| Literature DB >> 35425634 |
Johanna J Geeson1, Alistair J Hobday2, Cassie N Speakman1, John P Y Arnould1.
Abstract
Knowledge of factors affecting a species' breeding biology is crucial to understanding how environmental variability impacts population trajectories and enables predictions on how species may respond to global change. The Australian fur seal (Arctocephalus pusillus doriferus, AUFS) represents the largest marine predator biomass in southeastern Australia, an oceanic region experiencing rapid warming that will impact the abundance and distribution of prey. The present study (1997-2020) investigated breeding phenology and pup production in AUFS on Kanowna Island, northern Bass Strait. The pupping period varied by 11 days and the median pupping date by 8 days and were negatively correlated to 1- and 2-year lagged winter zonal winds, respectively, within Bass Strait. While there was no temporal trend over the study period, annual pup production (1386-2574 pups) was negatively correlated to 1-year lagged summer zonal winds in the Bonney Upwelling region and positively correlated to the current-year Southern Oscillation Index (SOI). In addition, a fecundity index (ratio of new-born pups to adult females at the median pupping date) was positively correlated with current-year Southern Annular Mode (SAM) conditions. Periods of positive SOI and positive SAM conditions are forecast to increase in coming decades, suggesting advantageous conditions for the Kanowna Island AUFS population.Entities:
Keywords: Bass Strait; Southern Annular Mode; Southern Oscillation Index; marine predator; phenology; pinniped
Year: 2022 PMID: 35425634 PMCID: PMC9006029 DOI: 10.1098/rsos.211399
Source DB: PubMed Journal: R Soc Open Sci ISSN: 2054-5703 Impact factor: 2.963
Figure 1Location of the Kanowna Island breeding colony study site (closed circle) within south eastern Australia, the influencing major water bodies and the Bonney Upwelling region. SAC: South Australian Current; EAC: East Australian Current; SASW: Sub-Antarctic Surface Waters. The shaded boxes labelled Bonney Upwelling (BU) and Bass Strait (BS) indicate the region for which local-scale environmental conditions were derived for BU and BS regions, respectively. Inset map shows the position of the region relative to Australia.
Local-scale environmental variables and broad-scale climate indices used in the analysis to investigate the environmental influences on breeding biology and pup production in Australian fur seals.
| variable | region | temporal scale | abbreviation | description |
|---|---|---|---|---|
| chlorophyll- | Bonney Upwelling | summer | Chl- | an indicator of primary productivitya |
| 1-year lagged | Chl- | |||
| 2-year lagged | Chl- | |||
| winter | Chl- | |||
| 1-year lagged | Chl- | |||
| 2-year lagged | Chl- | |||
| Bass Strait | summer | Chl- | ||
| 1-year lagged | Chl- | |||
| 2-year lagged | Chl- | |||
| winter | Chl- | |||
| 1-year lagged | Chl- | |||
| 2-year lagged | Chl- | |||
| SST | Bonney Upwelling | summer | SSTsummerBU | an indicator of the influence of different water bodies moving through the regionsb |
| 1-year lagged | SSTsummerBU Lag1 | |||
| 2-year lagged | SSTsummerBU Lag2 | |||
| Bass Strait | winter | SSTwinterBS | ||
| 1-year lagged | SSTwinterBS Lag1 | |||
| 2-year lagged | SSTwinterBS Lag2 | |||
| meridional wind component | Bonney Upwelling | summer | wind- | primary driver of water flow along the southern coast of Australiac |
| 1-year lagged | wind- | |||
| 2-year lagged | wind- | |||
| Bass Strait | winter | wind- | ||
| 1-year lagged | wind- | |||
| 2-year lagged | wind- | |||
| zonal wind component | Bonney Upwelling | summer | wind- | primary source of nutrients for the southern coast of Australiac |
| 1-year lagged | wind- | |||
| 2-year lagged | wind- | |||
| Bass Strait | winter | wind- | ||
| 1-year lagged | wind- | |||
| 2-year lagged | wind- | |||
| meridional GV | Bonney Upwelling | annual | GV- | a measure of ocean currents that may shift areas of primary productivity in the regionc |
| 1-year lagged | GV- | |||
| 2-year lagged | GV- | |||
| zonal GV | Bonney Upwelling | annual | GV- | |
| 1-year lagged | GV- | |||
| 2-year lagged | GV- | |||
| Indian Ocean Dipole | broad-scale | annual | IOD | a major weather and climate driver with influence across southern Australiad |
| 1-year lagged | IOD Lag1 | |||
| 2-year lagged | IOD Lag2 | |||
| Southern Annular Mode | broad-scale | annual | SAM | a major weather and climate driver with influence across Australiae |
| 1-year lagged | SAM Lag1 | |||
| 2-year lagged | SAM Lag2 | |||
| Southern Oscillation Index | broad-scale | annual | SOI | a major weather and climate driver with influence across southern Australia and a measure of El Niño and La Niña eventsf |
| 1-year lagged | SOI Lag1 | |||
| 2-year lagged | SOI Lag2 |
aThomalla et al. [62].
