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            <gco:CharacterString>Biodiversity patterns under a shifting baseline: Sensitive fish species core areas (Aim 1) 2024</gco:CharacterString>
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        <gco:CharacterString>The dataset contains outputs from Aim 1 in Bluemel et al. 2024 - Biodiversity 
patterns under a shifting baseline: important areas for sensitive fish species 
and ecosystem functioning to assist marine spatial planning (see attached), 
Cefas Project Report for Defra, 40 pp. The dataset includes regional 
core-areas (persistent areas of high fish population density) and projected 
spatial changes in the distribution of sensitive fish species (currently and 
under future environmental change) for nine focal species, including the 
common skate complex (Dipturus spp.), spurdog (Squalus acanthias), tope 
(Galeorhinus galeus), spotted ray (Raja montagui), undulate ray (Raja 
undulata), starry ray (Amblyraja radiata), John Dory (Zeus faber), Atlantic 
wolffish (Anarhichas lupus) and Atlantic halibut (Hippoglossus hippoglossus).

Historic core areas / home ranges: vectors of historic core-areas (persistent 
areas of high fish population density) and home ranges of the nine focal 
species derived from standardised trawl data (survey catch-rates expressed in 
terms of biomass per area swept by the trawl, kg.km2) from long-term 
fishery-independent monitoring programmes (Lynam &amp; Ribeiro 2022a). Where 
available, core areas were defined for each decade (1985 – 1994; 1995 – 2004; 
2005 – 2014) where 50% of the population’s kernel density was concentrated. 
Similarly, the species range was defined as the areas containing 95% of the 
population’s kernel density. NB, there are no historic core areas available 
for tope.

Species distributions: contains gridded rasters of the raw predicted habitat 
suitability projections from the Bayesian Additive Regression Trees (BART, 
Chipman et al., 2010) modeling algorithm for the nine fish species for the 
model training/current day period 2005 – 2014 ('Training') and expected 
habitat suitability for a species given future environmental conditions in 
2050 (climate projection representative concentration pathway (RCP) 4.5 
(medium emissions, high mitigation)) ('RCP4.5_2050').

Current core areas: contains vectors of current core-areas of the nine focal 
species derived from the expected habitat, based on a novel thresholding 
approach tailored to the projections of each species distribution model (SDM) 
by outcomes from the spatial analysis of survey-derived biomass. 

Future core areas under rcp4.5 emissions scenario in 2050: contains vectors of 
future core-areas of the nine focal species derived from the expected habitat, 
based on a novel thresholding approach tailored to the projections of each SDM 
by outcomes from the spatial analysis of survey-derived biomass. NB, no future 
core area is predicted for starry ray under this emissions scenario.

The spatial reference for all data is WGS84/UTM zone 30N (EPSG:32630)</gco:CharacterString>
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            <gco:CharacterString>Spatial analysis of core areas derived from observations:

Standardised trawl data (survey catch-rates expressed in terms of biomass per 
area swept by the trawl, kg.km2) from long-term fishery-independent 
monitoring programmes (Lynam &amp; Ribeiro 2022a) were used to delineate spatial 
changes in populations of the focal species. Survey catch rates are generally 
low for sensitive species in comparison to commercial stocks, so data were 
grouped by decadal time interval to ensure that analyses of change in the 
spatial distribution and core areas were representative for rarer species. The 
three decadal time periods investigated were: 1985 – 1994; 1995 – 2004; 2005 – 
2014; with the latter decade matching the period for which data were subset 
prior to modelling species habitats.

Due to the varying spatial coverage and temporal extent of scientific surveys 
investigated, we selected for analyses those surveys that offered a 
combination of the longest time series, largest extent, and highest catches of 
the focal species (given a minimum of 50 records of occurrence between 2005 – 
2014). For species occurring predominantly in the North Sea (i.e. wolfish 
*A. lupus, *halibut *H. hippoglossus *and* *starry ray* A. radiata*), 
we combined the ICES co-ordinated international bottom trawl surveys from 
quarter one (Q1) with those in Q3 (GNSIntOT1: 1983 - 2020 and GNSIntOT3: 1998 
- 2020, respectively). For undulate ray *R. undulata, *which predominantly 
occurs in the English Channel, the French otter trawl survey conducted in Q4 
(GNSFraOT4: 1998 - 2020) was used. For species widely distributed across the 
Celtic Seas ecoregion, we combined the Scottish otter trawl surveys conducted 
in Q1 and Q4 (CSScoOT1: 1985 – 2020 and CSScoOT4: 1997 – 2020, respectively), 
except for tope *G. galeus* as there were very few records of tope in the 
Scottish surveys. The Irish otter trawl survey conducted in Q4 (CSIreOT4: 2003 
– 2020) had the highest occurrence of tope across all surveys between 2005 – 
2014, but the time series was limited to only a single decade. For 
consistency, data from selected surveys was cropped to the spatial extent of 
the SDMs (excluding parts of the Skagerrak and Kattegat from the North Sea 
surveys).

Changes in the ranges and core areas of species were calculated using the 
spatial kernel density function, weighted by biomass, using gaussian kernels 
and default bandwidths in the spatialEco package v2.0-2 (Evans et al. 2023) in 
R v4.3.2 (R Core Team, 2023). Core areas were defined for each decade where 
50% of the population’s kernel density was concentrated. Similarly, the 
species range was defined as the areas containing 95% of the population’s 
kernel density. Additionally, biomass-weighted population centroids (i.e. the 
geometric centres of each population) were also calculated with spatialEco to 
identify any historic shifts in the species distribution, since the mid-1980s 
and within the survey extent.

