Table 1.
Moran’s I by distance (km)a |
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Layer | Abbrev | Min | Max | Mean | Standard deviation | Units | 25 | 50 | 100 | 200 | 500 | Data source | |
Mean sea surface temperature | SST | 2.197 | 19.859 | 10.600 | 2.916 | °C | 0.66 | 0.60 | 0.50 | 0.39 | 0.26 | NOAA | |
Standard deviation of sea surface temperature | sdSST | 1.201 | 8.211 | 3.587 | 1.595 | °C | 0.74 | 0.69 | 0.63 | 0.58 | 0.47 | NOAA | |
Mean thermal stress frequency | TSF | 0.00 | 22.00 | 1.10 | 0.84 | freqencyb | 0.45 | 0.39 | 0.30 | 0.23 | 0.15 | CoRTAD | |
Mean sea surface salinity | SSS | 2.108 | 36.524 | 29.928 | 10.607 | unitlessc | 0.72 | 0.64 | 0.57 | 0.51 | 0.37 | World Ocean Atlas 2013 v2 | |
Mean net primary productivity | NPP | 478 | 12,788 | 2,063 | 1697 | C m−2 day−1 | 0.73 | 0.62 | 0.52 | 0.44 | 0.35 | Ocean Productivity web | |
Standard deviation of net primary productivity | sdNPP | 276 | 15,945 | 3,521 | 3,080 | C m−2 day−2 | 0.76 | 0.67 | 0.59 | 0.52 | 0.39 | Ocean Productivity web | |
Bathymetry | BATH | −5,029 | 839 | −266 | 654 | Metres | 0.86 | 0.71 | 0.45 | 0.30 | 0.17 | ETOPO1 | |
Habitat exposure during Pleistocene low sea level stands | PLEIS | 0.000 | 1.000 | 0.398 | 0.297 | unitlessc | 1.00 | 0.99 | 0.98 | 0.87 | 0.35 | Derived from ETOPO1 |
aMoran’s I is a measure of spatial autocorrelation and can range from −1 (complete negative spatial autocorrelation) to +1 (complete positive spatial autocorrelation). Values were estimated from 10,000 random points and values above 0.70 (high spatial autocorrelation) are in bold.
bMean frequency of thermal stress anomalies ≥ 1 °C over the previous 52 weeks.
cSSS: g/kg seawater; PLEIS: proportion.