bWijffels et al. [63].
cSandery and Kampf [64].
dSaji et al. [65].
eLevenduski and Gruber [66].
fMiddleton et al. [67].
Most-likely models, in descending order, to explain the relationship between variations in pupping period, median pupping date, the IAPP, and the FI and inter-annual variation in environmental conditions. Only models with ΔAICc < 4 are shown and only the top 10 of those models are shown. LogLik, log-likelihood of the models; AICc, selection criteria; ΔAICc, the difference between the model's AICc and the minimum AICc value; AICc Wt, weight of Akaike's information criterion corrected for small sample sizes of the models; d.f., degrees of freedom of each model. Additional abbreviations as in table 1.
| candidate models | LogLik | AICc | ΔAICc | AICc Wt | DF |
|---|---|---|---|---|---|
| local-scale variables | |||||
| intercept + Chl- | −36.54 | 88.5 | 0.00 | 0.168 | 5 |
| intercept + Chl- | −38.68 | 88.7 | 0.16 | 0.155 | 4 |
| intercept + SSTwinterBS Lag1 + wind- | −39.38 | 90.1 | 1.55 | 0.078 | 4 |
| intercept + SSTsummerBU Lag2 | −41.21 | 90.3 | 1.73 | 0.071 | 3 |
| intercept + wind- | −41.25 | 90.4 | 1.81 | 0.068 | 3 |
| intercept + SSTwinterBS Lag1 | −41.32 | 90.5 | 1.96 | 0.063 | 3 |
| intercept | −42.94 | 90.7 | 2.19 | 0.056 | 2 |
| intercept + Chl- | −37.99 | 91.4 | 2.89 | 0.040 | 5 |
| intercept + SSTsummerBU Lag2 + wind- | −40.10 | 91.6 | 3.00 | 0.038 | 4 |
| intercept + Chl- | −42.10 | 92.0 | 3.50 | 0.029 | 3 |
| broad-scale variables | |||||
| intercept + IOD | −41.08 | 90.0 | 0.00 | 0.485 | 3 |
| intercept | −42.94 | 90.7 | 0.72 | 0.339 | 4 |
| intercept + SAM Lag2 | −42.76 | 93.4 | 3.36 | 0.091 | 4 |
| intercept + IOD + SAM Lag2 | −41.08 | 93.5 | 3.49 | 0.085 | 4 |
| local-scale variables | |||||
| intercept + wind- | −39.93 | 81.7 | 0.00 | 0.229 | 3 |
| intercept + wind- | −35.32 | 82.0 | 0.27 | 0.199 | 4 |
| intercept + wind- | −35.57 | 82.5 | 0.77 | 0.156 | 4 |
| intercept + wind- | −35.67 | 82.7 | 0.97 | 0.141 | 4 |
| intercept + wind- | −33.93 | 83.3 | 1.60 | 0.103 | 5 |
| intercept + wind- | −37.90 | 83.7 | 1.94 | 0.086 | 3 |
| intercept + wind- | −38.24 | 84.3 | 2.61 | 0.062 | 3 |
| broad-scale variables | |||||
| intercept + SOI Lag1 | −34.69 | 77.2 | 0.00 | 0.575 | 3 |
| intercept + SOI Lag1 + SOI Lag2 | −33.84 | 79.0 | 1.80 | 0.234 | 4 |
| intercept + IOD + SOI Lag1 | −34.38 | 80.1 | 2.87 | 0.137 | 4 |
| local-scale variables | |||||
| intercept + wind- | −146.5 | 303.7 | 0.00 | 0.696 | 4 |
| intercept + Chl- | −148.9 | 305.3 | 1.66 | 0.304 | 3 |
| broad-scale variables | |||||
| intercept + SOI + SOI Lag1 | −150.1 | 310.7 | 0.00 | 0.297 | 4 |
| intercept + SOI + IOD Lag2 | −150.3 | 311.0 | 0.28 | 0.259 | 4 |
| intercept + IOD Lag2 + SOI + SOI Lag1 | −148.7 | 311.3 | 0.59 | 0.222 | 5 |
| intercept + SOI | −152.1 | 311.7 | 1.01 | 0.180 | 3 |
| local-scale variables | |||||
| intercept + Chl- | 32.43 | −43.5 | 0.00 | 0.181 | 6 |
