作者查詢 / paleoworld
作者 paleoworld 在 PTT [ EarthScience ] 看板的留言(推文), 共264則
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1F→:搜尋我的話,會看到有一篇"深海CO2重返大氣..."的文章10/29 10:39
2F→:在討論類似的問題:)也可以當作參考10/29 10:39
5F→:地形上的確是這樣沒錯,感謝補充!05/31 23:51
6F→:我只是好奇為什麼環南極流都可以繞行一周了~還會有05/31 23:52
7F→:不同程度的冷卻與冰川發育作用~而且兩者相隔很廣05/31 23:52
8F→:再來是透過什麼樣的指標分辨西邊跟東邊的發育年代05/31 23:52
13F→:exactly~06/01 09:11
14F→:to s93015a: 有可能,但也可能這個問題的文獻06/01 09:36
15F→:我之前也沒有特別去追~現在想想才覺得不大對勁06/01 09:37
17F→:這個我也不知道哩~06/03 23:05
18F→:不好意思這兩個禮拜要準備進度報告,Oligocene06/19 08:30
19F→:與Miocene的氣候比較少閱讀,先暫停2-3周,感謝06/19 08:31
1F推:晚新世?....HA, 陳于高老師1996年的經典澎湖海水面05/29 00:24
2F→:變化的文章可以找找05/29 00:25
4F→:找找看誰引用過這篇文章囉!05/29 08:53
13F推:找找看誰引用過這篇文章囉~05/29 08:52
14F→:推錯~對不起!05/29 08:53
3F→:是的,但可以證明有季節性的海冰05/31 15:38
1F→:陸續連載,歡迎討論指正!05/19 11:49
7F→:paleocene/eocene boundary, 大約55 Ma05/20 07:18
8F→:歡迎轉載,有問題可以大家一起討論跟指正:)05/20 07:21
6F→:to rssai: 風化作用對氣候大多是指百萬年以上的尺度05/16 11:43
7F→:所以用千年尺度的事件來看的話,生物的作用應該是05/16 11:44
8F→:比較明顯的05/16 11:44
14F→:To s93015a:是的,所以我說是陸續離開。05/16 17:28
15F→:再查了一下,目前認為塔司馬尼亞是跟澳洲一起動的05/16 17:28
16F→:而塔司馬泥亞又比澳洲更南,所以最後離開的海峽05/16 17:29
17F→:是南極與塔司馬泥亞之間的海峽無誤05/16 17:29
21F→:To ntouhr: 沈積物通量的確是個好的想法,但試想一個05/19 11:24
22F→:狀況,這些沈積物,是早就被風化,透過幾次搬運05/19 11:24
23F→:才沈積下來,還是真的是一邊風化一邊就被帶下來呢?05/19 11:25
24F→:這會牽涉到所估計的沈積物通量與風化實際產生的時間05/19 11:25
25F→:有誤差。第二個狀況是:通常大量沈積物輸送堆積的時候05/19 11:26
26F→:年代的控制跟計算會變得相對困難05/19 11:26
30F→:to ntouhr: 當我們在討論一個事件的尺度的時候,除了05/19 15:26
31F→:結果之外,還有另一個很重要的是探討這樣子的事件的05/19 15:27
32F→:趨力(forcing),由於大規模造山運動所造成的風化加速05/19 15:27
33F→:是百萬年尺度的事件,但風化產物的的輸送過程05/19 15:28
34F→:的確有可能是“相對較短”千年-萬年尺度的過程05/19 15:29
35F→:所以這才是利用風化產物的輸送量來研究這樣因造山運動05/19 15:30
36F→:導致風化加速進而影響氣候的事件困難的點05/19 15:30
5F→:可否偷偷透露水深跟區域?XD03/20 01:18
6F→:大學的專題的話我想大概就先寫在大西洋的應用03/20 01:18
7F→:再稍微點出太平洋的不足之處,所以你要做這樣就不錯了03/20 01:19
9F→:got it, ha, 我找一下文章跟你分享03/20 07:06
11F→:我看到Benham Rise就知道了XD03/22 22:05
14F→:三小學長XD03/23 21:33
6F→:羞>///////<12/30 04:23
1F→:冰心的話則有一本半科普的書:two miles timemachine12/20 22:24
4F→:荒漠有甘泉:撒哈拉綠化!~古氣候嚴重中毒症狀XD12/21 00:17
6F→:表水當然有浮游囉!哈哈~其實我也跟底棲很不熟XD12/21 04:45