Plant species/lineage performance
Spartina alterniflora inhabits saline, low-elevation sites in coastal marshes whereas S. patens is found at higher elevations and more brackish habitats (Bertness, 1991; Hester, Mendelssohn, & Mckee, 1996; 2001). In contrast, S. californicus and Z. miliacea occupy freshwater habitats and co-occur with P. australis in the area where our study was conducted (Chabreck, 1970; Howard & Rafferty, 2006; Li, Hopkinson, Schubauer-Berigan, & Pennings, 2018). At two months post planting, all species/lineages had high survivorship (mean of 80%), despite considerable variability in water depths. We attribute this to our selection process for transplantation – plantings were chosen that had a minimum height of 61 cm (Table S1) whereas water depths were, in most cases, below this level (see Figure 3). However, by six months post-planting, the two Spartina species disappeared from all sites (Table 2).
By nine months post-planting, survivorship of plantings from all species and sites was just 32%. One possible explanation for this generally low performance is legacy effects from the dieback. In studies of P. australis in Europe, eutrophic conditions, coupled with elevated sulfide concentrations and organic matter accumulation were evident following dieback events (van der Putten, 1997; Brix, 1999). Similar results were found in areas of S. alterniflora dieback in coastal Louisiana (Alber et al., 2008; Elmer, Useman, Schneider, Marra, LaMondia, Mendelssohn, Jiménez-Gasco, & Caruso, 2013; Crawford & Stone, 2015) and for the recent P. australis dieback in the MRD (Lee et al., 2023). There is also the possibility that dieback was brought about by soil-borne pathogens that may persist in the soil for some time after a dieback event (Elmer et al., 2013). Specialist soil pathogens may inhibit reestablishment of pre-dieback vegetation (e.g., P. australis in the MRD), whereas generalist pathogens may prevent successful establishment of new plant species. Interestingly, lineages of P. australis have distinctly different microbial communities (Bowen, Kearns, Byrnes, Wigginton, Allen, Greenwood, Tran, Yu, Cronin, & Meyerson, 2017; Schroeder, Halbrook, Birnbaum, Waryszak, Wilber, & Farrer, 2020) such that dieback-associated pathogens could be lineage specific. At this point, we do not know how long the legacy effects persist, although Lee et al. (2023) found that dieback soils differed markedly from healthy (non-dieback soils) 1-2 years following a dieback event and that these differences translated into reduced growth rates for all three lineages of P. australis. Although there have been other attempts to restore marsh habitats following dieback events (Ostendorp, Iseli, Krauss, Krumscheid-Plankert, Moret, Rollier, & Schanz, 1995; Kuehl & Zemlin, 2000; Ogburn & Alber, 2006; Tang, Cui, & Zhao, 2006; Bakker, Veen, Ter Heerdt, Huig, & Sarneel, 2018), research is needed to understand how soil legacies may affect restoration success and how long those legacy effects persist.
Another explanation for low plant survival was variation in water depth among restoration sites. We purposely selected sites that varied in water depth and by nine months post-planting, there was a significant negative relationship between planting survivorship and water depth (Figure 5). Thus, we found support for prediction three that deeper-water sites would have lower restoration potential. Our experimental design did not allow us to assess whether species or lineages responded differently to water depth but with the exception of S. californicus, all plant types exhibited a negative relationship with water depth. Even though our focal plants thrive in wetland environments, biomass and survival can be negatively affected by prolonged waterlogging (Mendelssohn & Mckee, 1988; McKee, Mendelssohn , & Burdick, 1989; Latham, Pearlstine, & Kitchens, 1994; Weisner, 1996; Sloey, Willis, & Hester, 2015; Snedden, Cretini, & Patton, 2015; Li et al., 2018). For example, P. australis is regarded as tolerant of high-water levels because of its ability to aerate flooded tissues by transporting oxygen through the aerenchyma, creating an extensive network of internal airspaces (Armstrong & Armstrong, 1991; Jackson & Armstrong, 1999; Eller, Sorrell, Lambertini, Whigham, Hazelton, Skalova, Brix, Cronin, Caplan, Kettenring, Meyerson, McCormick, Pysek, Mozdzer, Guo, Guo, & Bhattarai, 2017). Yet, prolonged flooding and deeper waters are known to negatively affect P. australis (Hellings & Gallagher, 1992; Cronin et al., 2020). Consequently, P. australis usually first establishes upslope and then, through rhizomatous spread, expands into deeper water (Kuehl & Zemlin, 2000; Chambers, Osgood, Bart, & Montalto, 2003).
