Derivation of Life History Tables
Here, we focus on the first year of life for the estimation of biomass at recruitment. Our protocol relies on comprehensive and detailed information of how fish size and mortality evolve throughout that first year of life (i.e., daily or, at most, weekly intervals). However, comprehensive records of species-specific measurements of growth and mortality rates during the first year of life directly obtained in the field are seldom available. Instead, where adequate information exists for model initialization and validation, detailed life history tables for the first year of life can be derived using well established equations. Life history tables assess how fin- and shellfish individual length, mass, and mortality rates change with individual age. The equations are different for larval and juvenile stages, and they are combined to provide estimates of daily growth (length) and mortality rates throughout the first year. Standard weight-length conversions are used as appropriate. Here, we utilize estimates of mortality rates (as per day) and individual fresh weight (as grams of fresh weight per individual) over daily time intervals throughout the first year of life. The derivation of these estimates is explained in Appendix 1 (for further elaboration see French McCay et al. 2015) and the actual estimates provided in Appendix 2.
Species Studied
Species with Derived Life History Tables
We have chosen two fish species as examples, pinfish (Lagodon rhomboides) and black drum (Pogonias cromis). Species-specific values for model initialization and validation to derive the life history tables are obtained from Nelson (2002) for pinfish and Murphy and Muller (1995) for black drum. These species represent fish that recruit to shallow parts of coastal ecosystems, where they reside through their pre-adult stage and subsequently migrate to deeper waters as they become adults. Numerous records of fish density in coastal waters exist for pinfish; however, the number of density records for black drum in coastal waters is drastically lower. Thus, this comparison allows us to gauge how our calculations fare for well vs. poorly reported density data sets.
Pinfish is a widespread species in coastal ecosystems extending from Massachusetts (although rare north of Maryland) to the Yucatan Peninsula, and to Bermuda, and the Gulf of Mexico (Muncy 1984). Juveniles typically reside in the shallow parts of coastal systems from late winter to late fall, pre-adults move to deeper waters of coastal systems, and adults move farther offshore. The species is not commercially harvested, but it serves as an important consumer of invertebrates (as juveniles) and plants (as large juveniles and adults; Hoss 1974, Stoner 1982), and as prey (both as juveniles and adults) for harvested fish species (Jordan et al. 1996, Nelson et al. 2013). Pinfish has been extensively studied and its density in coastal ecosystems along the Gulf of Mexico is well documented.
Black drum inhabits a wider geographical range than pinfish extending from the Bay of Fundy to the North Atlantic and Gulf coasts to the South Atlantic coast (Argentina) (Sutter et al. 1986). The species occur in coastal habitats along this range, and it is common in the Gulf of Mexico. Juveniles stay in the shallower parts of coastal ecosystems from mid spring to mid fall, pre-adults (typically up to 2 years old) reside in deeper areas of coastal waters, and adults may move to even deeper areas farther from the coastline (Osburn and Matlock 1984, Cody et al. 1985). The species plays significant trophic roles as prey and predator. In addition, it constitutes important commercial and recreational fisheries in the Gulf of Mexico (Leard et al. 1993). In spite of this, there are relatively few reports of density for this species in coastal ecosystems along the Gulf of Mexico.
Species Without Derived Life History Tables
We have chosen two invertebrate species as examples, the mud crab (Rhithropanopeus harrisii) and the Gulf stone crab (Menippe adina). Life history tables cannot be derived with rigor for these species since information to initialize and validate them is not available. These two species reside in shallow parts of coastal ecosystems throughout their entire life cycles. Density reports for the Gulf of Mexico are more numerous for the former species; thus, this comparison allows us to gauge how this second method fares with varying levels of density data availability.
Mud crabs are omnivorous scavengers and mostly feed on algae; small invertebrates such as amphipods, copepods, polychaetes and bivalves; seagrass detritus; and other dead organic matter. The frequency at which they feed and the quality of what they eat depend on the habitat and their diurnal cycle of activity and foraging (Hegele-Drywa and Normant 2009; Williams 1984). Mud crabs can be found in coastal environments throughout the northern hemisphere, and they are considered global invaders introduced through ballast waters and commercial oyster shipments.
