GLORIA

GEOMAR Library Ocean Research Information Access

feed icon rss

Your email was sent successfully. Check your inbox.

An error occurred while sending the email. Please try again.

Proceed reservation?

Export
Filter
Document type
Keywords
Language
  • 1
    In: Journal of plankton research, Oxford : Oxford Univ. Press, 1979, 30(2008), 6, Seite 655-672, 1464-3774
    In: volume:30
    In: year:2008
    In: number:6
    In: pages:655-672
    Description / Table of Contents: Abundance, distribution, population structure, lipid content, lipid composition and reproductive and feeding activity of Rhincalanus nasutus were studied in the Gulf of Aqaba and in the northern Red Sea during RV "Meteor"-cruise M 44-2 in February/March 1999. Rhincalanus nasutus occurred in higher numbers in the Gulf of Aqaba (585 ind m-2) than in the northern Red Sea (254 ind m-2). Young developmental stages (nauplii, copepodite stages CI and CII) were absent. In the southern Gulf of Aqaba, the bulk of the population developed from stage CV to adult in the course of the 3-week study period. In contrast, immature CV stages dominated at the adjacent stations in the northern Gulf of Aqaba and in the northern Red Sea. Development was associated with the seasonal vertical migration from wintering mid-water layers and initiation of feeding starting as early as beginning of March in the southern Gulf of Aqaba. No upward migration was observed in the northern parts of the Gulf and in the northern Red Sea, where more than 90% of the females remained immature during our study. Lipids were dominated by wax esters in females and CV. The fatty acid and fatty alcohol compositions of females were very similar throughout the study region and period. Major fatty acids were 18:1(n-9), 16:1(n-7), 16:2(n-4) and 20:5(n-3). Our results support the previous reports of a seasonal dormancy of R. nasutus in the Gulf of Aqaba and suggest that the timing of vertical migration, feeding and maturation is closely coupled to the development of the spring bloom in oligotrophic subtropical waters.
    Type of Medium: Online Resource
    Pages: graph. Darst
    ISSN: 1464-3774
    Language: English
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 2
    Type of Medium: Book
    Pages: S. 2061 - 2250 , graph. Darst
    Series Statement: Deep sea research 57.2010,24/26
    Language: English
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 3
    ISSN: 1432-2056
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology
    Notes: Summary The Antarctic copepod species Rhincalanus gigas, Calanoides acutus and Calanus propinquus were studied in the area of the Antarctic Peninsula in May 1986. Research was focussed on vertical distribution and stage composition of the populations. Rhincalanus gigas occurred in greatest densities in the upper layers of the water column, and copepodite stages CI and CII and nauplii dominated the population. Gut content analyses suggest that R. gigas was actively feeding. Copepodite stage CV dominated the Calanoides acutus population. At two deep basin stations (water depth〉1000 m) the C. acutus population occurred below 500 m, whereas at shallower stations the majority was found above 300 m. Most specimens had empty guts. Calanus propinquus occurred in low densities, mainly in the upper water layers, and copepodite stage CV dominated. Most individuals of stage V had food in their guts. Our results suggest that C. acutus had ceased feeding and was overwintering in a resting stage (diapause), while C. propinquus and R. gigas were still active, the latter species having finished a late autumn spawning.
    Type of Medium: Electronic Resource
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 4
    Publication Date: 2020-06-10
    Description: The main emphasis of this study was to analyse the short-term development of abundance, population structure and vertical distribution of the dominant calanoid copepods during a phytoplankton bloom in the coastal area of the eastern Weddell Sea in December 2003. Microcalanus pygmaeus was by far the most abundant calanoid species. Metridia gerlachei, Ctenocalanus citer, Calanoides acutus, Calanus propinquus and the ice-associated Stephos longipes were also present in considerable proportions. The observed changes in the population characteristics and parameters of these species are described in detail and discussed in the context of the spring phytoplankton bloom. A conspicuous event occurring during the final stage of the study was the development of a strong storm. While the results suggest that this