Estimating Carbon Flux From Optically Recording Total Particle Volume at Depths Below the Primary Pycnocline

Alexander B. Bochdansky, Robert B. Dunbar, Dennis A. Hansell, Gerhard J. Herndl

Research output: Contribution to journalArticle

Abstract

Optical instruments can rapidly determine numbers and characteristics of water column particles with high sensitivity. Here we show the usefulness of optically assessed total particle volume below the main pycnocline to estimate carbon export in two systems: the open subarctic North Atlantic and the Ross Sea, Antarctica. Both regions exhibit seasonally high phytoplankton production and efficient export (i.e., a strong biological pump). Total particle volumes in the mesopelagic (200–300 m) were significantly correlated with those in the overlying surface mixed layer (50–60 m), indicating that most particles at depth reflect export from the surface. This connectivity, however, is modulated by the physical structure of the water column and by particle type (e.g., the presence of colonies of the haptophyte Phaeocystis antarctica versus diatoms). Evidence from both regions show that a strong pycnocline can delay or may even prevent particles from settling to deeper layers, which then succumb to disintegration, and microbial and zooplankton consumption. Strong katabatic winds in the Ross Sea may deepen the mixed layer, causing a rapid transfer of particles to mesopelagic depths through the mixed-layer pump. Independent estimates of seasonally integrated export production in the Ross Sea, based on upper water column carbon mass balance, were significantly correlated (in the order of shared variance) with (1) total particle volumes from images, (2) particulate organic carbon, and (3) chlorophyll fluorescence, all recorded at a depth range of 200–300 m. Carbon export was not significantly correlated with particle abundance measured by a Coulter counter at the same depth range. Measuring total particle volume below the primary pycnocline is therefore a useful approach to estimate carbon export at least in regions characterized by seasonally high particle export.

Original languageEnglish (US)
Article number778
JournalFrontiers in Marine Science
Volume6
DOIs
StatePublished - Dec 20 2019

Fingerprint

pycnocline
carbon flux
Fluxes
Carbon
carbon
Pumps
Optical instruments
Water
Phytoplankton
Disintegration
Chlorophyll
Organic carbon
mixed layer
water column
Fluorescence
pumps
Antarctica
particle
optical equipment
biological pump

Keywords

  • Antarctica
  • Atlantic
  • biological pump
  • carbon export
  • particle flux

ASJC Scopus subject areas

  • Oceanography
  • Global and Planetary Change
  • Aquatic Science
  • Water Science and Technology
  • Environmental Science (miscellaneous)
  • Ocean Engineering

Cite this

Estimating Carbon Flux From Optically Recording Total Particle Volume at Depths Below the Primary Pycnocline. / Bochdansky, Alexander B.; Dunbar, Robert B.; Hansell, Dennis A.; Herndl, Gerhard J.

In: Frontiers in Marine Science, Vol. 6, 778, 20.12.2019.

Research output: Contribution to journalArticle

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