Stone crabs occur on sediment bottoms, oyster reefs, and rock jetties in coastal ecosystems. Adults burrow in mud or sand while juveniles hide among rocks. Stone crabs are high-level predators in waters in the South Atlantic Bight, Caribbean (Western Atlantic stone crab, M. mercenaria), and northern and western Gulf of Mexico (Gulf stone crab, M. adina) (Williams and Felder 1986). Stone crabs are commercially fished in the southeastern United States and managed as one species (Gerhart and Bert 2008).
Density Data Set
The data used in this paper is part of an extensive data set of nekton abundance in shallow habitats of coastal ecosystems extending from Laguna Madre in southern Texas to the Caloosahatchee River in southern Florida presented in Hollweg et al. (2019). The compilation of the data set, including the databases searched, identity of the variables compiled, criteria applied for data selection, and how the data were extracted or calculated, is explained in detail in Hollweg et al. (2019). This is a companion paper in the Estuaries and Coasts special issue “Quantifying the Benefits of Estuarine Habitat Restoration in the Gulf of Mexico” organized by M. V. Carle and K. Benson. The data set contains mean density values, expressed in number of individuals per square meter of bottom, obtained for specific habitats and time periods as reported by the studies compiled. Here, we used density values compiled for pinfish, black drum, mud crab, and Gulf stone crab. Due to the shallow nature of the habitats included in the compilation and the life histories of these species, density estimates correspond to young of the year (YOY) for pinfish and black drum, and are inclusive of all ages for mud crabs and Gulf stone crabs.
At this point, it is important to emphasize that our protocol, both for the estimation of biomass at recruitment and productivity, can be applied to both temporary and permanent resident fin- and shellfish species in shallow coastal systems. For the estimation of biomass at recruitment, we focus on the first year of life, and thus, the density values used for this estimation must only represent YOY. This should be mostly the case for density data obtained for temporary resident species in shallow coastal systems, since most of the individuals of these species that occur in such shallow systems are YOY (such as the two examples used here, pinfish, and black drum). In contrast, density values obtained for permanent resident species in shallow coastal systems should include more life stages other than YOY. Thus, estimations of YOY density from the wider population density values obtained for permanent resident species in shallow coastal systems must be first carried out before deriving estimates of biomass at recruitment for these species using our protocol. Total population density values must be used in the estimation of productivity with our protocol, since those estimates correspond to the new biomass generated by all different species’ life cycle stages as they naturally occur in the system. For permanent resident species in shallow coastal systems, density values should include most life stages and such values can be used in the derivation of productivity estimates using our protocol. This is, however, not the case for density values of temporary resident species in shallow coastal waters, where efforts to estimate the fraction of life stages missing, and thereby produce density estimates that include all life stages within and out of the shallow coastal systems, are needed before deriving productivity estimates using our protocol.
The compiled density data for the four species targeted here (pinfish, black drum, mud crab and Gulf stone crab) included the following habitats: “near” submerged non-vegetated areas (within 5 m from fringing shoreline), “far” submerged non-vegetated areas (farther than 5 m from fringing shoreline), submerged aquatic vegetation (SAV), oyster reefs, and marshes. We divided the non-vegetated sites between “near” and “far” to account for shoreline edge effects (Peterson and Turner 1994, Minello and Rozas 2002). The primary intent of this paper is to demonstrate how our protocol can derive estimates of biomass at recruitment and productivity for fin- and shellfish species in coastal habitats. Additionally, we also suggest potential uses of these estimates such as comparisons across species and habitats with the ultimate goal of informing management decisions. The main purpose of such comparisons is to offer some illustrative examples of uses of our protocol, and thus, we have restricted the comparisons to natural habitats (i.e., habitats that were not ostensibly degraded by human activities and/or that had not been restored by humans) to keep the comparisons simple and consistent. Using our protocol for comparisons between natural and restored coastal systems is definitely a promising venue of work that should be explored in future efforts.
