4.7 Article

Influence of environmental variability and Emiliania huxleyi ecotypes on alkenone-derived temperature reconstructions in the subantarctic Southern Ocean

Journal

SCIENCE OF THE TOTAL ENVIRONMENT
Volume 812, Issue -, Pages -

Publisher

ELSEVIER
DOI: 10.1016/j.scitotenv.2021.152474

Keywords

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Funding

  1. European Union's Horizon 2020 research and innovation programme under the Marie Sklodowska-Curie grant [748690]
  2. Spanish Ministerio de Economia y Competitividad [CGL2015-68459-P]
  3. Portuguese national funds from FCT - Foundation for Science and Technology [UIDB/04326/2020]
  4. Portuguese national funds from operational programme CRESC Algarve 2020 [ALG-01-0145-FEDER-022121, POCI-01-0145-FEDER-022157]
  5. Portuguese national funds from operational programme COMPETE 2020 [ALG-01-0145-FEDER-022121, POCI-01-0145-FEDER-022157]
  6. [CEX2018-000794-S]
  7. [MCIN/AEI/10.13039/501100011033]
  8. Marie Curie Actions (MSCA) [748690] Funding Source: Marie Curie Actions (MSCA)

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Long-chain unsaturated alkenones produced by haptophyte algae are widely used as paleotemperature indicators, but complicating factors in the Southern Ocean, including the dominance of E. huxleyi var. aurorae, may impact the accuracy of alkenone-based SST reconstructions.
Long-chain unsaturated alkenones produced by haptophyte algae are widely used as paleotemperature indicators. The unsaturation relationship to temperature is linear at mid-latitudes, however, non-linear responses detected in subpolar regions of both hemispheres have suggested complicating factors in these environments. To assess the influence of biotic and abiotic factors in alkenone production and preservation in the Subantarctic Zone, alkenone fluxes were quantified in three vertically-moored sediment traps deployed at the SOTS observatory (140 degrees E, 47 degrees S) during a year. Alkenone fluxes were compared with coccolithophore assemblages, satellite measurements and surface-water properties obtained by sensors at SOTS. Alkenone-based temperature reconstructions generally mirrored the seasonal variations of SSTs, except for late winter when significant deviations were observed (3-10 degrees C). Annual flux-weighted averages in the 3800 m trap returned alkenone-derived temperatures similar to 1.5 degrees C warmer than those derived from the 1000 m trap, a distortion attributed to surface production and signal preservation during its transit through the water column. Notably, changes in the relative abundance of E. huxleyi var. huxleyi were positively correlated with temperature deviations between the alkenone-derived temperatures and in situ SSTs (r = 0.6 and 0.7 at 1000 and 2000 m, respectively), while E. huxleyi var. aurorae, displayed an opposite trend. Our results suggest that E. huxleyi var. aurorae produces a higher proportion of C-37:3 relative to C-37:2 compared to its counterparts. Therefore, the dom-inance of var. aurorae south of the Subtropical Front could be at least partially responsible for the less accurate alkenone-based SST reconstructions in the Southern Ocean using global calibrations. However, the observed correla-tions were largely influenced by the samples collected during winter, a period characterized by low particle fluxes and slow sinking rates. Thus, it is likely that other factors such as selective degradation of the most unsaturated alkenones could also account for the deviations of the alkenone paleothermometer.

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