| intercept + Chl- | 29.65 | −43.3 | 0.22 | 0.162 | 5 |
| intercept + Chl- | 27.30 | −43.0 | 0.55 | 0.137 | 4 |
| intercept + Chl- | 27.20 | −42.8 | 0.76 | 0.123 | 4 |
| intercept + Chl- | 29.10 | −42.2 | 1.33 | 0.093 | 5 |
| intercept + Chl- | 24.71 | −41.4 | 2.11 | 0.063 | 3 |
| intercept + Chl- | 28.43 | −40.9 | 2.66 | 0.048 | 5 |
| intercept + Chl- | 27.96 | −39.9 | 3.59 | 0.030 | 5 |
| intercept + SSTsummerBU + wind- | 25.64 | −39.7 | 3.87 | 0.026 | 4 |
| broad-scale variables | |||||
| intercept + SAM | 24.94 | −41.9 | 0.00 | 0.597 | 3 |
| intercept + SAM + SOI Lag2 | 26.20 | −40.8 | 1.12 | 0.341 | 4 |
The 95% confidence intervals for the environmental influences on pupping period (PP), median pupping date (MPD), the IAPP and the FI based on model averaging. Italicized figures represent variables whose 95% unconditional confidence intervals did not cross zero. Additional abbreviations as in table 1.
| variable | PP | MPD | IAPP | FI | ||||
|---|---|---|---|---|---|---|---|---|
| lower | upper | lower | upper | lower | upper | lower | upper | |
| local-scale | ||||||||
| Chl- | −2.58 | 68.79 | −842.60 | 5705.00 | ||||
| SSTwinterBS Lag1 | −0.53 | 7.07 | ||||||
| wind- | −2.69 | 0.22 | ||||||
| SSTsummerBU Lag2 | −0.83 | 4.34 | ||||||
| wind- | ||||||||
| wind- | −3.08 | 0.28 | ||||||
| wind- | ||||||||
| wind- | −0.075 | 0.01 | ||||||
| Chl- | ||||||||
| SSTsummerBU | ||||||||
| wind- | −0.01 | 0.12 | ||||||
| broad-scale | ||||||||
| IOD | −0.79 | 14.44 | ||||||
| SAM Lag2 | −2.44 | 4.16 | ||||||
| SOI Lag1 | −22.79 | 409.40 | ||||||
| SOI Lag2 | −0.73 | 2.63 | −0.014 | 0.073 | ||||
| SOI | ||||||||
| IOD Lag2 | −116.80 | 1163.00 | ||||||
| SAM | ||||||||
Figure 2The relationship between the pupping period (days) of Australian fur seals and the environmental variable 2-year lagged winter zonal wind in the Bass Strait region (wind-uwinterBS Lag2). Blue shading shows the 95% CI.
Figure 3Relationships between the median pupping date (days after 31 October) of Australian fur seals at Kanowna Island, northern Bass Strait, and (a) 1-year lagged winter zonal wind from the Bass Strait region (Wind-uwinterBS Lag1) and (b) the 1-year lagged Southern Oscillation Index (SOI Lag1). Blue shading shows the 95% CI.
Figure 4Mean annual SOI for the study period 1997–2020 and IAPP for Australian fur seals at Kanowna Island (no data available for 1999 and 2001).
Figure 5Relationships between the IAPP in Australian fur seals at Kanowna Island, northern Bass Strait, and 1-year lagged summer zonal wind in the Bonney Upwelling region (wind-usummerBU Lag1) (a) and the SOI (b). Blue shading shows the 95% CI.
Figure 6Relationships between the FI of Australian fur seals at Kanowna Island, northern Bass Strait, and (a) summer Chlorophyll-a in the Bonney Upwelling area (Chl-asummerBU), (b) summer SST in the Bonney Upwelling area (SSTsummerBU) and (c) the SAM. Blue shading shows the 95% CI.