Density Meta-analysis and Corrections
We followed the meta-analytic approach presented in Hollweg et al. (2019). We summarize the steps of this approach and we refer the reader to Hollweg et al. (2019) for further consultation. First, following an imputation method, we estimated the standard error (SE) for the mean density values in the data set where it was not reported or we could not calculate it based on the information available in the paper. Briefly, we used the expected relationship between the sample mean and sample standard deviation (SD) to impute missing SE (Hilbe 2014). Sample SD was regressed against sample mean from the records compiled, and tests were conducted to ensure the regression obtained was robust (Quinn and Keough 2002). SD was estimated from the regression for records with sample mean but not SE provided. If the sample size was not reported, we set it to n = 1.
Second, we calculated a weighted average and associated SE for all density entries for the same species corresponding to the same combination of habitat, sampling time, and gear type using a fixed effect model:
$$ \mathrm{density}\ \mathrm{weighted}\ \mathrm{average}=\frac{\sum {w}_i{\mathrm{mean}}_i}{\sum {w}_i} $$
(1)
$$ {w}_i=\frac{1}{SE_i^2} $$
(2)
$$ {SE}_{\mathrm{density}\ \mathrm{weighted}\ \mathrm{average}}=\sqrt{\frac{1}{\sum {w}_i}} $$
(3)
where meani is the ith mean of a given combination of habitat, sampling time, and gear type, wi is the weight of the ith mean, SEi is the standard error of the ith mean, and SEdensity weighted average is the standard error of the density weighted average. In the calculation of wi, we did not include a random error term encompassing variability due to author bias (i.e., several entries generated by the same authors) or the inclusion of different populations for the same combination of habitat, sampling time, and gear type because we did not have a sufficiently large sample size in the four species targeted to test for such random effects with rigor (Hollweg et al. 2019).
Third, we applied correction factors for gear selectivity, capture efficiency, and recovery efficiency. Gear selectivity corresponds to the range of individual fish sizes that can be collected by the gear given its characteristics. Some gears do not normally capture fish smaller than a minimum or larger than a maximum size threshold (Minello and Rozas 2002, Baker and Minello 2011). Capture efficiency corresponds to the fraction of size-apt fish within the sampled area that are actually enclosed and captured by the gear. Indeed some fish that are within the catchable size range out-swim and escape the gear as it is being operated (Rozas and Minello 1997). Recovery efficiency corresponds to the fraction of captured fish that is actually recovered from the gear and processed. Not all captured fish are necessarily recovered, particularly in gears with a secondary removal method (Rozas and Minello 1997).
Given the individual size ranges included in the data set for the four species considered, and the minimum and maximum size thresholds of the gear types (enclosure, towed and passive) in the data set, selectivity corrections were only deemed necessary for black drum collections with enclosure-type gears. This is further elaborated in the “Results” section as we address each of the four species separately. In contrast, corrections for gear capture and recovery efficiency apply to all four species and gear types considered. Along with gear type, capture and recovery efficiency also depend on the habitat considered. Thus, we developed correction factors for capture and recovery efficiency for all combinations of habitats and gear types compiled in our data set. To do that, we carried out an extensive literature search and, for each combination of habitat and gear type in our data set, we derived a mean conversion factor and SE. We did this separately for capture and recovery efficiency. The procedure is detailed in Hollweg et al. (2019).
We then calculated overall gear efficiency for each combination of habitat and gear type as:
$$ {G}_{hg}={C}_{hg}{R}_{hg} $$
(4)
where Chg and Rhg are the capture and recovery efficiency for the hth habitat and gth gear type. The variance of Ghg was calculated using the equation reported by Goodman (1960) that provides an unbiased estimate of the exact formula of the variance of the product of two independent random variables:
$$ \hat{\mathit{\operatorname{var}}}\left({G}_{hg}\right)={R}_{hg}^2\hat{\mathit{\operatorname{var}}}\left({C}_{hg}\right)+{C}_{hg}^2\hat{\mathit{\operatorname{var}}}\left({R}_{hg}\right)-\hat{\mathit{\operatorname{var}}}\left({C}_{hg}\right)\hat{\mathit{\operatorname{var}}}\left({R}_{hg}\right) $$
(5)
The entire populations of the capture and recovery efficiency values for each combination of habitat and gear type are not known in their entirety and without uncertainty. Our efforts, as exhaustive as they may be, can only provide a number of values out of the entire populations of those values. Thus, the mean for capture and recovery efficiency and their variances are based on a limited sample and not on the entire population of values. Because of this, population moments need to be replaced by the corresponding sample moments, and the exact equation of the variance of the product of two independent random variables is converted into its unbiased estimate depicted in Eq. 5 (for further elaboration see Goodman 1960). The inevitably limited sample size in our calculations, as it is the often the case in ecological studies, implies that using the exact equation of the variance of the product of two independent random variables is not as accurate as using its unbiased approximation.