Projecting future core areas:

To project changes in core areas of sensitive fish species under future 
environmental conditions, we combined the core areas defined from survey 
biomass with projections from a Species Distribution Model (SDM). These models 
determine a “climatic envelope” encompassing suitable environmental conditions 
for a species by examining environmental data in areas where the species is 
present or absent.

Species occurrences were sourced from fisheries-independent groundfish survey 
datasets from the Northeast Atlantic (Lynam &amp; Ribeiro 2022a,b). Additional 
records from the early years (2006 – 2014) of the quarter one southwest beam 
trawl survey (for ICES area 7.e that were not included in the data products) 
were sourced from the Cefas Survey System database (FSS code Q1SWBEAM). 
Additional Spanish groundfish survey data not included in the aggregated 
dataset was provided by Francisco Velasco at the Spanish Institute of 
Oceanography. Data were also sourced from the Cefas English and Welsh Observer 
Programme, which samples catches and discards from English and Welsh 
registered fishing vessels. For elasmobranchs, the dataset was supplemented 
with observations from the Ocean Biogeographic Information System (OBIS; 
Grassle, 2000; OBIS, 2021) and from the Global Biodiversity Information 
Facility (GBIF, 2021).

The data for each species were plotted and checked visually for 
inconsistencies, with duplicate records removed (where occurrence records had 
been included within multiple data sources). Species occurrence data from 2005 
to 2014 was used to train the Species Distribution Models (SDM) (matching the 
2005 to 2014 time period of the environmental data) and projected onto a 
0.125° x 0.125° study grid. Grid cells with distribution data were classified 
as “presence” sites and the remaining cells “pseudo-absence” sites. Absence 
records from scientific trawls were not considered true absences due to the 
likelihood of under-sampling and potential for false negatives for some rarer 
species.

Models were trained using Bayesian Additive Regression Trees (BART; Chipman et 
al., 2010). BART is a technique based on an ensemble of classification tree 
models, each built by sequentially splitting the data in two groups based on 
the value of the explanatory variables, with the aim to separate presence and 
absence sites. For further technical details of the BART modelling process, 
environmental data layers used (including bathymetry, sea surface temperature 
and salinity, difference between surface and bottom temperature, surface 
chlorophyll, median grain size, and gravel and sand percentage), and model 
validation, refer to section 4.8 in Astarloa et al., 2023). Once trained, the 
BART models were used to project expected habitat suitability for a species 
given future environmental conditions. The future climate projections used 
correspond to the “representative concentration pathway” (RCP) 4.5 (medium 
emissions, high mitigation) projections from the Intergovernmental Panel on 
Climate Change (IPCC)'s fifth phase of the Coupled Model Intercomparison 
Project (CMIP5) RCP dataset. They were produced using the POLCOMS-ERSEM 
coupled model running at a 10 km resolution, underpinned by the global climate 
model MPI-ESM-LR (Kay et al., 2018; available from Copernicus Climate Data 
Store, Kay 2020).

Future core areas were defined from the expected habitat, based on a novel 
thresholding approach tailored to the projections of each SDM by outcomes from 
the spatial analysis of survey-derived biomass. First, were plotted the 
biomass-derived core area for the period 2005 – 2014 (hereafter “biomass-CA”) 
for the selected survey per species overlaid with the SDM computed for the 
same decade for the same species. In each case we observed that the 
biomass-CAs overlapped with areas of high projected habitat suitability, but 
not perfectly so. Biomass-CAs also typically extended beyond modelled areas of 
(i.e., into areas of lower habitat suitability adjacent to high suitability 
areas). We sought a threshold value for modelled habitat suitability so that 
model grid cells with suitability above this value could be described as core 
for the species in a similar way to the biomass-CA. To maintain consistency 
with the biomass-CA, we sought to capture ≥ 90% of the cells that occur within 
the biomass-CA within the SDM-derived core area. This was achieved by 
determining a threshold value that captured the modelled areas of high habitat 
suitability with an additional spatial buffer to ensure any adjacent, 
sub-optimal habitats that were contained within the biomass-CA were also 
included (buffered until at least 90% of the biomass-CA was incorporated).

To define the species-specific threshold and spatial buffer that encompassed ≥ 
90% of the biomass-CA, we first extracted the modelled habitat suitability 
values at locations with known species occurrence ordered from low to high 
suitability and calculated the percentiles of suitability values in increments 
of 0.05. We then used each of these percentiles as model thresholds with a 
range of buffers (from 50km to 200km in increments of 50) to determine the 
spatial extent of the resulting core area. We selected the combination that 
included the highest percentile (i.e., containing the highest possible 
probability values from the model) with the smallest buffer to ensure ≥ 90% of 
the biomass-CA was incorporated with minimal spatial smoothing.

To check the consistency of these modelled-derived core areas beyond the 
selected survey extent, we examined the percentage overlap of biomass-CAs 
derived from other surveys (for those surveys that contained &gt; 50 records of 
the species between 2005 – 2014) and when combining data from all surveys that 
used Grand Ouverture Verticale (GOV) trawls (i.e., not accounting for 
potential survey and/or vessel effects or spatio-temporal variation) for all 
quarters between 2005 – 2014.

For each species, the final threshold and buffer were applied to the SDM 
projections for the 2005 – 2014 model training period and the RCP4.5 
projection in 2050 to determine any changes between current and future core 
areas.</gco:CharacterString>
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