"Cambria-kí" pán-pún chi-kan bô-kāng--ê tē-hng

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行內

2012-nî 9-goe̍h 2-ji̍t (lé-pài) 19:19 ê siu-tēng-pún

Chhui-chhek só͘ chāi ê Hân-bú-kì tē-kiû lio̍k hái hun-pō͘.

Cambria-kì, Hàn-bûn kóng Hân-bú-kì (寒武紀), sī Kó͘-seng-tāi (Paleozoic) lāi-té thâu-chi̍t-ê tē-chit sî-tāi, sî-kan tùi 542 ± 0.3 Ma (pah-bān nî chêng) kàu 488.3 ± 1.7 Ma.^[1] I-ê āu chi̍t tāi sī Ordovices-kì (Ordovician). "Cambria-kì" chit-ê miâ sī tùi "Cambria" (Cymru ê Lô-má miâ) só͘ hō.

Siong-koan

Chham-khó chu-liāu

↑ Gradstein, Felix M. (2004). A Geologic Time Scale 2004. Cambridge: Cambridge University Press. ISBN 0521786738. Cite uses deprecated parameter |coauthors= (help)

Pún bûn-chiuⁿ sī chi̍t phiⁿ phí-á-kiáⁿ. Lí thang tàu khok-chhiong lâi pang-chō͘ Wikipedia.

[ICS2004-1] Gradstein, Felix M. (2004). A Geologic Time Scale 2004. Cambridge: Cambridge University Press. ISBN 0521786738. Cite uses deprecated parameter |coauthors= (help)

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