Overall gear efficiency for each combination of habitat and gear type was used to correct the density weighted averages for specific combinations of habitat, sampling time, and gear type:
$$ {D}_{ht}^G=\frac{\mathrm{density}\ \mathrm{weighted}\ \mathrm{average}}{G_{hg}} $$
(6)
where using the unbiased estimate of the exact formula of the variance of the product of two independent random variables reported by Goodman (1960):
$$ \hat{\mathit{\operatorname{var}}}\left({D}_{ht}^G\right)={\left(\frac{1}{G_{hg}}\right)}^2\hat{\mathit{\operatorname{var}}}\left(\mathrm{density}\ \mathrm{weighted}\ \mathrm{average}\right)+{\left(\mathrm{density}\ \mathrm{weighted}\ \mathrm{average}\right)}^2\hat{\mathit{\operatorname{var}}}\left(\frac{1}{G_{hg}}\right)-\hat{\mathit{\operatorname{var}}}\left(\mathrm{density}\ \mathrm{weighted}\ \mathrm{average}\right)\hat{\mathit{\operatorname{var}}}\left(\frac{1}{G_{hg}}\right) $$
(7)
and using the Delta method (Casella and Berger 2002):
$$ \hat{\mathit{\operatorname{var}}}\left(\frac{1}{G_{hg}}\right)={\left(\frac{1}{G_{hg}}\right)}^4\hat{\mathit{\operatorname{var}}}\left({G}_{hg}\right) $$
(8)
Subsequently, we averaged all the density values corrected for overall gear efficiency that corresponded to the same combination of habitat and sampling time (Dht):
$$ {D}_{ht}=\frac{1}{N_{ht}}\sum {D}_{ht}^G $$
(9)
and calculated its variance as:
$$ \hat{\mathit{\operatorname{var}}}\left({D}_{ht}\right)=\frac{1}{{N_{ht}}^2}\sum \hat{\mathit{\operatorname{var}}}\ \left({D}_{ht}^G\right) $$
(10)
where \( {D}_{ht}^G \) are the density values corrected for overall gear efficiency corresponding to the specific combination of habitat and sampling time, and Nht is the count (number) of such values. All these steps are common to our calculations of biomass at recruitment and productivity (Fig. 1).
Calculations of Biomass at Recruitment and Productivity
Calculations of Biomass at Recruitment
The next step for these calculations was, using life history tables, to estimate density at recruitment from values of mean density at a given sampling time post-recruitment (Fig. 1). The fraction of YOY present at the beginning of day 1 that remain alive at the end of the day (YOY1) corresponds to:
$$ {YOY}_1={e}^{-{m}_1} $$
(11)
where m1is the mortality rate for day 1 and is expressed in day−1. In turn, the fraction of YOY remaining after t days (YOYt) corresponds to:
$$ {YOY}_t=\prod \limits_{i=1}^t{e}^{-{m}_i}={YOY}_{t-1}{e}^{-{m}_t} $$
(12)
where mi is the mortality rate for day i, mt is the mortality rate for day t, and YOYt − 1 is the fraction of YOY present at the beginning of day 1 that remain alive at the end of day t-1. All mortality rates are expressed in day−1 and can be obtained as modeled values provided in the life history tables (see Appendix 2 for actual values).
Following this, the density at recruitment (DR) can be estimated from the density obtained at a sampling time post-recruitment (Dht) as:
$$ {D}_R={D}_{ht}\ \left(\raisebox{1ex}{$1$}\!\left/ \!\raisebox{-1ex}{${YOY}_t$}\right.\ \right) $$
(13)
where t covers the time span elapsed from recruitment to sampling. This procedure allowed us to derive a separate estimate of density at recruitment for each density value in the data set obtained at a later date as specified by the sampling time.