storm did not have any considerable influence on the populations of all other investigated copepod species, it very likely caused pronounced changes in the S. longipes population present in the water column. Before the storm, S. longipes was found primarily in the upper 100 m of the water column, and its population was dominated by adults (mean proportion = 41%) and the copepodite stage I (mean proportion = 30%). After the storm, the abundance increased considerably, and the copepodite stage I contributed by far the largest proportion (53%) of the total population indicating that the early copepodite stages probably had been released from the sea ice into the under ice water layer due to ice break-up and ice melt processes caused by the storm.
    Type: Article , PeerReviewed
    Format: text
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 5
    Publication Date: 2015-02-04
    Description: In the framework of the R.V. Polarstern expedition “Ice station POLarstern” (ISPOL) spatial and temporal trends in composition, abundance and age structure of sea ice inhabiting copepods were investigated in the western Weddell Sea during the transition from the spring to the summer state. For the spatial scale, sea-ice coring was performed at six locations on a transect from the ice edge to the ice-drift station between 14 and 24 November 2004. The temporal changes were investigated in a time series study on a drifting sea-ice floe from 29 November to 30 December 2004. A relatively large number of copepod species (15) were found in the ice with a higher number at the time station (13) than at the transect (9). Drescheriella spp. was by far the most abundant taxon encountered in the sea ice throughout the present study (72–87%). On the transect, Idomene antarctica ranked second in abundance (7%) followed by Stephos longipes (2%) and Ectinosoma sp. (2%). In contrast, Diarthrode cf. lilacinus, which was not found on the transect, was the second most abundant species (11%) at the time station, followed by I. antarctica (9%), Ectinosoma sp. (6%) and S. longipes (1%). Naupliar stages dominated the populations of Drescheriella spp. and S. longipes both on the transect and during the time series. The Ectinosoma sp. population was dominated by nauplii only at the stations of the transect, while copepodite stages made up the largest fraction during the time series. Copepodids always predominated the I. antarctica populations, and it was the only species in which adults occurred in high densities contributing significantly to the abundance. Only Drescheriella spp. and S. longipes occurred throughout the sea-ice cores, while the occurrence of all other species was restricted to the bottom layer of the ice. The distribution of all species was very patchy and varied greatly between the sampling sites.
    Type: Article , PeerReviewed
    Format: text
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 6
    Publication Date: 2018-05-28
    Description: Zooplankton grazing on bacterio- and phytoplankton was studied in the Gulf of Aqaba and the Northern Red Sea during Meteor Cruise Me 44-2 in February-March 1999. Protozoan grazing on bacterioplankton and autotrophic ultraplankton was studied by the Landry dilution method. Microzooplankton grazing on phytoplankton 〉6 µm was studied by incubation experiments in the presence and absence of microzooplankton. Mesozooplankton grazing was studied by measuring per capita clearance rates of individual zooplankton with radioactively labelled food organisms and estimating in situ rates from abundance values. Protozoan grazing rates on heterotrophic bacteria and on algae 〈6 µm were high (bacteria: 0.7 to 1.1 d-1, ultraphytoplankton: 0.7 to 1.3 d-1), while grazing rates on Synechococcus spp. were surprisingly low and undetectable in some experiments. Mesozooplankton grazing was weak, cumulative grazing rates being ca. 2 orders of magnitude smaller than the grazing rates by protozoans. Among mesozooplankton, appendicularians specialised on smaller food items and calanoid copepods on larger ones.
    Type: Article , PeerReviewed
    Format: text
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 7
    facet.materialart.
    Unknown
    PANGAEA
    In:  Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven
    Publication Date: 2023-03-16
    Keywords: ANT-XXIV/1; Atlantic Ocean; AWI_PhyOce; CT; DATE/TIME; DEPTH, water; LATITUDE; LONGITUDE; Physical Oceanography @ AWI; Polarstern; PS71; PS71/1-track; Salinity; Temperature, water; Thermosalinograph; TSG; Underway cruise track measurements
