EML mapping question.
David Blankman
dblankman at lternet.edu
Mon Nov 18 12:36:22 PST 2002
Below is a metadata document from the McMurdo LTER site. In the
document they have a section called "CITATION".
* CITATIONS: *Spaulding, Sarah A, Diane M. McKnight, Richard L. Smith
and Richard Dufford. 1994. Phytoplankton population dynamics in
perennially ice-covered Lake Fryxell, Antarctica. Journal of Plankton
Research. Vol.16 no.5 pp.527-541.
It appears to be an indication that the data was used in that journal
article.
Where in the vast scheme of EML would that information be put? My first
thought was there ought to be something at the dataset level to use.
When I look at the ResourceGroup, I see pubDate and Series. The
documentation for series implies that there is a reference to a journal:
<doc:tooltip>Series</doc:tooltip>
<doc:summary>The series from which the resource
came.</doc:summary>
<doc:description>This field describes the series of
resources that
include the resource being described. For example, a volume of a
journal may be part of a series of the journal for a particular
year.</doc:description>
Perhaps I have been looking at EML too long and can't see the obvious,
but I couldn't find any obvious place to put this info. I can see that
one could use the title of the journal article as the title or
alternative title., but where would the following go:
Journal of Plankton Research. Vol.16 no.5 pp.527-541.
SUMMER PHYTOPLANKTON DENSITIES 1992-2001
------------------------------------------------------------------------
Acceptance and utilization of LTER data requires that:
* the Principal Investigator be sent a notice stating reasons for
acquiring any data and a description of the publication intentions.
* The Principal Investigator of the data set be sent a copy of the
report or manuscript prior to submission and be adequately cited
in any resultant publications.
* A copy of any resultant publications should be sent to the McMurdo
data manager at:
as well as the Principal Investigator. For a list of MCM LTER
Principal Investigators <http://huey.colorado.edu/LTER/pi.html>.
------------------------------------------------------------------------
SUMMER PHYTOPLANKTON DENSITIES 1992-2001
* FILE NAME: *phytplkt.dat
<http://huey.colorado.edu/LTER/datasets/lakes/plankton/phytplkt.dat>Data
File (Comma Delimited Ascii Format).
* PRINCIPAL INVESTIGATOR: *Diane McKnight
*Address:*INSTAAR, 1560 30th Street, Campus Box 450, Boulder CO, 80309-0450
*Phone:*(303)492-4687
*E-Mail:*mcknight at snobear.colorado.edu
<mailto:mcknight at snobear.colorado.edu>
* OTHERS: *
* KEYWORDS: *lake, limnology, phytoplankton, density, phylum
* ABSTRACT: *Phytoplankton were collected over four austral summers
(1991-92 through 1994-95) to examine seasonal and annual fluctuation in
species composition and biovolume in Lakes Fryxell, Hoare, West Lake
Bonney, and East Lake Bonney. All of these lakes are perennially
ice-covered lakes located in the Dry Valleys of South Victoria Land,
Antarctica. The phytoplankton consisted primarily of cryptophyte and
chlorophyte flagellates, and filamentous cyanobacteria. Some common taxa
were vertically stratified (Oscillatoria limnetica, Phormidium
angustissimum, Pyramimonas sp., Oscillatoria sp.), while others showed
no distinct vertical stratification (Chlamydomonas subcaudata,
Cryptomonas sp.). The stratification of the phytoplankton reflects the
gradients of nutrients and light, and the stability of the water column.
* VARIABLES: *limno run, location name, location code, date, depth (m),
phylum, species, density (cells/mL), file name
* RESEARCH LOCATION: *Lake Fryxell, Lake Bonney and Lake Hoare are all
located in Taylor Valley, South Victoria Land, Antarctica. Lake Fryxell
(77 37'S, 163 07'E) is at an elevation of 16 m above sea level. It has
an area of 7 km2 and a maximum depth of 19 m. The perennial ice cover
has a thickness of ~4.5 m. Sampling was conducted at a center station,
where the depth was 18.5 m. Lake Bonney is roughly 6.0 kilometers in
length and up tp 900 meters wide. It is comprised of a larger east basin
and a smaller west basin. Samples were gathered from both basins. The
east lobe has a perennial ice cover thickness of ~3.8 m; the west lobe
has a perennial ice cover thickness of ~3.7 m. Lake Hoare occupies a
narrower portion of the valley, is dammed by the Canada Glacier, and
would drain almost completely without this dam. It is roughly 4.2
kilometers long and up to 1100 meters wide. There are a number of
islands which may be related to an old terminal moraine of Canada
Glacier. The perennial ice cover thickness is ~4.0 m.