It came as no surprise that the two Spartina species failed to persist at our experimental sites given their proclivities for more saline conditions. Although we expected them to be eventually outcompeted by freshwater species, particularly P. australis (Bertness, 1991; Silliman & Bertness, 2004; Yuan, Wang, Li, Pan, Lv, Zhao, & Gao, 2013), they disappeared well before other potential competing plant species expanded into their grid plots. Consequently, other unknown abiotic or biotic factors were involved in the disappearance of these species. Similarly, Z. miliacea was gone by 20 months from 2 of the 3 sites in which it was planted. This species has been shown to do best in shallow water (Latham et al., 1994; Li et al., 2018) which may have limited its success in these sites.
Our results supported our first prediction that P. australis would have higher survival and greater clonal growth than the other species used in this study. However, this conclusion was only true for the Delta plantings which, by the end of the study, were still present in five of seven sites. Phragmites australis, as with the other plant species used in this study, spread through the production of rhizomes. Compared to other wetland plant species, P. australis has a very large root/rhizome system that occupies a greater soil volume (Lissner & Schierup, 1997a) which has several advantages: greater ability to compete for belowground nutrients (Burdick & Konisky, 2003), the ability to penetrate into deep, permeable soil layers that contain lower salinity water (Burdick, Buchsbaum , & Holt, 2001) and resists wave action and storm surges (Coops & van der Velde, 1996; Coleman, Cassalho, Miesse, & Ferreira, 2022).
In comparison to Delta, plantings of S. californicus were present in only two of six sites and the area of coverage of this species averaged 8.4 times less than that of Delta. At first glance, our findings are at odds with the study by Howard, Rafferty, and Johnson (2020) which found similarly high survivorship of S. californicus and P. australis in a restored marsh in Louisiana. However, there are two main differences between our studies that make comparisons unwarranted. First, P. australis in the Howard et al. (2020) study was determined to be primarily of European origin but the genetic methods used (see Saltonstall, 2002) were not capable of distinguishing between Delta and EU. Also, up to 1/3 of the plantings in Howard et al. (2020) reportedly could have been the Gulf lineage. As our current study and past work on P. australis clearly demonstrate, lineages of P. australis are functionally very different (Cronin et al., 2020; Knight et al., 2020). Second, high rates of survival among species in Howard et al. (2020) could be due to the fact that fencing was erected around plantings to prevent herbivory from nutria (Myocastor coypus), an important and common non-native inhabitant of Louisiana coastal marshes (Sasser, Holm, Evers-Hebert, & Shaffer, 2018).
Surprisingly, we must reject our second prediction, that the EU lineage would outperform the other P. australis lineages in our restoration trials. In fact, EU performed worst among the three lineages; surviving to 32 months in none of seven sites in comparison to five of seven and two of seven for Delta and Gulf, respectively (Table 2). The one site in which EU persisted to 20-22 months, Cheniere Pass Splay, was one of our shallowest sites (Table 1) that receives fresh water and sediments from an adjacent channel. Regarding area of coverage, the differences among lineages were more apparent. Numerous studies have reported that the EU lineage – the cryptic and highly invasive haplotype M (Saltonstall, 2002) – exhibits higher rates of clonal growth (i.e., rhizome spread, tiller production, above and belowground biomass production), greater plasticity in response to different environmental conditions, and more efficient nutrient assimilation than the North American native lineage of P. australis (Vasquez, Glenn, Brown, Guntenspergen, & Nelson, 2005; League, Colbert, Seliskar, & Gallagher, 2006; Holdredge, Bertness, von Wettberg, & Silliman, 2010; Price, Fant, & Larkin, 2014; Bhattarai, Meyerson, Anderson, Cummings, Allen, & Cronin, 2017; Eller et al., 2017). Comparisons between EU and other P. australis lineages are less common (but see Eller, Lambertini, Nguyen, & Brix, 2014; Allen, 2016; Cronin et al., 2020; Knight et al., 2020). Most notably, we previously found that in both field surveys and common-garden experiments, the EU lineage was more resistant to scale insects (i.e., supported lower abundances) and appeared to be impervious to the dieback syndrome exhibited by co-occurring Delta (Knight et al., 2018; Cronin et al., 2020; Knight et al., 2020). One possible reason why Delta performed better than EU is that Delta is more tolerant of inundation (a water depth of 40 cm) than EU or Gulf (Cronin et al., 2020). In that study, Gulf was least tolerant of inundation and this lineage is generally found at higher elevations, usually on roadsides and river embankments on the margins of the MRD (Cronin et al., 2020). Consequently, we were surprised that it did better than EU in our restoration trials.