    Type: Dataset
    Format: text/tab-separated-values, 8048 data points
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 8
    facet.materialart.
    Unknown
    PANGAEA
    In:  Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven
    Publication Date: 2023-03-17
    Keywords: Ciska; CISKA2005; CISKA2005_01-1; CISKA2005_02-1; CISKA2005_03-1; CISKA2005_04-1; CISKA2005_05-1; CISKA2005_06-1; CISKA2005_07-1; CISKA2005_08-1; CISKA2005_09-1; CISKA2005_10-1; CISKA2005_11-1; CISKA2005_12-1; CISKA2005_13-1; CISKA2005_14-1; CISKA2005_15-1; CISKA2005_16-1; CISKA2005_17-1; CISKA2005_18-1; CISKA2005_19-1; CISKA2005_20-1; CISKA2005_21-1; CISKA2005_22-1; CISKA2005_23-1; CISKA2005_24-1; CISKA2005_25-1; CISKA2005_26-1; CISKA2005_27-1; CISKA2005_28-1; CISKA2005_29-1; CISKA2005_30-1; CISKA2005_31-1; CISKA2005_32-1; CISKA2005_33-1; CISKA2005_34-1; CISKA2005_35-1; CISKA2005_36-1; CISKA2005_37-1; CISKA2005_38-1; CISKA2005_39-1; CISKA2005_41-1; CISKA2005_42-1; CISKA2005_43-1; CISKA2005_44-1; CISKA2005_45-1; CISKA2005_46-1; CISKA2005_47-1; CISKA2005_48-1; CISKA2005_49-1; CISKA2005_50-1; CISKA2005_51-1; CISKA2005_52-1; CISKA2005_53-1; CISKA2005_54-1; CISKA2005_55-1; CISKA2005_56-1; CTD, Sea-Bird, SBE 19plus; CTD/Rosette; CTD-RO; Date/Time of event; DEPTH, water; Elevation of event; Event label; Latitude of event; Longitude of event; Makasar Strait; Salinity; Science for the Protection of Indonesian Coastal Environment; SPICE; Temperature, water
    Type: Dataset
    Format: text/tab-separated-values, 4162 data points
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 9
    facet.materialart.
    Unknown
    PANGAEA
    In:  Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven
    Publication Date: 2023-03-16
    Keywords: APN; Apstein plankton net; Chlorophyll a; Ciska; CISKA2005; CISKA2005_01-2; CISKA2005_02-2; CISKA2005_04-2; CISKA2005_06-2; CISKA2005_08-2; CISKA2005_10-2; CISKA2005_11-2; CISKA2005_13-2; CISKA2005_16-2; CISKA2005_19-2; CISKA2005_20-2; CISKA2005_21-2; CISKA2005_24-2; CISKA2005_27-2; CISKA2005_30-2; CISKA2005_33-2; CISKA2005_35-2; CISKA2005_37-2; CISKA2005_38-2; CISKA2005_39-2; CISKA2005_43-2; CISKA2005_46-2; CISKA2005_47-2; CISKA2005_50-2; CISKA2005_53-2; Date/Time of event; DEPTH, water; Elevation of event; Event label; High Performance Liquid Chromatography (HPLC); Latitude of event; Longitude of event; Makasar Strait; Science for the Protection of Indonesian Coastal Environment; SPICE
    Type: Dataset
    Format: text/tab-separated-values, 63 data points
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 10
    facet.materialart.
    Unknown
    PANGAEA
    In:  Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven
    Publication Date: 2023-03-16
    Keywords: Amundsen Sea; ANT-III/3; ANT-IX/2; ANT-V/2; ANT-V/3; ANT-X/3; ANT-X/4; ANT-X/7; ANT-XI/3; ANT-XII/4; ANT-XXI/2; ANT-XXII/2; Bellingshausen Sea; CTD/Rosette; CTD-RO; DATE/TIME; Depth, bottom/max; Depth, top/min; DEPTH, water; ELEVATION; Event label; Gonad stage, ripe; Gonad stage, semi-ripe; Gonad stage, semi-spent; Gonad stage, spent; Gonad stage, unripe; LATITUDE; LONGITUDE; Marguerite Bay; MSN; MSN100; MULT; Multiple investigations; Multiple opening/closing net; Multiple opening/closing net, 100 µm meshsize; Polarstern; PS06/275; PS06/277; PS06/278; PS06/279; PS06/329; PS06/331; PS06/332; PS06/333; PS06/334; PS06 SIBEX; PS10/315; PS10/317; PS10/320; PS10/512-1; PS10/513-7; PS10/514-10; PS10/516-4; PS10/522-3; PS10/561-7; PS10/562-4; PS10/565-6; PS10/566-7; PS10/567-5; PS10/570-3; PS10/604-10; PS10/607-1; PS10/608-3; PS10/611-5; PS10/611-6; PS10/614-3; PS10/614-4; PS10/618-8; PS10/623-3; PS10 WWSP86; PS18/108; PS18/115; PS18 06AQANTIX_2; PS21; PS21/359; PS21/367; PS21/369; PS21/373; PS21/452; PS21/455; PS21/461; PS21/467; PS21/472; PS21/474; PS21/475; PS21/477; PS21/603; PS21/612; PS21 06AQANTX_4; PS23/013; PS23/015; PS23/019; PS23/021; PS23/080; PS23/084; PS23 06AQANTX_7; PS29; PS29/010; PS29/011; PS29/013; PS29/016; PS29/018; PS29/020; PS29/022; PS29/024; PS29/054; PS35/104; PS35/107; PS35/110; PS35/113; PS35/117; PS35/134; PS35 06AQANTXII_4; PS65/141-1; PS65/170-1; PS65/207-1; PS65/242-1; PS65/256-1; PS65/263-1; PS65/286-1; PS65/295-1; PS65/304-1; PS65 BENDEX; PS67/006-112; PS67/006-129; PS67/006-145; PS67/006-16; PS67/006-31; PS67/006-46; PS67/006-58; PS67/006-77; PS67/006-97; PS67 ISPOL; South Pacific; Weddell Sea
    Type: Dataset
    Format: text/tab-separated-values, 1450 data points
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
Close ⊗
This website uses cookies and the analysis tool Matomo. More information can be found here...