To estimate the variance of DR, we followed a multi-step process. The first step was to derive variance estimates for the daily mortality rates. To do this, we used the linear regression model provided by Bradford (1992):
$$ \mathit{\ln}\ \left(\mathit{\operatorname{var}}\left({m}_d\right)\right)=2.231\ \mathit{\ln}\ \left({m}_d\right)-1.893 $$
(14)
where md is the mean interannual daily mortality for day d, var (md) is the variance of the daily mortality values that compose the interannual mean, and ln denotes natural logarithm. The model was generated using a literature survey of mortality rates for egg, juvenile, and adult stages of marine, freshwater, and anadromous fish species. At least two values of daily mortality rates corresponding to different years were obtained for each species. The mean interannual daily mortality was calculated for each species, and after transformation to natural logarithms, the variance of the interannual daily mortality values was regressed against the mean (see Bradford 1992 for further details). Thus, this effort includes temporal variability in the estimates of variance for mortality rates, but it disregards other sources of variance such as spatial variability.
Thus:
$$ \hat{\mathit{\operatorname{var}}}\left({m}_d\right)=\exp \left(2.231\mathit{\ln}\left({m}_d\right)-1.893\right) $$
(15)
Then, the variance of the fraction of YOY present at the beginning of day d remaining at the end of the day (\( {e}^{-{m}_d} \)) can be derived using the Delta method (Casella and Berger 2002):
$$ \hat{\mathit{\operatorname{var}}}\left({e}^{-{m}_d}\right)=\hat{\mathit{\operatorname{var}}}\left({m}_d\right){e}^{-2{m}_d} $$
(16)
From this, we can calculate the variance of YOYt following an iterative process. The fraction of recruited YOY that remain alive at the end of day 2 (YOY2) corresponds to:
$$ {YOY}_2={e}^{-{m}_1}{e}^{-{m}_2} $$
(17)
where m1 and m2 are the mortality rates on day 1 and 2 respectively. The variance of this product can be estimated using the usual approximate formula for the variance of two dependent variables (Goodman 1960):
$$ \hat{\mathit{\operatorname{var}}}\left({YOY}_2\right)={e}^{-2{m}_2}\hat{\mathit{\operatorname{var}}}\left({e}^{-{m}_1}\right)+{e}^{-2{m}_1}\hat{\mathit{\operatorname{var}}}\left({e}^{-{m}_2}\right)+2{e}^{-{m}_1}{e}^{-{m}_2}\hat{\mathit{\operatorname{cov}}}\left({e}^{-{m}_1},{e}^{-{m}_2}\right) $$
(18)
where
$$ \hat{\mathit{\operatorname{cov}}}\left({e}^{-{m}_1},{e}^{-{m}_2}\right)=\hat{\rho}\sqrt{\hat{\mathit{\operatorname{var}}}\left({e}^{-{m}_1}\right)\hat{\mathit{\operatorname{var}}}\left({e}^{-{m}_2}\right)} $$
(19)
and \( \hat{\rho} \) is the estimated intra-class correlation for the cumulative remaining fraction of YOY.
We have chosen to use the usual approximate formula, and not the exact formula, for the variance of two dependent variables because the additional terms included in the exact formula not present in the approximate formula incur into complex derivatives that, while representing substantial effort, add relatively little to the magnitude of the calculation (see Goodman 1960).
