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Muelbert, Jose H; de Macedo-Soares, Luis Carlos Pinto; Favareto, L R; Costa, M D P (2018): Ichthyoplankton composition form NICOP-LaPlata cruise 1, Southern Brazilian Shelf, in 2003 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.888799, In: Muelbert, JH et al. (2018): Ichthyoplankton surveys in the southern Brazilian region from 1970 to 2010 [dataset publication series]. PANGAEA, https://doi.org/10.1594/PANGAEA.884342

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Related to:
de Macedo-Soares, Luis Carlos Pinto (2015): O papel das massas de água e do clima na variação espacial e temporal em grande escala do ictioplâncton no Oceano Atlântico Sudoeste (21° - 41°S) (PhD Thesis). Universidade Federal de Santa Catarina, 201 pp, https://bu.ufsc.br/teses/PECO0088-T.pdf
de Macedo-Soares, Luis Carlos Pinto; Garcia, Carlos Alberto Eiras; Freire, Andrea Santarosa; Muelbert, Jose H (2014): Large-scale ichthyoplankton and water mass distribution along the South Brazil Shelf. PLoS ONE, 9(3), e91241, https://doi.org/10.1371/journal.pone.0091241
Möller Jr, Osmar O; Piola, Alberto R (2004): The Plata Summer Cruise 2004, Cruise Report. Departamento de Ciencias de las Atmósfera y los Océanos, Universidad de Buenos Aires (Argentina), Instituto de Oceanografia, Universidade Federal do Rio Grande (Brazil), 24 pp, Summer2004_cruise_report.pdf (Summer2004_cruise_report.pdf)
Muelbert, Jose H; Acha, Marcelo; Mianzan, Hermes; Guerrero, Raúl; Reta, Raúl; Braga, Elisabete S; Garcia, Virginia M T; Berasategui, Alejandro; Gomez-Erache, Mónica; Ramírez, Alejandro (2008): Biological, physical and chemical properties at the Subtropical Shelf Front Zone in the SW Atlantic Continental Shelf. Continental Shelf Research, 28(13), 1662-1673, https://doi.org/10.1016/j.csr.2007.08.011
Piola, Alberto R; Möller Jr, Osmar O; Muelbert, Jose H (2003): The Plata Winter Cruise 2003, Cruise Report. Departamento de Ciencias de las Atmósfera y los Océanos, Universidad de Buenos Aires (Argentina), Instituto de Oceanografia, Universidade Federal do Rio Grande (Brazil), 23 pp, WInter2003_cruise_report.pdf (WInter2003_cruise_report_Pla_hi.pdf)
Coverage:
Median Latitude: -33.427108 * Median Longitude: -52.005422 * South-bound Latitude: -39.310000 * West-bound Longitude: -57.450000 * North-bound Latitude: -27.060000 * East-bound Longitude: -46.750000
Date/Time Start: 2003-08-20T17:33:00 * Date/Time End: 2003-09-01T11:37:00
Minimum Elevation: -1565.0 m * Maximum Elevation: -14.0 m
Event(s):
La_Plata_1_1 (111_1) * Latitude: -38.140000 * Longitude: -57.450000 * Date/Time: 2003-08-20T17:33:00 * Elevation: -24.0 m * Campaign: La_Plata_1 * Basis: Puerto Deseado * Method/Device: CTD/Rosette (CTD-RO)
La_Plata_1_2 (111_2) * Latitude: -38.250000 * Longitude: -57.230000 * Date/Time: 2003-08-20T19:06:00 * Elevation: -47.0 m * Campaign: La_Plata_1 * Basis: Puerto Deseado * Method/Device: CTD/Rosette (CTD-RO)
La_Plata_1_3 (111_3) * Latitude: -38.390000 * Longitude: -56.910000 * Date/Time: 2003-08-20T21:25:00 * Elevation: -80.0 m * Campaign: La_Plata_1 * Basis: Puerto Deseado * Method/Device: Net (NET)
Comment:
The NICOP-LA PLATA series cruises were carried out under the general objectives of the South Atlantic Climate Change Consortium (SACC), sponsored by the Inter-American Institute for Climate Change Research (IAI). The main objective of this project was to characterize the seasonal variations of the Rio de la Plata plume and the Subtropical Shelf Front (STSF) and their impacts on the circulation, and on the chemical and biological processes on the continental shelf. Eleven transects were performed perpendicular to the coastbetween Itajaí (26.9° S, 48.6° W - Brazil) and Mar del Plata (38.0° S, 57.5° W - Argentina) during the winter of 2003 (LA PLATA Winter Cruise) and the summer of 2004 (LA PLATA Summer Cruise). The sampling design resulted in 83 oceanographic stations taken with RV. Puerto Deseado in the winter cruise (August 20 to September 2), and 90 stations taken with the RV Antares in the summer cruises (February 1 to 19). Transects covered from near the coast (~ 18 km) to offshore depths greater than 1000 m (Piola et al., 2003; Möller Jr. & Piola, 2004).
