Generally, the design of the sampling strategy contains three main parts: to determine the sampling approach, to define the sample size and to arrange the sampling interval. Other aspects easy to judge according to specific situations, such as sample device, mesh size, sampling time, and sampling depth, are not discussed in this study (
Fanini and Lowry, 2016;
Ferraro and Cole, 2004;
Ferraro et al., 2006;
Hammerstrom et al., 2012;
Schlacher et al., 2008;
Schlacher and Wooldridge, 1996;
Souza and Barros, 2015). First, sampling methods include a range of standardized approaches that have already been applied to the estimation of species richness, such as random (
Shen et al., 2012), stratified (
Schooler et al., 2014), systematic (
Dowd et al., 2014) and transect sampling designs (
Beukema and Dekker, 2012). Each method has its own strengths and weaknesses related to the sampling area, efficiency, labor and cost. For intertidal areas, transect sampling has become a well-recognized strategy commonly used to survey macrobenthos (
Beukema and Dekker, 2012;
Schoeman et al., 2008;
Varfolomeeva and Naumov, 2013). Transect sampling in intertidal areas is often considered practical and efficient because these areas are spatially variable, and the variation presents itself as obvious environmental gradients (such as salinities, heights, sediment coarseness) along the axes perpendicular to shore (from high tide level to low tide level). Provided that an adequate number of across-shore transects are sampled, each of the likely across-shore “niches” present on the gradient will be represented in a pool of fewer samples by taking a sequence of samples along an across-shore line (
Schlacher et al., 2008). However, transect sampling is performed using numerous and continuous quadrats with the same intervals; thus, it has rarely been adopted in the intertidal zones of estuarine wetlands, as such sampling is not practical in the harsh physical field environment. An optimized transect sampling was designed versus a simple transect survey to solve the difficulties in harsh environments. This approach is called the within-transect stratification sampling design, which has stratification within the transect according to habitats types related to species distribution. It is assumed that the variation in density is small when the collection of habitat types within the transect is the same.
Skibo (2005) applied this within-transect approach with other routine methods (e.g., random sampling, simple transect sampling) to estimate the richness of red sea urchins in benthic subtidal areas by stratifying according to the substrate types of the strata. The results showed that this approach performed better in the sampling effort, precision and marginal cost, as it captured all aggregation patterns of urchins within a transect that may exist in different substrate types. Second, sampling size has become an important issue, as it provides sufficient precision of the “true” species richness. Until now, some studies still followed the sample size conventions of the sampling team (e.g., three to five samples at each tidal level along the high-low tide transects) (
Chen et al., 2009;
Lv et al., 2014,
2016;
Wang et al., 2010). This tended to result in negatively biased estimates for macrofaunal richness as accuracy decreased at low levels of sampling effort (
Schoeman et al., 2003). Fortunately, more and more researchers have explored the relationship between total sampling effort and macrobenthic species richness by using extrapolation procedures, such as species accumulation curves (
Beukema and Dekker, 2012;
Muxika et al., 2007;
Schoeman et al., 2003,
2008;
Schooler et al., 2014).
Jaramillo et al. (1995) recommended that a sampling effort of 4 m
2 would be appropriate for estimating macrobenthic richness in an intertidal sandy beach by using species accumulative curves. In addition to the ability to determine the minimum sampling effort based on a balance between accuracy, bias, and precision, the advantages of this method include that it provides more accurate estimates of species richness than observed values and allows for the comparison of species richness on different spatial or temporal scales (
Colwell et al., 2012). Many studies have not paid much attention to the third part, the determination of the sampling interval. Ecologists have traditionally arranged uniform intervals to take a sequence of samples along transects, and these intervals range between 1 and 25 m, depending on the aims of the studies (
Schlacher et al., 2008). This fixed interval method, however, is usually irrespective of the heterogeneous environmental gradient (morphology, sediment, vegetation distribution), inappropriate to capture species patchiness distributed at a small scale, and likely to result in spatial autocorrelation among the individual samples (
Schlacher et al., 2008). Instead of arbitrarily determining fixed sampling intervals,
Schoeman et al. (2003) applied a repeated resampling technique of datasets, Monte Carlo simulation, to gain an understanding of the range of results that might be possible for any given sampling method under consideration and to determine the proper sampling intervals and quadrat numbers needed for sampling a sandy beach.