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ADJ SC 0.95 N/A 1.03 1.01 0.98 0.96 0.96 0.95 0.97 |
DIS CK 1.03 1.03 0.93 0.95 1.03 1.00 0.96 0.93 0.98 |
DIS BL 1.02 1.00 0.91 1.02 0.92 1.16 0.98 1.15 1.02 |
ADJ BP 1.00 0.93 0.97 1.19 0.94 .96 1.14 0.97 1.01 |
ADJ CP 1.02 1.05 1.05 1.04 0.96 0.96 1.06 0.98 1.01 |
DIS TP 0.92 1.03 N/A 0.96 0.97 1.06 0.96 0.92 0.97 |
Average 0.99 1.00 0.98 1.03 0.97 1.02 1.01 0.97 |
Std. Dev. 0.044 0.047 0.061 0.086 0.04 0.077 0.076 0.092 |
ADJ: Adjacent to canals, DIS: Distant from canals. |
https://doi.org/10.1371/journal.pone.0229147.t002 |
Resilience of seagrass communities exposed to pulsed freshwater discharges |
PLOS ONE | https://doi.org/10.1371/journal.pone.0229147 February 21, 2020 9 / 15 |
was 1.07 (SD± = 0.08), recorded during the 1985–1991 time step. The lowest λ recorded for |
adjacent sites was 0.95, displayed in 2003–2009. The lowest λ for distant sites was 0.92 recorded |
from 1950–1963. No significant differences in average λ were found between distant (mean λ |
= 0.99 (±0.07)) and adjacent sites (mean λ = 1.0 (±0.07)) (t-test, p>0.05). |
The stable population proportions determined by the eigenvectors showed that size-3 |
patches composed the highest, on average, proportion of the population at 0.38 when all sites |
are combined (Table 3). Size 1 had the next highest proportion at 0.23, with size 2 composing |
0.21 of the population. Sizes 4 and 5 had the lowest proportions with values of 0.12 and 0.05 |
respectively. |
Population projections and fragmentation scenarios |
All scenarios were run over 17, 5-year intervals. Low fragmentation and high fragmentation |
scenarios used a fragmentation rate of 0.8 and 10.2 patches created per existing patch, respectively. Low recruitment scenarios used a recruitment rate of 0.007 patches created per existing |
patch, average recruitment was 0.15 patches created per existing patch, and high recruitment |
was 0.6 patches created per existing patch. The stable size distribution for the high fragmentation/low recruitment scenario was 0.39, 0.43, 0.11, 0.01, and 0.06 for the respective size classes. |
The stable size distribution for the low fragmentation/low recruitment scenario was 0.06, 0.32, |
0.41, 0.11, and 0.10 for the respective size classes. The stable size distribution for the high fragmentation/average recruitment scenario was 0.55, 0.37, 0.01, 0.02, and 0.05 for the respective |
size classes. The stable size distribution for the low fragmentation/average recruitment site was |
0.21, 0.08, 0.33, 0.20, and 0.17 for the respective size classes. The stable size distribution for the |
high fragmentation/high recruitment scenario was 0.66, 0.29, 0.01, 0.01, and 0.03 for the |
respective size classes. The stable size distribution for the low fragmentation/high recruitment |
scenario was 0.27, 0.04, 0.32, 0.18, and 0.19 for the respective size classes. |
Scenarios were run with an initial population vector composed of 200 patches divided into |
48 (size 1), 56 (size 2), 72 (size 3), 17 (size 4), and 7 (size 5) patches based on the average conditions recorded in this study. SAV population abundance declined to near zero in the high fragmentation scenarios regardless of recruitment rates (Fig 4). In contrast, seagrass populations |
persisted under low fragmentation scenarios and abundances for the larger size classes (4 and |
5) increased as recruitment increases (Fig 4). |
Discussion |
Seagrasses around the world have experienced multiple disturbances that have resulted in |
accelerating rates of loss of these important coastal ecosystems [10, 34]. Within this worldwide |
Table 3. Proportion of the population (i.e., eigenvectors) composed by each seagrass patch size class over time averaged across the six sites. |
Time Step Size 1 Size 2 Size 3 Size 4 Size 5 |
1938–1944 0.11 0.20 0.45 0.17 0.06 |
1944–1953 0.27 0.20 0.37 0.12 0.05 |
1953–1963 0.23 0.20 0.42 0.10 0.07 |
1963–1973 0.22 0.19 0.42 0.10 0.07 |
1973–1985 0.16 0.24 0.36 0.17 0.07 |
1985–1991 0.31 0.23 0.33 0.09 0.04 |
1991–2003 0.31 0.21 0.38 0.07 0.03 |
2003–2008 0.25 0.23 0.32 0.17 0.04 |
Average (±STD) 0.23 (0.07) 0.21 (0.02) 0.38 (0.05) 0.12 (0.04) 0.05 (0.02) |
https://doi.org/10.1371/journal.pone.0229147.t003 |
Resilience of seagrass communities exposed to pulsed freshwater discharges |
PLOS ONE | https://doi.org/10.1371/journal.pone.0229147 February 21, 2020 10 / 15 |
context of degradation, nearshore habitats of Biscayne Bay have shown remarkable resilience, |
having experienced, on average, only < 4% declines in SAV cover over 70 years [23]. This limited decline is also noteworthy considering that the nearshore habitats of Biscayne Bay have |
been significantly modified over the past 5–6 decades by the construction of a canal system |
Fig 4. SAV patch abundance patterns over time simulated under high fragmentation (left panels) and low fragmentation (right panels) for (A, D) |
