Public KRILLBASE data support a southward shift of SW Atlantic krill since 1926-1939, but the reported 1400 km south-west shift depends on cells with one or two cruise-seasons
Atkinson et al. (2021) reported that the centre of gravity (CoG) of post-larval Antarctic krill in the SW Atlantic moved about 1400 km south-west from 1926-1939 to 1996-2016, mostly after 1976-1995. They gave no uncertainty interval. We applied their comparable-cell method to the public 2016 KRILLBASE-abundance release (standardised net-haul densities, 2 x 5 degree cells sampled in all three eras). The result agreed with the published value: 43 cells and 1398 km. We then resampled whole cruise-seasons, removed single cruise-seasons and cells, used robust cell summaries, and kept only well-sampled cells. With all cells, the southward component was resolved: 631 km (95% cruise-season bootstrap interval 383-783 km). The total distance was very uncertain (507-1729 km). In 23 of the 43 cells, one era has data from only one or two cruise-seasons. With the 20 cells that have at least 3 cruise-seasons in every era, the shift was 654 km (249-1250). The westward component fell from 22.4 to 8.1 degrees of longitude, and its interval included zero. The southward component stayed resolved (456 km, 201-738). One 1976 cruise-season is the only 1976-1995 source in eight cells. If we remove it, the westward shift after 1976-1995 decreases from 25.1 to 11.0 degrees. In well-sampled cells, the southward shift after 1976-1995 was not resolved (315 km, -8 to 586). A Tweedie GLM with cell fixed effects gave a 68% decrease in density after 1976-1995 (95% CI 37-84%). Its north-south difference had the sign of a contraction but was not resolved. Limitations: one method, public data that differ slightly from the authors' screened set, no larval data, and no propagation of the standardisation uncertainty. The data support a southward shift of several hundred kilometres, but not a resolved 1000-1400 km south-west jump after the 1990s.
Antarctic krill · Euphausia superba · KRILLBASE · range shift · centre of gravity · cluster bootstrap · Southern Ocean · Scotia Sea · sampling bias · reanalysis
References
8- usesdoi:10.5285/8b00a915-94e3-4a04-a903-dd4956346439
KRILLBASE-abundance 2016 public release; the source of all krill densities.
- usesdoi:10.5194/essd-9-193-2017
Describes KRILLBASE and the density standardisation that we use.
- challengesdoi:10.1111/gcb.16009
We reproduce its centre-of-gravity method (1398 km against the reported 1400 km) and show that the distance and the timing after 1976-1995 depend on thinly sampled cells and one cruise-season. The southward component is supported.
- doi:10.1038/s41558-018-0370-z
Original report of the southward contraction; same era boundaries.
- doi:10.1093/jcbiol/ruy072
Earlier re-analysis of KRILLBASE density trends (no decline 1976-2016).
- doi:10.1093/jcbiol/ruz004
Reply that supports the decline.
- doi:10.1093/jcbiol/ruz010
Response in the density-trend debate.
- doi:10.3389/fmars.2024.1307402
Discusses how sampling scale affects detection of krill change.
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