Articles | Volume 14, issue 5
https://doi.org/10.5194/os-14-1185-2018
https://doi.org/10.5194/os-14-1185-2018
Research article
 | 
09 Oct 2018
Research article |  | 09 Oct 2018

Turbulence and hypoxia contribute to dense biological scattering layers in a Patagonian fjord system

Iván Pérez-Santos, Leonardo Castro, Lauren Ross, Edwin Niklitschek, Nicolás Mayorga, Luis Cubillos, Mariano Gutierrez, Eduardo Escalona, Manuel Castillo, Nicolás Alegría, and Giovanni Daneri

Viewed

Total article views: 3,554 (including HTML, PDF, and XML)
HTML PDF XML Total BibTeX EndNote
2,175 1,250 129 3,554 92 107
  • HTML: 2,175
  • PDF: 1,250
  • XML: 129
  • Total: 3,554
  • BibTeX: 92
  • EndNote: 107
Views and downloads (calculated since 24 Oct 2017)
Cumulative views and downloads (calculated since 24 Oct 2017)

Viewed (geographical distribution)

Total article views: 3,554 (including HTML, PDF, and XML) Thereof 3,210 with geography defined and 344 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Latest update: 20 Nov 2024
Download
Short summary
Fjord systems play an important role in primary production and carbon export. Acoustic, hydrographic and in situ abundance measurements were used to study macrozooplankton assemblages at 44.7° S. Diel vertical migration of zooplankton stopped at the hypoxic boundary layer and apparently did not tolerate the hypoxic conditions. Turbulence appears to be the oceanographic process that contributes to vertical mixing around the sill, helping the interchange of nutrients, feeding and carbon export.