Cambria-kì

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.

[siu-kái] Siong-koan

[siu-kái] Chham-khó chu-liāu

↑ Gradstein, Felix M. (2004). A Geologic Time Scale 2004. Cambridge: Cambridge University Press. ISBN 0521786738.

Chit phiⁿ bûn-chiuⁿ sī chi̍t ê phí-á-kiáⁿ. Chhiáⁿ tàu siu-kái hō͘ i ū phong-phài ê lōe-iông.

[ICS2004-0] Gradstein, Felix M. (2004). A Geologic Time Scale 2004. Cambridge: Cambridge University Press. ISBN 0521786738.

[1]

Cambria-kì

[siu-kái] Siong-koan

[siu-kái] Chham-khó chu-liāu

Kò-jîn kang-khū

Miâ-khong-kan

piàn-thé

Khoàⁿ

Tōng-chok

Chhiau-chhoē

Se̍h chām

Pian-chi̍p

Ke-si kheh-á

Kî-thaⁿ ê gí-giân