costa et al., 2011; Oliveira Santos et al., 2016; Pinheiro et al., 2013, 2011; Rodrigues et al., 2019), India (Ku Sahu et al., 2012), United States of America (DeLancey, 1987; Morgan et al., 2016; Stull et al., 2015); Argentina (Baleani et al., 2020; Menéndez et al., 2019), Egypt (Aboul Ezz et al., 2014) and Mexico (Fernández-Aldecoa et al., 2019). The surf zone communities included Copepoda, Cirripedia, Mysidacea, Bivalvia, Polychaeta, Decapoda larvae, Amphipoda and Isopoda, being the first group the dominant one.