low recruitment, (B, E) average recruitment, and (C, F) high recruitment scenarios. |
https://doi.org/10.1371/journal.pone.0229147.g004 |
Resilience of seagrass communities exposed to pulsed freshwater discharges |
PLOS ONE | https://doi.org/10.1371/journal.pone.0229147 February 21, 2020 11 / 15 |
that has not only reduced the overall amount of fresh water reaching Biscayne Bay but also created large gradients in salinity [16, 35]. Our historical seascape and patch dynamic analyses |
shows that seagrass stability has not been greatly affected by these changes and that seagrass |
meadows appear to be both resistant and resilient to the modified salinity patterns. The fluctuation in lambda values documented, showing alternating periods of population decline with |
periods of population growth due to variable disturbance regimes, are further evidence of SAV |
resilience patterns in Biscayne Bay. |
While the limited historical loss of seagrasses cover documented here and previously by |
Santos et al. [23] is a positive result compared to the multiple reports of declines elsewhere, our |
patch-based seagrass population model developed based on the historical imagery showed that |
fluctuating salinity found near canals does have a negative impact through the fragmentation |
of seagrass meadows. Thus, even if seagrass habitats in Biscayne Bay have retained areal coverage, they are showing signs of salinity-driven fragmentation. Reports from other systems have |
shown that fragmented habitats are more susceptible to further disturbance and that they can |
decline rapidly [36–38]. Our simulation scenarios suggest that, under persistent high rates of |
fragmentation, seagrass populations may fall below a resistance threshold and decline rapidly |
thereafter. While recruitment of new seagrass patches through sexual or asexual reproduction |
may, to some extent, mitigate the impacts of high fragmentation, here we found that populations under simulated continuous high fragmentation scenarios can disappear within 50 years. |
This study is the first to quantify the patch dynamics of seagrass communities in South Florida and our seascape approach has revealed key aspects of how seagrass populations respond |
to differing environmental conditions. The mortality rate of seagrass patches was significantly |
affected by patch size, with the mortality rate of the smallest patches (57%) being an order of |
magnitude higher than that of the largest patches (< 5%). Similar size-based patterns of mortality were documented for corals and sponges, clonal/colonial taxa that also showed higher |
mortality of the smaller size classes [28, 39]. Smaller seagrass patches have been shown in other |
studies to have higher susceptibility to physical disturbances [25, 38]. The high mortality rate |
of smaller patches could be due to their lower biomass-to-perimeter ratio that may limit their |
anchoring capabilities as well as expose them to higher erosion rates along the patch perimeter |
[23]. Larger patches may have a more extensive root system with higher storage of belowground biomass that can help increase their resilience and lead to lower mortality rates. |
Considering the large difference in mortality rates among patch sizes, any shift in population structure that reduces mean patch size (e.g., fragmentation) would reduce the resilience of |
seagrass populations. This pattern was captured as output of our simulated scenarios that |
showed rapid population declines under high fragmentation scenarios. In Biscayne Bay, 94% |
of the seagrass patches created by fragmentation were produced by the two largest size classes. |
The stability in the cover of the seagrass meadows recorded over the 70-year period of record |
by Santos et al. [23], even when fragmentation rates were high in some time periods, is likely |
due to the fact that the larger patches were able to fragment and still remain within the large |
size classes that provide a size refuge against mortality. Continued fragmentation would, eventually, lead to a reduction in the abundance of these large and stable patch sizes, resulting in |
the population declines observed in our simulations. The persistence of the simulated seagrass |
populations was directly related to the fragmentation rates that affected the proportion and |
size distribution of patches. Under high fragmentation scenarios, the abundance of larger |
patches declined quickly. Without the source of new small patches through fragmentation as |
these larger patches decline, the populations disappeared within 50 years, regardless of recruitment rates. In contrast, under low fragmentation scenarios, the abundance of larger patches |
remains stable or even increases over time, leading to the persistence of the population. Thus, |
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