Contributors | Affiliation | Role |
---|---|---|
Pfister, Catherine | University of Chicago | Principal Investigator |
Altabet, Mark A. | University of Massachusetts Dartmouth SMAST (UMASSD-SMAST) | Co-Principal Investigator |
Post, David | Yale University | Co-Principal Investigator |
Copley, Nancy | Woods Hole Oceanographic Institution (WHOI BCO-DMO) | BCO-DMO Data Manager |
See the other datasets associated with this project for methodology.
Seawater and filter sample isotope methodology is described in references cited below:
2014. Pather, S., C. A. Pfister, M. Altabet, D. M. Post. Ammonium cycling in the rocky intertidal: remineralization, removal and retention. Limnology and Oceanography 59:361-372. http://aslo.org/lo/toc/vol_59/issue_2/0361.html
in review (March 2014). Pfister, C. A., M. Altabet, D. Post.
Carbon system measurements are described in:
2012. Wootton, J. T. & C. A. Pfister. Carbon system measurements and potential climatic drivers at a site of rapidly declining ocean pH. PLoS ONE 7(12): e53396. doi:10.1371/journal.pone.0053396. Data associated with this paper are uploaded to the World Ocean DataBase, www.nodc.noaa.gov
Related files and references:
2010. Pfister, C. A., F. Meyer, D. A. Antonopoulos. Metagenomic profiling of a microbial assemblage associated with the California mussel, Mytilus californianus: a node in networks of carbon and nitrogen cycling. PLoS ONE 5(5): e10518. doi:10.1371/ journal.pone.0010518. Metagenome data associated with this paper are uploaded to MGRAST server at metagenomics.anl.gov
File |
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N_regen_v3.csv (Comma Separated Values (.csv), 205.35 KB) MD5:2ca6c08a416b35a9efe78b8d99ca2c7a Primary data file for dataset ID 489045 |
Parameter | Description | Units |
year | year | yyyy |
shore_offshore | close to shore or off-shore | text |
cruise_id | cruise identification | unitless |
month_local | day of month | 1-12 |
day_local | day; local time | 1-31 |
date_local | date; local time | MM/DD/YYYY |
time_local | local time; Pacific time zone | HH:MM:SS |
yrday_local | day and decimal time. eg. 326.5 for the 326th day of the year (November 22) at 1200 hours (noon). | unitless |
ISO_DateTime_Local | Date/Time (UTC) ISO formatted | YYYY-MM-DDThh:mm:ss[.xx]Z |
latitude | latitude; north is positive | decimal degrees |
longitude | longitude; east is positive | decimal degrees |
station | locale of station | text |
site | site code; may be same as station code | text |
depth_nom | nominal depth | meters |
depth | depth | meters |
vol_filt | volume filtered | liters |
filterpacket | filter packet id | unitless |
del15N | total nitrogen isotopic composition (delta 15N:N14) | parts per thousand vs. VSMOW (Vienna Standard Mean Ocean Water) |
del13C | total carbon isotopic composition (delta C13: 13C/12C) | parts per thousand vs. VSMOW (Vienna Standard Mean Ocean Water) |
N_pct | percent total nitrogen | percent |
C_pct | percent total carbon | percent |
comment_filter | comments pertaining to the filter | text |
bottle_isoN | nitrogen isotope bottle number | integer |
dN15_NO3 | nitrogen isotopic composition (delta 15N:N14) of nitrate | parts per thousand vs. VSMOW (Vienna Standard Mean Ocean Water) |
d18O_NO3 | oxygen isotopic composition (delta O18: 18O/16O) of nitrate | parts per thousand vs. VSMOW (Vienna Standard Mean Ocean Water) |
d15N_NH4 | nitrogen isotopic composition (delta 15N:N14) of ammonium | parts per thousand vs. VSMOW (Vienna Standard Mean Ocean Water) |
d15N_NO2 | nitrogen isotopic composition (delta 15N:N14) of nitrite | parts per thousand vs. VSMOW (Vienna Standard Mean Ocean Water) |
bottle_nut | nutrient bottle number | integer |
PO4 | phosphate concentration | microMolar |
Si | silicate concentration | microMolar |
NO3 | nitrate concentration | microMolar |
NO2 | nitrite concentration | microMolar |
NH4 | ammonium concentration | microMolar |
sstemp | sea surface temperature?? This value is given for depths within a profile so it may actually be temperature, not sea surface temperature. | degrees Celsius |
salinity | salinity | parts per thousand |
pH | pH: The measure of the acidity or basicity of an aqueous solution | unitless; pH scale |
O2_umol_kg | dissolved oxygen concentration | micromoles/kilogram |
O2_ml_L | dissolved oxygen concentration | milliliters/liter |
O2_mg_L | dissolved oxygen concentration | milligrams/liter |
O2_sat_pcnt | dissolved oxygen concentration | percent |
chl | chlorophyll-a concentration | milligrams/liter |
upwelling_day | daily average coastal upwelling index for 48 deg N; from http://www.pfeg.noaa.gov/products/pfel/modeled/indices/upwelling/upwelli... | meters^3/second/100 meters cosastline |
upwelling_mon | monthly average coastal upwelling index for 48 deg N; from http://www.pfeg.noaa.gov/products/pfel/modeled/indices/upwelling/upwelli... | meters^3/second/100 meters cosastline |
cond | specific conductance | milliSiemens/centimeter |
TDS | total dissolved solids | grams/liter |
LDO | luminescent/optical dissolved oxygen | milligrams/liter |
LDO_pcent | luminescent/optical dissolved oxygen saturation | percent saturation |
time_of_day | day = sample taken during day | text |
