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| DC 欄位 | 值 | 語言 |
|---|---|---|
| dc.contributor.advisor | 魏國彥(Kuo-Yen Wei) | |
| dc.contributor.author | Matteo Ternelli | en |
| dc.contributor.author | 毛特立 | zh_TW |
| dc.date.accessioned | 2021-05-16T16:18:29Z | - |
| dc.date.available | 2014-08-20 | |
| dc.date.available | 2021-05-16T16:18:29Z | - |
| dc.date.copyright | 2013-08-20 | |
| dc.date.issued | 2013 | |
| dc.date.submitted | 2013-08-15 | |
| dc.identifier.citation | Anderson C.; 1997, Transfer function vs. modern analog technique for estimating Pliocene sea-surface temperatures based on planktonic foraminiferal data, western equatorial Pacific Ocean, Journal foraminiferal research, Volume 27-2, Page 123 – 132.
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| dc.identifier.uri | http://tdr.lib.ntu.edu.tw/jspui/handle/123456789/5932 | - |
| dc.description.abstract | Late Pliocene has been recognized as a good analog to the possible future global warming condition since it is warmer than toady, but already in a glacial-interglacial fluctuation mode. Pacific Ocean, and in particular, the West Pacific Warm Pool, is a key area of great interest for studying the climate evolution in the global warming context.
We have reconstructed sea-surface salinities and temperatures of the West Pacific Warm Pool using oxygen isotopic (δ18O) and Mg/Ca ratio of planktonic foraminifera. The studied species are Neogloboquadrina dutertrei and its ancestor, Neogloboquadrina humerosa. The specimens were picked from the late Pliocene – early Pleistocene section of the deep-sea core ODP 1115B retrieved from the southern margin of the West Pacific Warm Pool off the east coast of Papua New Guinea. The δ18O curve shows a gradual increasing trend of about 0.6-0.7 permil. In addition, it appears that the periodicities the cycles changes from circa 11 thousand years to more than 14 thousand years. Comparison of it a δ18O curve of the subsurface from DSDP 214 in north-east Indian Ocean, shows an already ceased exchange of water between Indian Ocean and the WPWP. Comparison with surface δ18O shows possible variation of the thermocline. Similar trends exist in the sea surface condition in at least two occasions: between 3.05 and 3.15 million years ago and between 2.45 and 2.55 million years ago. Comparing the surface and thermocline δ18O of our site with surface and thermocline δ18O of the ODP 851 (east equatorial Pacific) reveal a consistent trend between the two sides of the ocean, and shows an ENSO-like condition in the Pacific Ocean around 2.1 – 2.2 Ma, with difference in sea surface value and tilting in the thermocline, shoal in east Pacific, more deep in west Pacific; corroborating with the hypothesis that the thermocline structure changed due to the formation of the Panama’s Isthmus and the closure of the Indonesian Seaway (Cane et al., 2001; Haug et al., 1998). Comparison of δ13C reveals a connection between Caribbean area deep ocean ventilation (ODP 999), east Pacific (ODP 851) upwelling and carbon isotope ratio (Haug & Tiedemann 1998, Steph et al. 2010) and the west Pacific water ventilation, although with some light variation, the trend is similar and the main changes are followed by all the three sites, although the curves of the Pacific started their trend from a lower value, after an abrupt increase around 3.0 Ma and then show a similar trend with that of the west Atlantic sites. | en |
| dc.description.provenance | Made available in DSpace on 2021-05-16T16:18:29Z (GMT). No. of bitstreams: 1 ntu-102-R99224115-1.pdf: 7323101 bytes, checksum: 61b600ce00fce799cb873928477294c5 (MD5) Previous issue date: 2013 | en |
| dc.description.tableofcontents | Table of contents
Acknowledgment s 03 Abstract 04 Table of contents 06 List of figures 08 List of tables 10 1. Introduction 11 1.1. Purposes of this study 11 1.2. Background information 12 1.2.1. Pliocene-Pleistocene periods, global conditions 12 1.2.2. Permanent El Niño-like situation 15 1.2.3. North hemisphere glaciation 18 1.2.4. Panama Isthmus closure 20 1.2.5. Indonesian Gateway 23 1.2.6. Consequence of the Panama’s Isthmus closure 27 1.2.7. Consequences of the closure of the Indonesian Seaway 30 1.3. Thermocline 32 1.3.1. Definition of thermocline 32 1.3.2. Concept of the thermocline 33 1.3.3. Seasonal variation of the thermocline 34 1.3.4. Modality of measuring the thermocline 35 2. Materials and Methods 37 2.1. Leg 180, ODP 1115B and core description 37 2.1.1. ODP 1115B and Led 180 38 2.1.1.1. Biostratigraphy 41 2.2. Literature review 42 2.3. Neogloboquadrina’s Lineage 44 2.3.1. Distinction criteria 50 2.4. Analytic procedures 55 2.4.1. Brief introduction of the methods 55 2.4.2. Sample preparation procedures 57 3. Results 66 3.1. δ18O and Mg/Ca 72 3.2. Mg/Ca 74 3.3. δ13C 76 3.4. Spectral analyses 77 4. Discussion 78 4.1. Isotopic analyses correction 78 4.2. WPWP and north-east Indian Ocean thermocline water exchange 82 4.3. East and west Pacific thermocline, sea surface and ENSO-like state 85 4.4. Enhancing of the AMOC, east Pacific deep water upwelling and west Pacific water ventilation 89 5. Conclusions 93 References 96 Appendix 103 a. Data table (core’s data, n° specimens) 103 b. Data table (sample data: δ18O, δ13C, Mg/Ca, Temp.) 111 c. Tectonic history of the Woodlark Basin and the surrounding area 119 | |
| dc.language.iso | en | |
| dc.subject | Pliocene. | zh_TW |
| dc.subject | Neogloboquadrina dutertrei | zh_TW |
| dc.subject | Neogloboquadrina Humerosa | zh_TW |
| dc.subject | thermocline | zh_TW |
| dc.subject | West Pacific Warm Pool | zh_TW |
| dc.title | the variation of the thermocline structure in the southern marginal West Pacific Warm Pool during 2.2-3.2 million years ago | en |
| dc.type | Thesis | |
| dc.date.schoolyear | 101-2 | |
| dc.description.degree | 碩士 | |
| dc.contributor.coadvisor | 米泓生(Horng-Sheng Mii) | |
| dc.contributor.oralexamcommittee | 沈川洲(Chuan-Chou Shen),陳明德(Min-Te Chen) | |
| dc.subject.keyword | Neogloboquadrina dutertrei,Neogloboquadrina Humerosa,thermocline,West Pacific Warm Pool,Pliocene., | zh_TW |
| dc.relation.page | 124 | |
| dc.rights.note | 同意授權(全球公開) | |
| dc.date.accepted | 2013-08-15 | |
| dc.contributor.author-college | 理學院 | zh_TW |
| dc.contributor.author-dept | 地質科學研究所 | zh_TW |
| 顯示於系所單位： | 地質科學系 | |
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