Relationship between scale abundance and plant performance
The roseau cane scale, N. biwakoensis, is an important pest of P. australis in its native habitat in eastern Asia (Kaneko, 2004; Brix et al., 2014; Schneider, Broadley, Andersen, Elkinton, Hwang, Liu, Noriyuki, Park, Dao, Lewis, Gould, Hoelmer, & Diaz, 2022) and has been implicated in the dieback of P. australis in the MRD (Cronin et al., 2020; Knight et al., 2020). Even at modest densities (20 adult females per stem), the scale can depress P. australis growth (Cronin et al., 2020) and therefore can impose a constraint on restoration success. The potential for herbivores to thwart restoration efforts has been reported for P. australis (Bakker et al., 2018; Temmink, van den Akker, van Leeuwen, Thöle, Olff, Reijers, Weideveld, Robroek, Lamers, & Bakker, 2022) and other wetland systems (e.g., Llewellyn & Shaffer, 1993; Qian, Chen, Zhang, Wu, Ma, Silliman, Wu, Li, & He, 2021; Wasson, Tanner, Woofolk, McCain, & Suraci, 2021).
In this study, we found that the scale insects can quickly colonize P. australis plantings in less than a year, spreading up to 40 m to our most isolated plantings. Active dispersal by this species occurs via first-instar crawlers; which probably limits its movement to a meter or less. However, passive dispersal by winds, water currents and avian vectors is possible and is probably responsible for most of the colonization of our experimental plantings. As has been reported among naturally occurring stands of P. australis in the MRD (Knight et al., 2020; Bumby & Farrer, 2022), plantings of the Delta lineage had more than four times the abundance of scale insects as the other two lineages. Interestingly, scale abundance (number per meter of stem) was related to stem density of the plantings, although the relationship differed among lineages. With passive dispersal, it would make sense that more dense patches would “capture” more colonists (Hambäck & Englund, 2005). Alternatively, colonists may simply have higher growth rates on more vigorously growing patches of plants (plant vigor hypothesis; Price, 1991). But, a positive relationship between scale abundance and stem density was only evident for Gulf. For both Delta and EU, the relationship was negative. We cannot easily explain this result, although a temporal separation between when scale colonization occurred and when we measured stem density at 11 months could have resulted in a disconnect or even reversal in the relationship between scale abundance and stem density. Unfortunately, the dispersal and colonization behavior of N. biwakoensis, as with most scale insects, is poorly understood (but see e.g., Gullan & Kosztarab, 1997; Magsig-Castillo, Morse, Walker, Bi, Rugman-Jones, & Stouthamer, 2010).
We have no evidence to suggest that N. biwakoensis negatively impacted survivorship of our plantings of P. australis. Neither stem density nor mean stem heights of the plantings exhibited a negative relationship with scale abundance. In fact, we actually found positive associations between stem height and scale abundance for the EU and Gulf lineages. Again, this finding could be due to taller plants being better traps for passive dispersers than shorter plants or that scales do better on vigorous. However, at 11 months, it may have been too early to expect to find measurable negative effects of scales on planting growth. We did not measure scale insect abundance on subsequent survey dates because of the rapidly declining survivorship of EU and Gulf. However, given that the Delta lineage has greatest susceptibility to scale attack (Cronin et al., 2020; Knight et al., 2020), and was most prevalent at the end of the study, it seems unlikely that the scales played a determining role in which lineage was best in these restoration trials. It remains to be seen if the scales eventually cause dieback of our surviving Delta plantings.