* METHODS: *Discrete samples for phytoplankton enumeration were
collected from the oxygenated portion of the water column (below the
bottom of the ice to a depth of 10 m) at 0.5 m intervals. Sampling was
done primarily between the hours of 14:00 and 20:00 (during the austral
summer, the illuminated period is 24 h/day) by either peristaltic pump
or Kemmerer bottle. Samples were collected in 1 l bottles and preserved
immediately with Lugon's solution (American Public Health Association,
1985). Identification and counts were made with an inverted microscope
by the method of Utermohl (1958). At least 100 individuals of the most
numerous algae were counted per sample at 100x magnification. The total
number of individuals counted was dependent on the number of taxa, but
ranged between 200 and 500. Counting error ranged between 13 and 26%,
depending on species. Algal species identifications were made using
Geitler (1932), Seaburg et al. (1979) and Prescott (1962). Cell volumes
were estimated for dominant taxa by measuring cell dimensions of 50-100
individuals and using closest geometric formulas of additional dates and
depths to determine changes in cell volume over time. For rare taxa,
volume estimates were made from fewer cell measurements.
Primary productivity was measured using the method of Strickland and
Parsons (1972). In situ 24 h incubations were made in triplicate 300 ml
light and duplicate 300 ml dark bottles with Na14CO3 (3 uCi per 300 ml,
New England Nuclear). Following 24 h incubation, samples were well
shaken and filtered through Whatman GF/F filters in the dark. The
filters were placed in scintillation vials and acidified with 1 ml of 5%
acetic acid in methanol to remove [C14] carbonates. The [C14] fixed by
biological activity was determined in Aquasol (New England Nuclear) by
liquid scintillation.
Samples for nitrate and orthophosphate were frozen within several hours
of collection, later filtered through 0.45 um Nucleopore filters and
analyzed by air-segmented continuous-flow absorption spectrophotometry
(Alpkem RFA-300) (Antweiler et al., 1993). Chlorophyll extractions were
made in 95% ethanol (Jesperson and Christoffersen, 1987) and measured in
a Turner Designs Model 10 Fluorometer.
* TIMING: *Samples were gathered from the following locations and dates:
*LocationDate(s)*
Lake Fryxell:1/10/92, 11/16/93, 1/7/94, 1/18/94, 11/14/94, 12/4/94,
1/17/95, 9/14/95, 11/26/95, 12/27/95, 10/26/96, 11/19/96, 1/9/97,
11/18/97, 12/29/97, 10/28/98, 11/23/98, 12/20/98, 10/30/99, 11/27/99,
12/23/99, 11/7/00, 12/3/00, 12/30/00, 1/17/01
East Lake Bonney:10/27/93, 11/24/93, 12/21/93, 11/2/94, 12/17/94
West Lake Bonney:10/29/93, 11/26/93, 12/23/93, 11/4/94, 12/19/94
Lake Hoare:11/5/93, 12/1/93, 12/30/93, 1/19/94, 11/10/94, 12/24/94,
1/20/95, 10/10/95, 11/21/95, 12/23/95, 11/8/96, 12/2/96, 11/14/97,
12/1/97, 12/26/97, 11/3/98, 12/1/98, 12/26/98, 11/17/99, 12/12/99,
1/4/00, 11/11/00, 1/2/01
* CITATIONS: *Spaulding, Sarah A, Diane M. McKnight, Richard L. Smith
and Richard Dufford. 1994. Phytoplankton population dynamics in
perennially ice-covered Lake Fryxell, Antarctica. Journal of Plankton
Research. Vol.16 no.5 pp.527-541.
--
David E. Blankman
Database Integration Developer
Long Term Ecological Research Network Office
University of New Mexico
801 University, SE #104
Albuquerque, NM 87106
(505) 272-7346 / (505) 272-7080 FAX
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