Biology
provided by Arctic Ocean Biodiversity 2011
One of most abundance shelf copepods of Arctic shelves
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Life Cycle
provided by Arctic Ocean Biodiversity 2011
Females beginning spawn in spring at least partly based on lipid reserves from previous year, with continued reproduction throughout the summer; Female carries eggs in a single large clutch until hatching; Clutch size dependent on size of female with maximums of ~60 and typically ~30 eggs; Generation length estimated at 1 year; Life expectancy unknown
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Trophic Strategy
provided by Arctic Ocean Biodiversity 2011
Suspension "filter" feeder on phytoplankton and protists; Lipid deposits accumulated for over-wintering; Thought to be one of the arctic's key grazers in shelf waters
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Comprehensive Description
provided by Arctic Ocean Biodiversity 2011
Body almost completely transparent, red color may be prominent on posterior quarter of prosome, mouth parts, and/or parts of the urosome (the tail); Lipid sac can be prominent; Urosome (tail) somewhat long (~40% of prosome); Antennae longer then prosome, but less than total length; Anterior of body somewhat peaked with prominent spines on posteriot ventral margins of thorathic segments I & II
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Habitat
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Boreal to arctic waters; Abundant on shelves, limited occurrence over deep basins; Outside of the Arctic, it moves into deeper, colder waters seasonally
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Pseudocalanus minutus
provided by wikipedia EN
Pseudocalanus minutus is a small copepod found in the Arctic Ocean and surrounding waters.
Description
A small copepod,[1] the female is generally between 1 and 2.15 millimetres (0.039 and 0.085 in), and the male typically between .85 and 1.6 millimetres (0.033 and 0.063 in) in length.[2]
Distribution
P. minutus is found primarily in the Arctic, but it is also found in the northwest Atlantic, the northern Pacific,[2] and more temperate waters where Atlantic and Arctic waters are mixed.[1]
Ecology
Life cycle and reproduction
In Toyama Bay, P. minutus reproduces from February to April, producing two generations. This is during the temperature minimum (of about 10 to 12 °C (50 to 54 °F)) and phytoplankton maximum. All stages are found at shallower depths during the night (diel vertical migration) in Toyama Bay during this time. During the annual temperature maximum (of over 26 °C (79 °F)) in September, stage V copepodites migrate (possibly gradually) to deeper, colder waters to diapause (in contrast to the congeneric P. newmani, which does not seem to be able to diapause). They moult to adults before January, rising to the surface to breed.[3] In Kongsfjorden, P. minutus reproduces during May and June, producing one generation (consistent with a trend for higher latitude populations to produce less generations). It descends in autumn and winter[a] to depths below 100 metres (330 ft) as a stage III to stage V copepodite. Females and stage I copepodites are found throughout the water column during November. From June and July till May, younger stages tend to be found towards the surface, and older stages tend to migrate to overwinter earlier.[1] It develops during the winter and reproduces with energy gained from the spring phytoplankton bloom, indicating a one year life cycle.[4]
Feeding
P. minutus is opportunistic, being mainly herbivorous except during the winter, when it is either carnivorous or omnivorous.[4]
References
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^ All seasons are for the Northern Hemisphere
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^ a b c Lischka, Silke; Hagen, Wilhelm (2005). "Life histories of the copepods Pseudocalanus minutus, P. acuspes (Calanoida) and Oithona similis (Cyclopoida) in the Arctic Kongsfjorden (Svalbard)". Polar Biology. 28 (12): 910–921. doi:10.1007/s00300-005-0017-1. ISSN 0722-4060.
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^ a b Razouls C.; de Bovée F.; Kouwenberg J.; Desreumaux N. (2018). "Diversity and Geographic Distribution of Marine Planktonic Copepods". Sorbonne Université, CNRS. Retrieved 20 October 2018.
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^ Yamaguchi, Atsushi; Ikeda, Tsutomu; Shiga, Naonobu (1998). "Population structure and life cycle of Pseudocalanus minutus and Pseudocalanus newmani (Copepoda: Calanoida) in Toyama Bay, southern Japan Sea". Plankton Biology and Ecology. 45 (2).
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^ a b Lischka, Silke; Hagen, Wilhelm (2007). "Seasonal lipid dynamics of the copepods Pseudocalanus minutus (Calanoida) and Oithona similis (Cyclopoida) in the Arctic Kongsfjorden (Svalbard)". Marine Biology. 150 (3): 443–454. doi:10.1007/s00227-006-0359-4. ISSN 0025-3162.
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Pseudocalanus minutus: Brief Summary
provided by wikipedia EN
Pseudocalanus minutus is a small copepod found in the Arctic Ocean and surrounding waters.
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Distribution
provided by World Register of Marine Species
Saguenay Fjord, northern Gaspe waters, southern Gaspe waters (Baie des Chaleurs, Gaspe Bay to American, Orphan and Bradelle banks; eastern boundary: eastern Bradelle Valley), downstream part of middle St. Lawrence estuary, Magdalen Islands (from Eastern Bradelle valley to the west, as far as Cape North, including the Cape Breton Channel), lower St. Lawrence estuary, Prince Edward Island (from the northern tip of Miscou Island, N.B. to Cape Breton Island south of Cheticamp, including the Northumberland Strait and Georges Bay to the Canso Strait causeway), Upper Laurentian Channel (bathyal zone off Sept- Iles), middle North Shore (from Sept- Iles to Cape Whittle, including the Mingan Islands), Laurentian Channel (bathyal zone)(=Honguedo Strait), lower North Shore, Laurentian Channel (bathyal zone)(=Esquiman Channel), lower Laurentian Channel (bathyal zone as far as Cabot Strait: Cape North, N.S., St. Paul Island to Cape Ray, NL.), North slope of Anticosti Island; western slope of Newfoundland, including the southern part of the Strait of Belle Isle but excluding the upper 50m in the area southwest of Newfoundland
North-West Atlantic Ocean species (NWARMS)
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Habitat
provided by World Register of Marine Species
upper mesopelagic, and upper epipelagic of the Gulf and estuary
North-West Atlantic Ocean species (NWARMS)
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