Three strategies were applied for ichthyoplankton sampling. Integrated vertical arrays were conducted at the stations located near the 50 m and 200 m isobaths with a with 300 μm mesh and 0.6 m diameter Motoda net. During the second cruise, a 0.6 m in diameter WP-2 net with 140 μm mesh net (damaged and replaced by a mesh of 500 μm later) and was used in integrated vertical trawls. The second strategy consisted of vertical stratified hauls at two depths using a WP-2 net coupled with a closing mechanism. The hauls were carried out in stations near a 100 m isobath. This net was subsequently replaced during the second cruise by a 0.6 m diameter conical net with 200 μm mesh. The third strategy was conducted in the Albardão transect (between 33ºS and 34ºS) using the Motoda net, which was trawled horizontally for 10 minutes in two depths. All the stratified samples were taken below and above the halocline (Piola et al., 2003; Möller Jr. & Piola, 2004; Macedo-Soares, 2015).
The samples were fixed and preserved in formaldehyde solution, buffered with sodium tetraborate, diluted in sea water with a final approximate concentration of 4%. The filtrate volume was calculated based on the measurement of coupled flowmeters in each net, and was used to standardize the abundance of eggs and fish larvae per 100 m3 of filtered water. Two subsamples were obtained with a Folson splitter and shared between the Federal University of Rio Grande (FURG) and the National Institute of Fisheries Research and Development (INIDEP). For this cruises dry zooplankton biomass was determined and is express as milligrams per cubic meter of filtered water. The data compiled in the database are derived from the analyzes of the subsamples analyzed at LEI/FURG.
Parameter(s):
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
1Event labelEventMuelbert, Jose H
2Date/Time of eventDate/TimeMuelbert, Jose H
3Latitude of eventLatitudeMuelbert, Jose H
4Longitude of eventLongitudeMuelbert, Jose H
5Depth, bathymetricBathy depthmMuelbert, Jose H
6DistanceDistancekmMuelbert, Jose Hfrom shore
7Temperature, waterTemp°CMuelbert, Jose Hat surface
8SalinitySalMuelbert, Jose Hat surface, PSU
9VolumeVolm3Muelbert, Jose Hfiltered
10Zooplankton, biovolumeZooplankton biovolµm3/mlMuelbert, Jose H
11Fish eggsFish eggs#Muelbert, Jose H
12Fish larvaeFish larv#Muelbert, Jose H
13Fish eggsFish eggs#/m3Muelbert, Jose Habundance at station
14Fish larvaeFish larv#/m3Muelbert, Jose Habundance at station
15OrderOrderMuelbert, Jose H
16FamilyFamilyMuelbert, Jose H
17SpeciesSpeciesMuelbert, Jose H
18Number of speciesSpec No#Muelbert, Jose Hof fish eggs
19Number of speciesSpec No#Muelbert, Jose Hof fish larvae
20Fish eggsFish eggs#/m3Muelbert, Jose Hper species or taxon
21Fish larvaeFish larv#/m3Muelbert, Jose Hper species or taxon
22FlagFlagMuelbert, Jose H1 = beginning of new station, 0 = same station as above
23Method commentMethod commMuelbert, Jose Hhaul type: VT = total vertical, HS = horizontal surface, VST = vertical stratified, HST = horizontal stratified (eg Multinet)
24Depth, top/minDepth topmMuelbert, Jose Hhaul depth, minimum range, = the actual depth of the haul (vertical, oblique or horizontal haul), OR the depth range in case of stratified hauls. E.g. the net went down to 250m and it was hauled to 100m depth, so haul depth is 150m (250-100)
25Depth, bottom/maxDepth botmMuelbert, Jose Hhaul depth, maximum range, = the actual depth of the haul (vertical, oblique or horizontal haul), OR the depth range in case of stratified hauls. E.g. the net went down to 250m and it was hauled to 100m depth, so haul depth is 150m (250-100)
26Method commentMethod commMuelbert, Jose Hstation type: PKT = plankton trawl station, CTD = CTD station
27TransectTransectMuelbert, Jose H
28Device typeDeviceMuelbert, Jose Hnet
Size:
3332 data points

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