Similarly, the fraction of recruited YOY that remain alive at the end of day 3 (YOY3) corresponds to:
$$ {\mathrm{YOY}}_3={\mathrm{YOY}}_2{e}^{-{m}_3} $$
(20)
and its variance:
$$ \hat{\mathit{\operatorname{var}}}\left({\mathrm{YOY}}_3\right)={e}^{-2{m}_3}\hat{\mathit{\operatorname{var}}}\left({\mathrm{YOY}}_2\right)+{\mathrm{YOY}}_2^2\hat{\mathit{\operatorname{var}}}\left({e}^{-{m}_3}\right)+2{\mathrm{YOY}}_2{e}^{-{m}_3}\ \hat{\mathit{\operatorname{cov}}}\left({\mathrm{YOY}}_2,{e}^{-{m}_3}\right) $$
(21)
Using this approach iteratively to YOY4, YOYt − 1 and finally to YOYt:
$$ \hat{\mathit{\operatorname{var}}}\left({\mathrm{YOY}}_t\right)={e}^{-2{m}_t}\hat{\mathit{\operatorname{var}}}\left({\mathrm{YOY}}_{t-1}\right)+{\mathrm{YOY}}_{t-1}^2\hat{\mathit{\operatorname{var}}}\left({e}^{-{m}_t}\right)+2{\mathrm{YOY}}_{t-1}\ {e}^{-{m}_t}\hat{\mathit{\operatorname{cov}}}\left(\ {\mathrm{YOY}}_{t-1},{e}^{-{m}_t}\right) $$
(22)
Subsequently, the variance of DR can be calculated by applying to Eq. 13 the expression reported by Goodman (1960) that provides an unbiased estimate of the exact formula of the variance of the product of two independent random variables:
$$ \hat{\mathit{\operatorname{var}}}\left({D}_R\right)={\left(\raisebox{1ex}{$1$}\!\left/ \!\raisebox{-1ex}{${\mathrm{YOY}}_t$}\right.\right)}^2\hat{\mathit{\operatorname{var}}}\left({D}_{ht}\right)+{D}_{ht}^2\hat{\mathit{\operatorname{var}}}\left(\raisebox{1ex}{$1$}\!\left/ \!\raisebox{-1ex}{${YOY}_t$}\right.\right)-\hat{\mathit{\operatorname{var}}}\left({D}_{ht}\right)\hat{\mathit{\operatorname{var}}}\left(\raisebox{1ex}{$1$}\!\left/ \!\raisebox{-1ex}{${\mathrm{YOY}}_t$}\right.\right) $$
(23)
where using the Delta method (Casella and Berger 2002):
$$ \hat{\mathit{\operatorname{var}}}\left(\raisebox{1ex}{$1$}\!\left/ \!\raisebox{-1ex}{${\mathrm{YOY}}_t$}\right.\right)={\left(\raisebox{1ex}{$1$}\!\left/ \!\raisebox{-1ex}{${\mathrm{YOY}}_t$}\right.\right)}^4\hat{\mathit{\operatorname{var}}}\left({\mathrm{YOY}}_t\right) $$
(24)
Finally, from the estimates of density at recruitment and their variances, we estimated a grand average of density at recruitment per habitat (DRH) and its variance as:
$$ {D}_{RH}=\frac{1}{N}\sum {D}_R $$
(25)
$$ \hat{\mathit{\operatorname{var}}}\left({D}_{RH}\right)=\frac{1}{N^2}\sum \hat{\mathit{\operatorname{var}}}\left({D}_R\right) $$
(26)
where DR is each of the estimates of density at recruitment for the given habitat, and N is the count of estimates in the habitat. Density estimates can be converted to biomass from knowledge of the mean individual fish weight at recruitment, which can be obtained from life history tables.
As indicated above, one of the main applications of our protocol is to allow for robust comparisons, or at least as robust as permitted by the size of the data sets available, of fin- and shellfish biomass across diverse shallow coastal habitats (i.e., SAV, oyster reefs, marshes, and non-vegetated bottoms). Such comparisons should be done for the same sampling time in all habitats; otherwise, temporal differences would confound the comparison and attribution of differences to habitat variability. If, rather than back-calculating to the time of recruitment, we had done comparisons across habitats with the same sampling time using the density data (or biomass after conversion from life history tables) directly reported in the data set, we would have been able to carry out only one comparison encompassing all habitats in the case of pinfish (i.e., month of May). All other comparisons for this species would have included three or four habitats, with different combinations of habitats for comparisons with the same number of habitats (for instance the comparison for July would encompass near non-vegetated, SAV, oyster reefs and marshes, and the comparison for October would encompass near non-vegetated, far non-vegetated, SAV and marshes, see Table 1). In the case of black drum, comparisons across habitats for the same sampling time would have involved at most three habitats, with many of them involving only two habitats (see Table 2).
