Publications des scientifiques de l'IRD

Assuncao R., Lebourges Dhaussy Anne, da Silva A. C., Roudaut Gildas, Ariza A., Eduardo L. N., Queiroz S., Bertrand Arnaud. (2023). Fine-scale vertical relationships between environmental conditions and sound scattering layers in the Southwestern Tropical Atlantic. PLoS One, 18 (8), [24 p.]. ISSN 1932-6203.

Titre du document
Fine-scale vertical relationships between environmental conditions and sound scattering layers in the Southwestern Tropical Atlantic
Année de publication
2023
Type de document
Article référencé dans le Web of Science WOS:001043329800034
Auteurs
Assuncao R., Lebourges Dhaussy Anne, da Silva A. C., Roudaut Gildas, Ariza A., Eduardo L. N., Queiroz S., Bertrand Arnaud
Source
PLoS One, 2023, 18 (8), [24 p.] ISSN 1932-6203
Ocean dynamics initiate the structure of nutrient income driving primary producers, and these, in turn, shape the distribution of subsequent trophic levels until the whole pelagic community reflects the physicochemical structure of the ocean. Despite the importance of bottom-up structuring in pelagic ecosystems, fine-scale studies of biophysical interactions along depth are scarce and challenging. To improve our understanding of such relationships, we analyzed the vertical structure of key oceanographic variables along with the distribution of acoustic biomass from multi-frequency acoustic data (38, 70, and 120 kHz) as a reference for pelagic fauna. In addition, we took advantage of species distribution databases collected at the same time to provide further interpretation. The study was performed in the Southwestern Tropical Atlantic of northeast Brazil in spring 2015 and autumn 2017, periods representative of canonical spring and autumn conditions in terms of thermohaline structure and current dynamics. We show that chlorophyll-a, oxygen, current, and stratification are important drivers for the distribution of sound scattering biota but that their relative importance depends on the area, the depth range, and the diel cycle. Prominent sound scattering layers (SSLs) in the epipelagic layer were associated with strong stratification and subsurface chlorophyll-a maximum. In areas where chlorophyll-a maxima were deeper than the peak of stratifications, SSLs were more correlated with stratification than subsurface chlorophyll maxima. Dissolved oxygen seems to be a driver in locations where lower oxygen concentration occurs in the subsurface. Finally, our results suggest that organisms seem to avoid strong currents core. However, future works are needed to better understand the role of currents on the vertical distribution of organisms.
Plan de classement
Sciences du milieu [021] ; Limnologie physique / Océanographie physique [032]
Description Géographique
ATLANTIQUE ; ZONE TROPICALE
Localisation
Fonds IRD [F B010090153]
Identifiant IRD
fdi:010090153
Contact