English
 
User Manual Privacy Policy Disclaimer Contact us
  Advanced SearchBrowse

Item

ITEM ACTIONSEXPORT

Released

Journal Article

Advective transport and decomposition of chain-forming planktonic diatoms in permeable sediments

MPS-Authors
/persons/resource/persons210350

Ehrenhauss,  S.
Department of Biogeochemistry, Max Planck Institute for Marine Microbiology, Max Planck Society;

/persons/resource/persons210468

Huettel,  M.
Flux Group, Max Planck Institute for Marine Microbiology, Max Planck Society;

External Ressource
No external resources are shared
Fulltext (public)
There are no public fulltexts stored in PuRe
Supplementary Material (public)
There is no public supplementary material available
Citation

Ehrenhauss, S., & Huettel, M. (2004). Advective transport and decomposition of chain-forming planktonic diatoms in permeable sediments. Journal of Sea Research, 52(3), 179-197.


Cite as: http://hdl.handle.net/21.11116/0000-0001-D102-0
Abstract
In laboratory chamber experiments we demonstrate that permeable sediments (>7×10−12 m2) exposed to boundary flows filter chain-forming coastal bloom diatoms (Skeletonema costatum and Thalassiosira rotula) from the water column, causing rapid transfer of fresh organic particulate matter into sediment layers as deep as 5 cm within 72 h. The penetration depth of the diatoms depends on the permeability of the bed and the length of the chains. Long chains were not transported as deep into the sediment as short chains or single cells. The fast advective transfer of phytoplankton cells into sandy sediments may be an important process facilitating organic matter uptake and preventing resuspension of deposited organic material in high-energy coastal environments. High advective flushing rates in medium- and coarse-grained sandy sediments enhanced the mineralisation of the trapped diatoms (2300 to 3200 μmol C m−2 d−1), stimulated benthic oxygen consumption (2300 to 3000 μmol O2 m−2 d−1), as well as nitrification (up to 20 μmol NO3− m−2 d−1), relative to sediment where diffusion dominated the solute exchange. Advective solute exchange rates that increase with increasing permeability prevent the accumulation of Si(OH)4 near the dissolving frustules and in the pore water, leading to an effective recycling of dissolved silica to the production process in the water column (95 to 101 μmol Si(OH)4 m−2 d−1). This process may also enhance dissolution rates of the deposited opal in coarse-grained sands by maintaining higher degrees of undersaturation than in fine-grained sediments. Our results suggest that advective filtration of planktonic diatoms into permeable sediments increases mineralisation and recycling of Si(OH)4 and organic matter in high energetic shelf areas.