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Figure 6 in First observation and seasonal dynamics of the new invasive planktonic copepod Oithona davisae Ferrari and Orsi, 1984 along the southern Black Sea (Anatolian Coast)

Figure 6. Major shipping lanes in the Black Sea http://www.marinevesseltraffic.com/2013/06/black-sea-marine-traffic.html. © Marine Vessel Traffic. Reproduced by permission of Marine Vessel Traffic. Permission to reuse must be obtained from the rightsholder.

Figure 5 in First observation and seasonal dynamics of the new invasive planktonic copepod Oithona davisae Ferrari and Orsi, 1984 along the southern Black Sea (Anatolian Coast)

Figure 5. (a) Abundance of Oithona davisae (ind. m−3); (b) abundance of female O. davisae with egg sac (ind. m−3).

Figure 4 in First observation and seasonal dynamics of the new invasive planktonic copepod Oithona davisae Ferrari and Orsi, 1984 along the southern Black Sea (Anatolian Coast)

Figure 4. Photographs of Oithona davisae: (a, b) lateral view of female with egg sac; (c) dorsal view of male; (d) lateral view of urosome; (e) rostrum of female (Photographs by Yildiz and Feyzioglu).

Figure 7 in First observation and seasonal dynamics of the new invasive planktonic copepod Oithona davisae Ferrari and Orsi, 1984 along the southern Black Sea (Anatolian Coast)

Figure 7. Black Sea coastal current system (http://www.ims.metu.edu.tr/cv/oguz/circulation.htm). © Temel Oguz. Reproduced by permission of Temel Oguz. Permission to reuse must be obtained from the rightsholder.

Figure 1 in First observation and seasonal dynamics of the new invasive planktonic copepod Oithona davisae Ferrari and Orsi, 1984 along the southern Black Sea (Anatolian Coast)

Figure 1. (●) Previous report sites of Oithona davisae (Altukhov et al. 2014), (▲) Time series stations and (+) sampling locations.

Figure 7 in First observation and seasonal dynamics of the new invasive planktonic copepod Oithona davisae Ferrari and Orsi, 1984 along the southern Black Sea (Anatolian Coast)

Figure 6 in First observation and seasonal dynamics of the new invasive planktonic copepod Oithona davisae Ferrari and Orsi, 1984 along the southern Black Sea (Anatolian Coast)

Figure 1 in First observation and seasonal dynamics of the new invasive planktonic copepod Oithona davisae Ferrari and Orsi, 1984 along the southern Black Sea (Anatolian Coast)

Figure 1. (●) Previous report sites of Oithona davisae (Altukhov et al. 2014), (▲) Time series stations and (+) sampling locations.

publicJun 2014View details →

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Data from: A metagenetic approach for revealing community structure of marine planktonic copepods

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Data from: Metabarcoding and metabolome analyses of copepod grazing reveal feeding preference and linkage to metabolite classes in dynamic microbial plankton communities

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publicSep 2016View details →

Figure 2 in Spatiotemporal distribution of planktonic copepod communities in Tokyo Bay where Oithona davisae Ferrari and Orsi dominated in mid-1980s

Figure 2. Horizontal distribution of surface temperature, surface and bottom salinity, bottom DO and transparency in Tokyo Bay (modified from Investigation Committee for Fisheries Impacts of Trans-Tokyo Bay Highway and Japan Fisheries Resources Conservation Assoc 1987). Numerals in parentheses indicate mean. Surface: 0.5 m, bottom: 1 m above sea floor.

Figure 1 in Spatiotemporal distribution of planktonic copepod communities in Tokyo Bay where Oithona davisae Ferrari and Orsi dominated in mid-1980s

Figure 1. Map showing stations where plankton samples were collected. Numerals in parentheses indicate depth (m). Broken lines show boundaries between areas as used in the text.

Figure 7 in Seasonal changes in the population structure of dominant planktonic copepods collected using a sediment trap moored in the western Arctic Ocean

Figure 7. Seasonal changes in the flux of adult females, lipid accumulation (upper panels) and gonad maturation (lower panels) composition (stage I−III) of C6F (a, d) Calanus hyperboreus; (b, e) Metridia longa; and (c, f) Paraeuchaeta glacialis.

Figure 4 in Seasonal changes in the population structure of dominant planktonic copepods collected using a sediment trap moored in the western Arctic Ocean

Figure 4. Seasonal changes in the copepod flux and species composition at St. NAPt from October 2010 to September 2012.

Figure 6 in Inter-oceanic comparison of planktonic copepod ecology (vertical distribution, abundance, community structure, population structure and body size) between the Okhotsk Sea and Oyashio region in autumn

Figure 6. Vertical distribution of the prosome length ratios of the copepods (PLOkhotsk: PLOyashio) (left) and temperature anomalies (°C: TOkhotsk – TOyashio) (right) between the Okhotsk Sea (St. OK24) and Oyashio region (St. 19) evaluated by IONESS from October to November 1996. The vertical distribution of each copepod is calculated by daily duplicate samples in the Okhotsk Sea (symbols and bars indicate the means and standard deviations of D50%, respectively). For inter-oceanic comparison, the dashed lines in each panel indicate that the positions of values of both regions are equal.

Figure 6 in Seasonal changes in the population structure of dominant planktonic copepods collected using a sediment trap moored in the western Arctic Ocean

Figure 6. Seasonal changes in the flux and copepodid stage composition of the four large calanoid copepods: (a) Calanus hyperboreus; (b) Metridia longa; (c) Paraeuchaeta glacialis; and (d) Heterorhabdus norvegicus.

Figure 2 in Seasonal changes in the population structure of dominant planktonic copepods collected using a sediment trap moored in the western Arctic Ocean

Figure 2. Seasonal changes in depth (a) and temperature (b) of the sediment trap at St. NAPt from October 2010 to September 2012. The current velocity at 188 and 275 m at St. NAPt (c) was estimated by a physical ocean general circulation model.

Figure 1 in Seasonal changes in the population structure of dominant planktonic copepods collected using a sediment trap moored in the western Arctic Ocean

Figure 1. The location of St. NAPt (Northwind Abyssal Plain) in the western Arctic Ocean where the sediment trap was moored at a depth of approximately 184–260 m from October 2010 to September 2012.

Figure 5 in Seasonal changes in the population structure of dominant planktonic copepods collected using a sediment trap moored in the western Arctic Ocean

Figure 5. (a) Seasonal changes in the flux and copepodid stage composition of the dominant copepod Oncaea parila (Poecilostomatoida). *C6F with egg sacs occurred. (b) The relationship between O. parila flux and the total mass flux. A positive relationship was detected in 2010–2011 (first year).

Figure 5 in Spatiotemporal distribution of planktonic copepod communities in Tokyo Bay where Oithona davisae Ferrari and Orsi dominated in mid-1980s

Figure 5. Grouping results for copepod community in Tokyo Bay by a two dimensional NMDS ordination plot. Arrows indicate environmental gradients that have a significant (p <0.01) multiple regression to the ordination score from low to high.