instrument | instrument used for measurement | text |
d18O_vial | oxygen isotopic composition (delta O18: 18O/16O) of seawater | parts per thousand vs. VSMOW (Vienna Standard Mean Ocean Water) |
d13C_seawater | carbon isotopic composition (delta C13: 13C/12C) of seawater | parts per thousand vs. VSMOW (Vienna Standard Mean Ocean Water) |
bottle_dickson | Dickson bottle number | integer |
sal | salinity | unitless |
TALK | total alkalinity | micromoles/kilogram |
DIC | dissolved inorganic carbon concentration | micromoles/kilogram |
bottle_niskin | Niskin bottle number | integer |
comment | comments | text |
Website | |
Platform | R/V Clifford A. Barnes |
Start Date | 2010-07-21 |
End Date | 2010-07-23 |
Description |
Website | |
Platform | R/V Clifford A. Barnes |
Start Date | 2010-08-25 |
End Date | 2010-08-27 |
Description |
Website | |
Platform | R/V Clifford A. Barnes |
Start Date | 2011-06-21 |
End Date | 2011-06-23 |
Description |
Website | |
Platform | R/V Clifford A. Barnes |
Start Date | 2011-07-25 |
End Date | 2011-07-27 |
Description |
Website | |
Platform | R/V Clifford A. Barnes |
Start Date | 2011-08-16 |
End Date | 2011-08-18 |
Description |
Website | |
Platform | R/V Clifford A. Barnes |
Start Date | 2012-06-29 |
End Date | 2012-06-30 |
Description |
Website | |
Platform | R/V Clifford A. Barnes |
Start Date | 2012-07-26 |
End Date | 2012-07-27 |
Description |
Website | |
Platform | R/V Clifford A. Barnes |
Start Date | 2012-08-14 |
End Date | 2012-08-16 |
Description |
Website | |
Platform | R/V Clifford A. Barnes |
Start Date | 2010-06-22 |
End Date | 2010-06-24 |
Website | |
Platform | Pfister small boat |
Start Date | 2009-06-24 |
End Date | 2009-06-24 |
Description | Seawater sampling in a small boat. |
Website | |
Platform | Pfister shore |
Start Date | 2009-06-24 |
End Date | 2012-08-20 |
NSF Award Abstract:
A fundamental and persistent question in a multitude of ecosystems is the extent to which new versus regenerated nutrients support ecosystem productivity. In coastal marine systems, nitrate derived from upwelling (= new nitrogen) and ammonium regeneration in coastal waters and sediments (= regenerated nitrogen) are major nitrogen sources that fuel coastal ocean productivity. Because inorganic nitrogen availability clearly regulates production in a large number of areas, understanding nitrogen supply is essential. In open coast regions away from river mouths, nitrate inputs are determined by large-scale physical processes promoting upwelling of deep, nutrient-rich water including wind direction and intensity. In contrast, regenerated nitrogen (mainly ammonium) is generally the result of local animal and microbial processes. Along marine rocky shores, where upwelling is typically used as a proxy for productivity, we know very little about the dynamics of regenerated nutrients and their potential contribution to productivity at larger scales; only upwelling is typically used as a proxy for productivity. Associations of the abundant California mussel, Mytilus californianus, with water nutrients, algal productivity, stable isotope signatures, and microbial genetics indicate potentially strong regeneration of nitrogen by these animals and suggest an important secondary role of nitrifying microbes affiliated with these animals.
In this project, the investigators will quantify the relative contribution of regenerated nitrogen on rocky shores through censuses and experiments across a gradient of mussel abundance. They will use stable nitrogen and oxygen isotopes of ammonium, nitrite, and nitrate to disentangle the contribution of different biological processes versus upwelling to the nitrogen supply and uptake of rocky shore regions. This includes both natural abundance and tracer addition studies.
Broader Impacts. Regenerated nitrogen supply, as opposed to new nitrogen via upwelling, is a local process dependent upon an intact animal community. However, mussels and other nearshore animals may be particularly vulnerable to a changing thermal environment, toxic algal blooms, and ocean acidification. Given the dramatic changes to the coastal nitrogen cycle in recent years, and potential changes to currents, upwelling, ocean chemistry, and El Niño frequencies portended by global changes to our climate, we to know the relative effect of local versus larger scale oceanic events on the nitrogen cycle. The proposed work links biological interactions in situ with its implications for coastal productivity.
In addition to expected publications in high quality journals, educational activities will continue to focus on graduate and undergraduate education and mentoring. The proposal will fund two graduate students and two undergraduates per year. The PI's will work closely with government (Olympic Marine National Sanctuary) and tribal (Makah Tribe) representatives to communicate this research. We will also work with Makah Museum Board of Trustees and the Makah Higher Education Committee to identify Makah students as research assistants. All three PI's teach broadly across their respective campuses, instructing almost every type of undergraduate major.
Funding Source | Award |
---|---|
NSF Division of Ocean Sciences (NSF OCE) |