Table 1 Pinfish: Density at sampling and SE; density at recruitment and SE back-calculated from the sampling month; overall density at recruitment per habitat and SE; and biomass at recruitment per habitat and SE. Density is in number of YOY per square meter of habitat, and biomass at recruitment is in gram DW per square meter of habitat. Biomass at recruitment has been derived by multiplying overall density at recruitment times the mean individual weight for YOY at that time (0.00198 g DW per individual) as reported in the life history tables for the species’ first year of life (Appendix 2; see text for more details). For these calculations, mean individual weight is considered constant Table 2 Black drum: Density at sampling and SE; density at recruitment and SE back-calculated from the sampling period; overall density at recruitment per habitat and SE; and biomass at recruitment per habitat and SE. Density is in number of YOY per square meter of habitat, and biomass at recruitment is in gram DW per square meter of habitat. Biomass at recruitment has been derived by multiplying overall density at recruitment times the mean individual weight for YOY at that time (0.000726 g DW per individual) as reported in the life history tables for the species’ first year of life (Appendix 2; see text for more details). For these calculations, mean individual weight is considered constant The problems of reducing the number of habitat types that can be compared with the same sampling time when using directly reported density data, and additionally having discrepant combinations of habitat types among comparisons involving the same number of habitat types, apply to most other species included in the Hollweg et al. (2019) density data set. To avert these problems, we have developed the protocol presented above. The protocol allows for the simultaneous inclusion of all sampling times into the cross-habitat comparison by providing back-calculations from any sampling time to a common time point, i.e., the time of recruitment. The protocol provides an integrated and coherent comparison of fin- and shellfish biomass across habitats by bringing together all sampling times in the data set to the same time point. We have chosen time at recruitment because of its ecological and management significance (i.e., appearance of new recruits and onset for their growth in shallow coastal systems). Importantly, we propagate the error involved in our calculations throughout the derivation process, such that the final estimates allow for sound comparisons across habitats where the certainty and robustness of the differences found can be well informed.
Calculations of Productivity
Our protocol for the derivation of productivity values relies on estimation of the P:B ratio (ratio of productivity to biomass) and subsequent multiplication by biomass. Derivation of productivity using the P:B ratio and biomass has been carried out in the literature for macro-invertebrates (Sprung 1993, Cusson and Bourget 2005) and fish (Waters 1977, Randall 2002). Here, we used an empirical model developed by Robertson (1979) for benthic macro-invertebrates that relates the species average P:B to its life span. The model corresponds to a linear regression fit using least-squares to the relationship between the base 10 logs of the two variables for 45 species of benthic macro-invertebrates including polychaetes, gastropods, bivalves, crustaceans, and echinoderms:
$$ {\mathit{\log}}_{10}\left(P:B\right)=0.660-0.726{\mathit{\log}}_{10}\left(\mathrm{Lifespan}\right) $$
(27)
In this equation, life span is expressed in years and ranges from 1.6 to 25.1 years. The P:B ratio is expressed in year−1 and ranges from 0.5 to 6.3 year−1. It is important to stress that P:B corresponds to the mean ratio for the species, that is a ratio that includes all individual age classes and represents the mean P:B that would be measured at a population level including simultaneously all the different species’ life cycle stages as they naturally occur in the system.
