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29 results for “Mesozooplankton”
Figure 1 in Structure of mesozooplankton community in the Barents Sea and adjacent waters in August 2009
Figure 1. Barents Sea and adjacent waters. Location of sampling stations in 2009 and general scheme of main water masses (Ozhigin and Ivshin 1999): MCW, Murmansk coastal waters; AW, Atlantic waters; SCW, Svalbard coastal waters; ArW,– Arctic waters; BW, Bear Island waters; NCW, Norwegian coastal waters; TAW, Transformed Atlantic waters (Barents Sea waters); WCW, White Sea coastal waters; PCW, Pechora coastal waters; NZCW, Novaya Zemlya coastal water.
Figure 5 in Structure of mesozooplankton community in the Barents Sea and adjacent waters in August 2009
Figure 5. Mesozooplankton biomass (a: mg dry mass m−3 ± standard error; b: g dry mass m−2 ± standard error) within different water masses in the upper 100-m layer in the Barents Sea and adjacent waters in August 2009. MCW, Murmansk coastal waters; AW, Atlantic waters; AWF, Atlantic waters (frontal zone); BW, Bear Island waters; SCW, Svalbard coastal waters; ArW, Arctic waters.
Figure 4 in Structure of mesozooplankton community in the Barents Sea and adjacent waters in August 2009
Figure 4. Cluster dendrogram of sampling station based on the mesozooplankton abundance in the upper 100-m layer in the Barents Sea and adjacent waters in August 2009. MCW, Murmansk coastal waters; AW, Atlantic waters; SCW, Svalbard coastal waters; ArW, Arctic waters.
Bulk and amino acid nitrogen specific isotope data from particulate organic matter and mesozooplankton (1000-2000 µm) from the Mekong River plume and southern South China Sea
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DNA metabarcoding reveals trophic niche diversity of micro and mesozooplankton species: supplementary data and code
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Data from: Metabolism and foraging strategies of mid-latitude mesozooplankton during cyanobacterial blooms as revealed by fatty acids, amino acids and their stable carbon isotopes
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Assembled file of spring annual averages of measures of total mesozooplankton organic biomass as carbon, in the California Current System, 1951 - 2008.
Reference for zooplankton organic carbon is Lavaniegos and Ohman (2007). More than 400 zooplankton types counted.
Figure 3 in Biological diversity and seasonal variation of mesozooplankton in the southeastern Black Sea coastal ecosystem
Figure 3. The variation in total mesozooplankton abundance and temperature with respect to years (SST: sea surface temperature).
Time series of mesozooplankton data at LTER-MC in the Gulf of Naples (1984-2015)
<p>The present dataset contains the abundance data (ind. m<sup>-3</sup>) of total mesozooplankton, main groups and copepod species from the Long Term Ecological Research station MareChiara in the Gulf of Naples (st. LTER-MC, 40°48.5’ N, 14°15’ E) over the years 1984-2015. Zooplankton samples were collected by vertical tows in the upper 50 m using an Indian Ocean net (200-µm mesh, 113-cm mouth diameter) and fixed with buffered formaldehyde (2–4% final concentration). In the laboratory, the samples were concentrated and resuspended in filtered seawater to a volume of 200 ml to remove the formaldehyde. Aliquots ranging from 1/4 to 1/32, according to the sample density, were initially taken using the Huntsman beaker subsampling technique and successively with a large-bore graduated pipette after careful mixing. Aliquots were transferred to a mini-Bogorov chamber (10 ml) and examined under a stereomicroscope and all zooplankton taxa were identified and counted. The entire sample was checked for the presence of rare species. The copepod abundances reported here correspond to the whole population (adult females and males, and copepodites).</p>
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