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GLIN==> UPCOMING SEMINAR
- Subject: GLIN==> UPCOMING SEMINAR
- From: Kanika Suri <Kanika.Suri@noaa.gov>
- Date: Tue, 22 Aug 2006 15:43:15 -0400
- Delivered-to: glin-announce-archive@glc.org
- Delivered-to: glin-announce@great-lakes.net
- List-name: GLIN-Announce
- User-agent: Mozilla Thunderbird 1.0 (Windows/20041206)
*Dr. Wayne S. Gardner*, from The University of Texas Marine Science
Institute, will be giving a seminar on Wednesday August 30, as a part of
the NOAA/ University of Michigan Great Lakes Seminar Series.
Please find details of his talk listed below.
Title: Dissimilatory nitrate reduction to ammonium (DNRA), a mechanism
for retaining bioavailable nitrogen in coastal ecosystems
Speaker: *Dr. Wayne S. Gardner*, University of Texas Marine Science
Institute
Date: Wednesday August 30
Time: 1030 AM
Location: NOAA/ GLERL
2205 Commonwealth Blvd., Ann Arbor, MI, 48105
Abstract
Denitrification and DNRA are dissimilatory heterotrophic nitrate
reduction processes, which occur at the sediment-water interface in
coastal or other aquatic environments. Denitrification converts
nitrate-N into the relatively inert N_2, whereas DNRA converts it to
NH_4 ^+ , an N form that can be re-assimilated by plants and bacteria.
Denitrification has been measured in a variety of freshwater and marine
systems but DNRA has not been considered as often, in part because
measurement is cumbersome. Nitrogen transformations, relative to oxygen
consumption rates, were examined in a variety of shallow coastal marine
and lake systems. Concentration changes of nutrients and gases between
inflow and outflow waters were measured as site water was passed
continuously over intact cores before and after addition of ^15
N-labeled nitrate to inflow water. DNRA is an important process in some
Texas coastal systems and its importance increases with salinity. DNRA
is also a significant mechanism for retaining nitrogen in Florida Bay.
DNRA rates related to sediment oxygen consumption rates in that region,
regardless of season (August 2004 vs. January 2005), whereas
denitrification rates were low in summer. DNRA thus provides an
explanation for the high NH_4 ^+ :NO_3 ^- and high NH_4 ^+ :PO_4 ^3-
ratios, often observed in Florida Bay. It may be an important mechanism
affecting N and O_2 dynamics in marine “low-oxygen dead zones,” as occur
in the northern Gulf of Mexico and other regions, but is less important
in comparable freshwater systems such as Lake Erie.
------------------------------------------------------------------------
If you have any questions or concerns, please email me at
kanika.suri@noaa.gov; or call 734-741-2147.
For more information about the seminar series, please visit our website
at http://www.glerl.noaa.gov/news/seminars/
--
XXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXXX
Kanika Suri
Web Designer Associate
NOAA Great Lakes Environmental Research Laboratory
2205 Commonwealth Blvd.,
Ann Arbor, MI
48105
Tel: (734) 741-2147
Fax: (734) 741-2055
www.glerl.noaa.gov
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