We can use the Robertson (1979) model to predict P:B from lifespan values for species of interest. Those predictions can be multiplied by mean biomass to derive estimates of productivity (Fig. 1). Thus, the uncertainty in these productivity estimates comes from the uncertainty in the predicted P:B values and the uncertainty in the mean biomass. To derive the predicted P:B value, we inputted the lifespan for the species of interest in the equation above and solved for P:B. The entry corresponds to a species not included in the initial regression in Robertson (1979), and thus, the predicted P:B value for the entered lifespan is determined by the overall functional association between life span, body size and turnover rate across species (Brown et al. 2004), on the one hand, and idiosyncratic, species-specific variability in such functional association on the other. Therefore, we estimated the uncertainty of this prediction as the variance associated with a predicted single value of the dependent variable from a given value of the independent variable in the linear regression model (and not as the predicted mean value of the dependent variable for a given value of the independent variable, Neter et al. 1996). This variance \( \left({\hat{\mathit{\operatorname{var}}}}_{\hat{Y}\ \mathrm{single}}\right) \) corresponds to:
$$ {\hat{\mathit{\operatorname{var}}}}_{\hat{Y}\ \mathrm{single}}= MSE\left(1+\frac{1}{n}+\frac{{\left({x}^{\ast }-\overline{x}\right)}^2}{S_{xx}}\right) $$
(28)
where MSE is the mean squared error from the model fit, n is the number of paired observations in the regression, x∗is the specific value of the independent variable for which we seek the predicted value of the dependent variable, \( \overline{x} \) is the mean for all the values of the independent variable used to obtain the regression fit, and Sxx is the sum of squares of the independent variable. Since we used a regression model with base 10 log variables, the variance derived in this way corresponded to \( \hat{\mathit{\operatorname{var}}}{\log}_{10}\left(P:B\right).\kern0.5em \)We used the Delta method (Casella and Berger 2002) to calculate \( \hat{\mathit{\operatorname{var}}}\ P:B \):
$$ \hat{\mathit{\operatorname{var}}}\ P:B=\hat{\mathit{\operatorname{var}}}{\mathit{\log}}_{10}\left(P:B\right)\ {\left(P:B\ \mathit{\ln}10\right)}^2 $$
(29)
where ln10 denotes the natural logarithm of 10, and P:B is the back transformed value of the predicted log10(P : B):
$$ P:B={10}^{\log_{10}\left(P:B\right)} $$
(30)
To derive mean biomass and its variance by habitat, we first estimated the mean density and its variance in the specific habitat (Fig. 1). Estimates of mean density came from a two-step process. First, we pooled all density values corrected for overall gear efficiency corresponding to the same combination of habitat and sampling time, i.e., we derived Dht from \( {D}_{ht}^G \), and \( \hat{\mathit{\operatorname{var}}}\left({D}_{ht}\right) \) from \( \hat{\mathit{\operatorname{var}}}\ \left({D}_{ht}^G\right) \) as explained in Eqs. 9 and 10. Second, we estimated the grand average density (DH) and its variance \( \left(\hat{\mathit{\operatorname{var}}}\left({D}_H\right)\right) \) per habitat by pooling all the sampling times within the specific habitat:
$$ {\mathrm{D}}_H=\frac{1}{N_t}\sum {D}_{ht} $$
(31)
$$ \hat{\mathit{\operatorname{var}}}\left({\mathrm{D}}_H\right)=\frac{1}{{N_t}^2}\sum \hat{\mathit{\operatorname{var}}}\left({D}_{ht}\right) $$
(32)
where Nt is the number of sampling times in the habitat. The purpose was to obtain a mean biomass value for the population that includes all individual age classes, or at least as many as possible, as they naturally occur. Thus, by first averaging all density values corrected for overall gear efficiency corresponding to the same combination of habitat and sampling time, this approach helps to reduce overweighting our final estimates with specific sampling times that could under- or over-represent certain age classes.
We then derived estimates of mean biomass per habitat (BH) as the product between DH and mean individual weight (IW), with the latter also encompassing all size classes. Values of IWand its variance were obtained from the literature. We calculated the variance of BH using the equation reported by Goodman (1960) that provides an unbiased estimate of the exact formula of the variance of the product of two independent random variables:
$$ \hat{\mathit{\operatorname{var}}}\left({B}_H\right)={IW}^2\hat{\mathit{\operatorname{var}}}\left({D}_H\right)+{D}_H^2\hat{\mathit{\operatorname{var}}}(IW)-\hat{\mathit{\operatorname{var}}}\left({D}_H\right)\hat{\mathit{\operatorname{var}}}(IW) $$
(33)
where values and variance of DH and BH are specific to the habitat, and the value and variance of IW are applied uniformly to all habitats. Finally, we derived estimates of mean productivity per habitat (PH) as the product between BH and P:B, and its variance as (Goodman 1960):
$$ \hat{\mathit{\operatorname{var}}}\ \left({P}_H\right)={\left(P:B\right)}^2\ \hat{\mathit{\operatorname{var}}}\ \left({B}_H\right)+{B}_H^2\hat{\mathit{\operatorname{var}}}\ \left(P:B\right)-\hat{\mathit{\operatorname{var}}}\ \left({B}_H\right)\ \hat{\mathit{\operatorname{var}}}\ \left(P:B\right) $$
(34)
where the value and variance of the predicted P:B is applied uniformly to all habitats.