An important goal of coastal wetland restoration is to support and rehabilitate wildlife populations, including birds, fish, and key invertebrate species, by providing habitat and trophic support (Tori et al. 2002, Wozniak et al. 2006, Benson et al. 2018). Restoring these ecological functions can provide substantial support for local, regional, and national economies by increasing the populations commercially and recreationally important species (Engle 2011, Mazzotta et al. 2019). This economic value shapes near- and long-term management priorities that focus on conserving and restoring these wildlife-based functions as the primary goals of many local and regional wetland restoration projects.
Coastal wetland restoration projects sometimes employ beneficial uses (BU) of dredge material techniques to bring large degraded areas to an elevation appropriate for emergent marsh vegetation (Parson and Swafford 2012). Plant coverage often increases quickly in these areas through seed dispersal and vegetative spread (Matthews and Endress 2008, Yando et al. 2019, Armitage 2021) but this outcome is not always directly related to the restoration goal of boosting wildlife use of the degraded area. In particular, BU projects do not always target shorebirds or wading birds (Warren et al. 2002), even though those birds can boost the economic benefit of a restoration project by drawing birdwatchers to the area. Wetland birds require a combination of habitats including non-vegetated tidal flats, ponds and creeks to meet their life cycle requirements and support foraging on biofilms (surficial slurries of microalgae and organic matter) and burrowing organisms (infauna) (Jourdan et al. 2021, Kuwae et al. 2021). When non-vegetated features that support these trophic sources are integrated into restored sites, there is rarely adequate data to assess their persistence and value over time. Here, we describe a case study that assessed whether older restored sites retained non-vegetated features that could support wetland bird foraging.
The J.D. Murphree Wildlife Management Area on the Upper Texas Coast was the focal system for this project (Figure 1; also see site map in Armitage 2021). Wetlands in the area have a long history of anthropogenic and natural disturbances that have resulted in marsh degradation and loss (TPWD 2013). Since 2006, dredge materials obtained from nearby port and channel maintenance projects have been used in a BU approach to raise more than 8 km2 of subsided habitat to emergent marsh elevation in the study area (TPWD 2013). The study area included BU restoration areas that were created in 2013 or 2021. Subsets of BU areas created in 2013 were actively planted with emergent marsh vegetation (P13), and others were left unplanted (U13). All BU areas created in 2021 were unplanted (U21). Reference marshes (REF) were adjacent unmanaged areas comprised of a mix of relict plant communities and non-vegetated features at comparable elevations and tidal influence. Three sites in each of the four restoration states (U13, P13, U21, REF) were sampled; all sites included two broadly defined habitat types: vegetated habitat (including interior and marsh edge) and lower elevation, non-vegetated habitat (mudflats and ponds).
Map depicting array of study sites within the J.D. Murphree Wildlife Management Area in Texas, USA. An expanded area map is available in Armitage (2021). Restoration states are P13 (sites created and planted in 2013), U13 (sites created in 2013 but not planted), U21 (created in 2021 but not planted), REF (reference sites).
Infaunal Communities
Infauna (including macroinvertebrates, microinvertebrates and protists) were collected in replicate cores (2.5 cm diameter, 5 cm deep; volume 24.5 cm3) from each habitat type within each restoration state during the 2022 growing season (between May and October). Replication varied based on habitat presence and accessibility, with 6–15 cores per habitat type in each restoration state. Cores were rinsed through a 500 mm sieve and fixed and stained in a 10% Formalin/Rose Bengal solution. Trained observers identified infauna under a dissecting microscope to the lowest practical taxonomic level (most commonly to class). Data were square-root transformed prior to analysis. Differences in infaunal abundance were assessed with a two-way Analysis of Variance, and differences in community composition was assessed with a two-way Analysis of Similarity (ANOSIM) based on a Bray-Curtis similarity matrix. The factors were habitat type (vegetated and non-vegetated) and restoration state (U13, P13, U21, REF) (R Core Team 2020). In spring 2014, infauna were collected from the non-vegetated habitat at a subset of U13 and P13 sites; these values were qualitatively compared to 2022 values.
Across all 2022 sampling sites, the most common types of infauna were native taxa including annelid worms, ostracods, foraminiferans, insect larvae, and gastropods. Total infauna abundance in U13 sites was substantially higher in 2014 (average count per core 722 ± 341 SE) than in 2022 (35 ± 12). In P13 sites, there was little change in infaunal abundance between 2014 (36 ± 16) and 2022 (25 ± 9). In 2022, total infaunal abundance varied among habitat types and restoration state (ANOVA habitat type * restoration state df = 3, F = 15.35, p < 0.001). The highest macro/microfaunal abundances occurred in the non-vegetated areas of U13 sites (Figure 2a). In contrast, the highest protist (foraminiferan) abundances occurred in the vegetated areas of the reference sites (Figure 2b). ANOSIM indicated a high degree of overlap in infaunal community composition among habitat types and across restoration states (habitat type R = 0.149; restoration state R = 0.178). Infaunal abundance is often linked to edaphic characteristics (Craft and Sacco 2003), and previous work at an adjacent site suggested that soils in reference areas were sandier and had higher nutrient content than those in restored areas, but that all restored areas were largely similar to each other (Armitage et al. 2014). Thus, the large difference between U13 and P13 areas (Figure 2a) suggests that other factors, perhaps linked to the plant community, may have influenced infaunal abundance in these areas.
Total infaunal counts per core (24.5 cm3) in different habitat types and restoration states. a) Macro- and microinvertebrates; b) foraminiferans. See Figure 1 for description of restoration states. Box plots depict the median (bold line), first and third quartiles (box), minimum and maximum values (whiskers), and outliers (points).
