Tiong-sin-sè
| Hē/ Kí | Thóng/ Sè | Kai/ Kî | Sî-kî (Ma) | |
|---|---|---|---|---|
| Tē-sì-kí | Keng-sin-sè | Gela-kî | khah sin | |
| Sin-chiâⁿ-kí | Sian-sin-sè | Piacenza-kî | 2.58 | 3.600 |
| Zancle-kî | 3.600 | 5.333 | ||
| Tiong-sin-sè | Messina-kî | 5.333 | 7.246 | |
| Tortona-kî | 7.246 | 11.63 | ||
| Serravalle-kî | 11.63 | 13.82 | ||
| Langhe-kî | 13.82 | 15.97 | ||
| Burdigala-kî | 15.97 | 20.44 | ||
| Aquitaine-kî | 20.44 | 23.03 | ||
| Kó͘-seⁿ-kí | Chiām-sin-sè | Chatti-kî | khah kó͘ | |
| Sin-seⁿ-kí ê hun-koah, kun-kù ICS tī 2017 nî ê chu-liāu.[1] | ||||
Tiong-sin-sè (Eng-gí: Miocene) sī tē-chit sî-tāi lāi-bīn Sin-seⁿ-kí ê thâu chi̍t tōaⁿ, sî-kan tùi 23.03 kàu 5.332 pah-bān-nî-chêng.
Pún sî-kî ê hō-miâ sī Charles Lyell tēng--ê, chhú Hi-lia̍p-gí meiōn (μείων, "khah-kiám") kap kainos (καινός, "sin"), ì-sù sī "bô hiá-nī kīn", in-ūi pún sî-tāi ê tōng-bu̍t pí Sian-sin-sè (Pliocene) koh khah kó͘.
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