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Calanus sinicus

species of crustacean

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Record originEnglish Wikipedia
Text licenseCC BY-SA 4.0
Source revisionAug 17, 2023
Entity authorityQ6552371
Source-derived summary

Calanus sinicus is a copepod found in the northwest Pacific.

Description

The female C. sinicus generally ranges from about 2.1 to 3.6 millimetres (0.083 to 0.142 in). The male generally ranges between about 2 and 3.5 millimetres (0.079 and 0.138 in). For adults and copepodite stages IV and above, lower temperatures result in longer prosomes.

Distribution

C. sinicus is found in the northwest Pacific, off of the east coast of Asia to the South China Sea.

Ecology

Life cycle and reproduction

C. sinicus reproduces throughout the year. There are generally two peaks in reproduction. In the southern Yellow Sea, these peaks occur from May to July and from November to January. These peaks occur when the temperatures throughout the water column fall into its preferred temperature range of 10 to 23 °C (50 to 73 °F). It can tolerate ranges between 1 and 27 °C (34 and 81 °F) for limited periods of time, and can reproduce between about 5 and 23 °C (41 and 73 °F).

Editorial summary

Begin with the source’s own compact description: “Calanus sinicus” is species of crustacean. The dossier treats that line as a proposition to test through Calanus, sinicus and species, not as a finished interpretation.

Editorial reviewA practical orientation to terminology and classification, particularly when read beside dated observations, specimens or technical literature. The current 167-word lead offers orientation but no explicit four-digit date, so chronology should not be assumed. The selected authority fields contribute no independent date. For this dossier, Calanus, sinicus and species is the immediate research focus.
Editorial analysis

Why this record matters

The phrase “species of crustacean” supplies a clear boundary for inquiry. It also exposes the unanswered questions: who defined that boundary, when it became stable and which sources sit outside it.

Evidence profile

Datasets, specimens, observations and peer-reviewed methods provide the appropriate test for the technical claims summarized here. The source revision retrieved here is dated Aug 17, 2023. The linked authority identifier is Q6552371. None of the 0 selected statements returned an explicit reference.

Critical limits

A general summary may omit uncertainty, sample limits or methodological disagreement that is explicit in the technical record. The source lead contains qualifying language; that uncertainty should survive quotation, summary and reuse. Authority statements aid reconciliation but still require their own references, qualifiers and ranks to be checked.

How to read it

Check terminology, classification and the date of the cited evidence. Scientific names and technical consensus can change while older records retain historical value.

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  • Classification context
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Primary datasets, specimen catalogues, standards bodies and the most recent peer-reviewed literature.

Three-step research path

  1. Establish the record: confirm the title “Calanus sinicus”, its source revision and the description used here.
  2. Expand the search: follow Calanus sinicus primary sources, Calanus sinicus archive and Calanus research across catalogues and specialist indexes.
  3. Test the account: compare the strongest cited source with the responsible institution’s current record and note any disagreement.

Questions for further research

  1. Which source most directly establishes the central claim about “Calanus sinicus”?
  2. Which observation, specimen, dataset or publication supports the account?
  3. Is the terminology current, historical or disputed?
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Source & attribution

This entry incorporates text from Calanus sinicus” on English Wikipedia. Contributors are listed in the page history. Text is available under the Creative Commons Attribution-ShareAlike 4.0 License. Selected authority identifiers and statements are retrieved from Wikidata under CC0; their references and qualifiers remain part of the verification path.