Sin-chiâⁿ-kí

Sin-chiâⁿ-kí 23.03–23.03 百萬年前 PreЄ Є O S D C P T J K Pg N
通時期的平均大氣O 2 含量	約。21.5體積 %^[1]^[2] (現代水準的 108%)
通時期的平均大氣CO 2 含量	約。280ppm^[3] (工業時代進前水準的1背)
通時期的平均表面溫度	約。14 °C^[4] (權過現代水準 0 °C)
先生紀的關鍵事件 -18 — – -18 — – -18 — – -18 — – -18 — – -18 — – -18 — – -18 — – -18 — – -18 — – -18 — – -18 — – -18 — – -18 — – -18 — – -18 — – -18 — – -18 — – -18 — – -18 — – -18 — – -18 — – -18 — – -18 — – -18 — – -18 — – -18 — – -18 — – -18 — – -18 — – -18 — – S i n s e n g t 也 i 古成紀 S i n c h i â ⁿ k 以第四紀 T i o n g s i n s 裔 S 伊 a n s 伊 n s 裔 Aquitaine其 Burdigala其 Langhe其 Serravalle其 Tortona其 Messina其 Zancle其 Piacenza其 ← Messina鹽度危機^[5] ← 完新世開始佇11.7家從 <div class="annot-bar" style=" width:auto; font-size:100%; position:absolute; text-align:center; margin-top:Biēu-dăk-sék ô dâng:ê̤ṳ-gĭ cī-nguôi gì < ông-sáung-cṳ̄.em; "> <div class="annot-bar" style=" width:auto; font-size:100%; position:absolute; text-align:center; margin-top:Biēu-dăk-sék ô dâng:ê̤ṳ-gĭ cī-nguôi gì < ông-sáung-cṳ̄.em; "> <div class="annot-bar" style=" width:auto; font-size:100%; position:absolute; text-align:center; margin-top:Biēu-dăk-sék ô dâng:ê̤ṳ-gĭ cī-nguôi gì < ông-sáung-cṳ̄.em; "> <div class="annot-bar" style=" width:auto; 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font-size:100%; position:absolute; text-align:center; margin-top:Biēu-dăk-sék ô dâng:ê̤ṳ-gĭ cī-nguôi gì < ông-sáung-cṳ̄.em; "> <div class="annot-bar" style=" width:auto; font-size:100%; position:absolute; text-align:center; margin-top:Biēu-dăk-sék ô dâng:ê̤ṳ-gĭ cī-nguôi gì < ông-sáung-cṳ̄.em; "> <div class="annot-bar" style=" width:auto; font-size:100%; position:absolute; text-align:center; margin-top:Biēu-dăk-sék ô dâng:ê̤ṳ-gĭ cī-nguôi gì < ông-sáung-cṳ̄.em; "> 關kiàn先生紀事件的約略時間尺. 直尺: 百萬冬前.

新成紀 (Sin-chiâⁿ-kí) (應 (eng)。Neogene period; 日 (ji̍t)。新成紀^[6]) 是 (sī)一 (chi̍t)段 (toāⁿ)地質 (tē-chit)時代 (sî-tāi)，時間 (sî-kan)是23.03到 (kàu)2.58百萬年 (pah-bān-nî)前 (chêng)之 (chi)間 (kan)。本 (Pún)時代是以早 (í-chá)講的 (kóng--ê)第三紀 (tē-saⁿ-kí) (tertiary period) 的 (ê)後 (āu)段 (tōaⁿ)。

站 (Tiām)這个 (chit-ê)時期 (sî-kî)，市奶類 (chhī-leng-lūi)佮 (kap)鳥類 (chiáu-lūi)繼續 (kè-sio̍k)向 (hiòng)現代 (hiān-tāi)形體 (hêng-thé)進化 (chìn-hòa)，同時 (tông-sî)其他 (kî-tha)的生物 (seng-bu̍t)相對 (siong-tùi)較 (khah)無 (bô)變化 (piàn-hòa)。上 (Siōng)早 (chá)的人科 (lâng-kho)動物 (tōng-bu̍t)佇 (tī)時期的尾 (bóe)塹 (chām)出現 (chhut-hiān)佇非洲 (Hui-chiu)。大陸 (Tāi-lio̍k)的徙動 (sóa-tāng)內面 (lāi-bīn)較活顯的 (oa̍h-hiáⁿ--ê)是鮮新世 (Sian-sin-sè)尾期 (bóe-kî)北 (Pak)美洲 (Bí-chiu)佮南 (Lâm)美洲的相接 (sio-chiap)，這个事件 (sū-kiāⁿ)切 (chhiat)斷 (tn̄g)了 (liáu)太平洋 (Thài-pêng-iûⁿ)佮大西洋 (Tāi-se-iûⁿ)之間的燒熱 (sio-joa̍h)溶瘤 (iûⁿ-liû)。

佇新成紀，地球 (Tē-kiû)的運動 (ūn-tōng)明顯 (bêng-hián)降低 (kàng-kē)，綴尾 (tè-bé)引 (ín)chhōa入 (ji̍p)第四紀 (Tē-sì-kí)的濟 (chē)改 (kái)兵荷華 (peng-hô-hòa) (glaciation)。

參照 (Chham-chiàu)[修改]

↑ Image:Sauerstoffgehalt-1000mj.svg
↑ File:OxygenLevel-1000ma.svg
↑ Image:Phanerozoic Carbon Dioxide.png
↑ Image:All palaeotemps.png
↑ Krijgsman， W。; Garcés， M。; Langereis， C。 G。; Daams， R。; Van Dam， J。; Van Der Meulen， A。 J。; Agustí， J。; Cabrera， L。 (1996). "A new chronology for the middle to late Miocene continental record in Spain". Earth and Planetary Science Letters. 142 (3-4): 367–380. Bibcode:1996E&PSL.142..367K. doi:10.1016/0012-821X(96)00109-4.
↑ 鈴木寿志 & 石田志朗 (2005). "PalaeogeneとNeogeneに対応する日本語について". 111 (9): 565–568. doi:10.5575/geosoc.111.565.

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

[1] Image:Sauerstoffgehalt-1000mj.svg

[2] File:OxygenLevel-1000ma.svg

[3] Image:Phanerozoic Carbon Dioxide.png

[4] Image:All palaeotemps.png

[Krijgsman1996-5] Krijgsman， W。; Garcés， M。; Langereis， C。 G。; Daams， R。; Van Dam， J。; Van Der Meulen， A。 J。; Agustí， J。; Cabrera， L。 (1996). "A new chronology for the middle to late Miocene continental record in Spain". Earth and Planetary Science Letters. 142 (3-4): 367–380. Bibcode:1996E&PSL.142..367K. doi:10.1016/0012-821X(96)00109-4.

[6] 鈴木寿志 & 石田志朗 (2005). "PalaeogeneとNeogeneに対応する日本語について". 111 (9): 565–568. doi:10.5575/geosoc.111.565.

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Sin-chiâⁿ-kí

參照 (Chham-chiàu)[修改]

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