DMS emissions from the Arctic marginal ice zone - Archive ouverte HAL Accéder directement au contenu
Article Dans Une Revue Elementa: Science of the Anthropocene Année : 2021

DMS emissions from the Arctic marginal ice zone

Martí Galí
Martine Lizotte
  • Fonction : Auteur
David Kieber
  • Fonction : Auteur
Achim Randelhoff
Rachel Hussherr
  • Fonction : Auteur
Lei Xue
  • Fonction : Auteur
Julie Dinasquet
Eric Rehm
Maurice Levasseur
  • Fonction : Auteur

Résumé

Phytoplankton blooms in the Arctic marginal ice zone (MIZ) can be prolific dimethylsulfide (DMS) producers, thereby influencing regional aerosol formation and cloud radiative forcing. Here we describe the distribution of DMS and its precursor dimethylsulfoniopropionate (DMSP) across the Baffin Bay receding ice edge in early summer 2016. Overall, DMS and total DMSP (DMSPt) increased towards warmer waters of Atlantic origin concurrently with more advanced ice-melt and bloom stages. Relatively high DMS and DMSPt (medians of 6.3 and 70 nM, respectively) were observed in the surface layer (0–9 m depth), and very high values (reaching 74 and 524 nM, respectively) at the subsurface biomass maximum (15–30 m depth). Microscopic and pigment analyses indicated that subsurface DMS and DMSPt peaks were associated with Phaeocystis pouchetii, which bloomed in Atlantic-influenced waters and reached unprecedented biomass levels in Baffin Bay. In surface waters, DMS concentrations and DMS:DMSPt ratios were higher in the MIZ (medians of 12 nM and 0.15, respectively) than in fully ice-covered or ice-free conditions, potentially associated with enhanced phytoplanktonic DMSP release and bacterial DMSP cleavage (high dddP:dmdA gene ratios). Mean sea–air DMS fluxes (µmol m–2 d–1) increased from 0.3 in ice-covered waters to 10 in open waters (maximum of 26) owing to concurrent trends in near-surface DMS concentrations and physical drivers of gas exchange. Using remotely sensed sea-ice coverage and a compilation of sea–air DMS flux data, we estimated that the pan-Arctic DMS emission from the MIZ (EDMS, MIZ) was 5–13 Gg S yr–1. North of 80°N, EDMS, MIZ might have increased by around 10 ± 4% yr–1 between 2003 and 2014, likely exceeding open-water emissions in June and July. We conclude that EDMS, MIZ must be taken into account to evaluate plankton-climate feedbacks in the Arctic.
Fichier principal
Vignette du fichier
elementa.2020.00113.pdf (2.43 Mo) Télécharger le fichier
Origine : Fichiers éditeurs autorisés sur une archive ouverte

Dates et versions

hal-03458198 , version 1 (08-04-2022)

Licence

Paternité

Identifiants

Citer

Martí Galí, Martine Lizotte, David Kieber, Achim Randelhoff, Rachel Hussherr, et al.. DMS emissions from the Arctic marginal ice zone. Elementa: Science of the Anthropocene, 2021, 9 (1), ⟨10.1525/elementa.2020.00113⟩. ⟨hal-03458198⟩

Collections

INSU CNRS
51 Consultations
15 Téléchargements

Altmetric

Partager

Gmail Facebook X LinkedIn More