Implications for Restoration
The fate of the Lower MRD depends on the stabilization of soil elevation by emergent vegetation which is under threat by eutrophication, salinity intrusion, elevated atmospheric CO2 concentrations, increasing intensity and frequency of hurricanes and storms and flooding events (Turner, 1990; Cahoon, White, & Lynch, 2011). The Mississippi River Delta is of particular concern given its high rates of sea level rise (8.5-9.5 mm year-1), high land subsidence rates that can exceed 1 cm/yr-1 and coastal wetland degradation (Shea & Karen, 1990; Day, Conner, Costanza, Kemp, & Mendelssohn 1993; González & Tornqvist, 2006). As such, it is no surprise that the ongoing P. australis dieback in the Lower MRD is attributed to complex interactions of multiple abiotic and biotic stressors, making identification of the causal agent(s) difficult (Cronin et al., 2020; Knight et al., 2020). While natural recolonization following dieback may occur, the rate of growth may be insufficient to revegetate vast regions of the MRD before soil erosion makes that impossible. Moreover, some areas of dieback, have been colonized by less desirable invasive and shallow-rooting or floating aquatic plants; e.g., water hyacinth (Pontederia crassipes (Mart.) Solms or elephant ear (Colocasia esculenta (L.) Schott) (Cronin et al., 2020).
Restoration using vegetation plantings is often designed to promote vertical accretion for the maintenance or building of marsh elevation (Hatton, DeLaune, & Patrick Jr., 1983; Bricker-Urso, Nixon, Cochran, Hirschberg, & Hunt, 1989; Nyman, DeLaune, Roberts, & Patrick, 1993; Chmura & Hung, 2004). Vertical accretion via plant growth involves mechanisms that promote the accumulation of organic matter, expansion of belowground root structures and sediment trapping via surface litter (Wolaver, Dame, Spurrier, & Miller, 1988; Craft, Seneca, & Broome, 1993; Nyman et al., 2006). Phragmites australis is adept at accreting sediments (Rooth & Stevenson, 2000; Kiviat, Meyerson, Mozdzer, Allen, Baldwin, Bhattarai, Brix, Caplan, Kettenring, Lambertini, Pysek, Weis, Whigham, & Cronin, 2019). Additionally, the typically dense clonal stands of P. australis are connected through their extensive belowground rhizome network which facilitate nutrient acquisition and can mitigate against some, but obviously not all, potential biological and physiological stress (Lissner & Schierup, 1997b).
Although much is known about the ability of the EU lineage of P. australis to invade and spread under a wide variety of marsh conditions (Chambers, Meyerson, & Saltonstall, 1999; Clevering, 1999; Saltonstall, 2002), relatively little is known about the Delta lineage whose distribution is limited to the MRD and surrounding areas (but see e.g., Hauber et al., 2011; Achenbach & Brix, 2014; Cronin et al., 2020). Our study clearly suggests that the Delta lineage would be the best choice for revegetating areas of dieback. Revegetation can begin shortly after the dieback event, despite some modest negative legacy effects mediated through changes in soil chemistry (Lee et al., 2023). Planting would need to take place in relatively shallow water, preferably under 0.5 m in depth. Revegetation of deeper-water areas will likely have to take place through growth and expansion of the planted material from shallow- to deeper-water areas (e.g., down a channel embankment).
To offset wetland loss in the MRD, The Beneficial Use of Dredged Material Program was authorized by the Water Resources Development Act (WRDA) of 2007 - Section 7006(d). Maintenance dredging of navigation channels has been used frequently over the years, with dredge material being deployed to restore degraded marshes and to create new marsh habitat (CPRA, 2017). Although dredge soils are deficient in nutrients and some metals (Lee et al., 2023), our experimental work has shown that all three lineages can grow on those soils, with only modestly lower growth rates than on undisturbed marsh soils (Lee et al., 2023). Our field observations confirm the natural colonization of those sites by P. australis. In addition, (Howard et al., 2020) demonstrated that transplanted P. australis to dredge sites could rapidly spread within two-years. In our current study, we had included one dredge site, Sawdust MC South, but the unexpected addition of new dredge sediments, caused the destruction of all of our plantings. Consequently, it remains an open question as to which P. australis lineages would do best on dredge soils. Finally, efforts to restore marsh habitat by building elevation through the deposition of dredge material and/or by revegetation of open areas cannot possibly keep up with the scale at which dieback is occurring in the MRD. However, these methods remain viable for high-risk (e.g., areas along channels that have high water flow) or high-value (e.g., near residential or commercial structures) areas.