Avian Communities
To assess bird use of restored and reference sites, game cameras were set up at one site in each of three restoration states: U13, P13, and REF. Cameras were installed on poles one meter from the ground, overlooking a representative mixture of vegetated and non-vegetated habitat within each site. Cameras were deployed for six two-week periods during migration and overwintering periods between October 2013 and April 2015. The photos were manually reviewed and bird abundance and identity were recorded. Counts focused on native, wetland-dependent species that forage on benthic organisms. Individual birds were not counted more than once if they appeared in a sequential series of photos. The high incidence of images with no detectable birds precluded meaningful statistical analysis, so patterns of bird use are described qualitatively. In 2022, we recorded qualitative bird observations in person during the infaunal sampling events.
In 2013–2015, birds were most frequently observed in unplanted restored areas (Figure 3). Species richness (S) at each site (cumulative across all survey dates) was substantially higher in unplanted (U13) areas (S = 17) relative to planted (P13) areas (S = 3) or reference marshes (S = 8). In 2022, all older sites (U13, P13, REF) were heavily vegetated by a monoculture of native Spartina alterniflora (Armitage 2021) and few birds were observed in those sites. Large mixed-species aggregations of shorebirds and wading birds were observed only in non-vegetated (mudflat or pond) areas, particularly in U21 sites that had little emergent vegetation coverage.
Heat map showing average bird abundance (number/2 weeks) over a series of six observation periods from 2013–2015 at one representative site in each of three restoration states as defined in Figure 1.
Potential and realized bird use of restored wetlands was linked to the availability of non-vegetated habitat such as mudflats and ponds. Shortly after restoration, bird assemblages were more diverse and abundant in areas that had not yet developed dense stands of wetland plants (Figure 3). As noted above, infaunal abundance, a proxy for trophic support for benthic foraging bird species, was highest in unplanted areas after restoration, and remained high in those areas that persisted in an unvegetated state over the following decade (Figure 2). However, dietary needs among wetland-dependent birds are not monolithic, and there are numerous smaller species (e.g., Family Scolopacidae) that consume biofilms—a slurry of protists, benthic microalgae and organic matter on the sediment surface (Kuwae et al. 2008). Based on our observed patterns of foraminiferan abundance, biofilm biomass may be higher on substrates supporting diverse stands of vegetation, such as those found in reference areas (Figure 2b).
Overall, our results indicated that an ideal restoration design should increase small-scale elevation heterogeneity to create persistent non-vegetated features to enhance shorebird use while balancing permit-mandated goals to increase vegetation cover. There is broad recognition that wetland restoration has strong potential to increase bird abundance (Ortega-Álvarez and Lindig-Cisneros 2012, Sullivan 2015), but a more intentionally designed heterogeneous elevation approach may further enhance diversity and habitat use for a wider array of avian species (Comín et al. 2001, Armitage et al. 2007, Pickens and King 2013, Boothby 2017). Planning for heterogeneity can support populations of shorebirds that forage on mudflats or in tidal creeks (Armitage et al. 2007) while also providing critical habitat for marsh birds such as rails or other marshnesting species (Pickens and King 2013). However, that heterogeneity in the elevation and vegetation landscape may not persist over time as dense monocultures of native wetland vegetation often develop rapidly in non-vegetated areas (Ward et al. 2003, Armitage 2021).
Although there is broad agreement that elevation heterogeneity is likely to increase bird use of restoration projects, challenges remain in translating that accepted ecological paradigm into quantitative elevation guidelines for the engineers designing and constructing the sites (Armitage et al. 2024). These guidelines, including specific elevation targets and ratios of vegetated, mudflat and submerged habitat, must be informed by site-specific data on bird use of habitat types. Future research should aim to produce elevation guidance that can be used by practitioners in marsh construction projects. Monitoring protocols for shorebirds, wading birds, and others are well-developed in the region (Brush et al. 2019). Yet, monitoring efforts are pervasively underfunded, yielding piecemeal data that does not completely cover the scope of bird use and health. This results in limited applicability to management in practice (Schulz 2021). Studies focused on longer-term use and life history patterns of birds could help to unravel complexities in bird habitat use; this knowledge can then be used to improve management decisions (Schulz 2021). Further, such in-depth studies would establish a robust baseline, allowing for more informed responses to future disturbances or changes in management needs.
Author Contributions
AA: Conceived the study, collected and analyzed data, wrote the paper. AGH: analyzed data, edited paper. AM, MP, JT: collected data, edited paper.
Acknowledgements
This paper was funded in part by a Texas Coastal Management Program grant approved by the Texas Land Commissioner, providing financial assistance provided under the Coastal Zone Management Act of 1972, as amended, administered by the National Oceanic and Atmospheric Administration (NOAA), Office for Coastal Management, pursuant to NOAA Award Nos. NA19NOS4190106, NA21NOS4190136, and NA24NOSX419C0025. In addition, this paper is a result of research funded by the National Oceanic and Atmospheric Administration’s RESTORE Science Program under award NA21NOS4510174 to Texas A&M University at Galveston. The views expressed herein are those of the authors and do not necessarily reflect the views of NOAA, the U.S. Department of Commerce, or any of their subagencies. This work was made possible by many resilient field assistants, especially K. Bowers, J. Sigren, C. Weaver, A. Whitt, C. Hall, and M. Ciesielski.
This open access article is distributed under the terms of the CC-BY-NC-ND license (http://creativecommons.org/licenses/by-nc-nd/4.0) and is freely available online at: http://er.uwpress.org