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| DC 欄位 | 值 | 語言 |
|---|---|---|
| dc.contributor.advisor | 沈川洲(Chuan-Chou Shen) | |
| dc.contributor.author | Yun-Chuan Chung | en |
| dc.contributor.author | 鍾昀娟 | zh_TW |
| dc.date.accessioned | 2021-06-08T03:39:26Z | - |
| dc.date.copyright | 2019-07-15 | |
| dc.date.issued | 2019 | |
| dc.date.submitted | 2019-07-10 | |
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| dc.identifier.uri | http://tdr.lib.ntu.edu.tw/jspui/handle/123456789/21603 | - |
| dc.description.abstract | The orbital parameters during marine isotope stage (MIS) 5a, 85.8-76.0 thousand years ago (ka, before AD 1950), after an abrupt global temperature rise from MIS 5b, 95.0-85.8 ka, are similar with those during Holocene. However, it is still a controversial analogue for comparison of the climate fluctuations in MIS 5a and Holocene. In addition, lack of paleoclimate records with good age-control from MIS 5a hampers our understanding of regional climatic change and corresponding global links on centennial-to-millennial scales. Here, we present a 230Th-dated stalagmite δ18O-inferred precipitation time series during 83.7-80.2 ka from Observatoire Cave (43°44’N, 7°25’E), Monaco, southern Europe. The record shows a millennial-scale decreasing trend in precipitation from 83.7 to 82.5 ka punctured by an abrupt 200-year wet event at 82.7 ka and a rapid shift from aridity to wetness during 82.5-82.4 ka, followed by relatively stable conditions until 80.2 ka in southern Europe. This hydroclimatic variability is consistent with changes in seawater circulation in the Mediterranean during sapropel 3 and an ice rafted debris event in the Nordic Sea on multi-centennial-to-millennial scales. Consistent with published proxy records, the results reveal that southern Europe hydroclimate influenced water circulation in the Mediterranean, and a strong connection between mid-latitude and high-latitude climate systems. The indistinguishable differences between regional hydroclimate at the early stage MIS 5a and in Holocene imply a similar clime system in this two periods in southern Europe. | en |
| dc.description.provenance | Made available in DSpace on 2021-06-08T03:39:26Z (GMT). No. of bitstreams: 1 ntu-108-R04224209-1.pdf: 1914321 bytes, checksum: 0b50b65ac2f6bd8c9a5211c56370da98 (MD5) Previous issue date: 2019 | en |
| dc.description.tableofcontents | Abstract i
摘要 ii Content iii List of figures/tables v Chapter 1 Introduction 1 Chapter 2 Regional setting and methods 4 2.1 Study material and site setting 4 2.2 Experimental procedure 7 2.2.1 Subsamples for U-Th dating 7 2.2.2 Subsamples for δ18O and δ13C analysis 7 2.2.3 Labware for chemical procedure of U-Th dating 8 2.2.4 U-Th dating chemical procedure 8 2.2.5 U-Th dating instrumentation 11 2.2.6 Stable oxygen isotope analysis instrumentation 11 Chapter 3 Results 12 3.1 U-Th dating results and age model 12 3.2 Oxygen stable isotope records 14 3.2.1 Hendy test 14 3.2.2 Oxygen stable isotope series 15 Chapter 4 Discussion 17 4.1 Interpretation of δ18O variations 17 4.2 Comparison with regional paleoclimate proxy records 19 4.3 Comparison with global paleoclimate proxy records 23 4.4 Comparison with Holocene record 25 Chapter 5 Conclusions 28 Reference 29 Appendix 34 Figure 1.1 Climatic Hot-Spots. 1 Figure 1.2 Comparison of Asian monsoon (AM) and NHSI. (a) NHSI at 65°N 2 Figure 1.3 Earth’s orbital parameters and AM variations from MIS 15 3 Figure 2.1 The locations of Observatoire Cave and other terrestrial and marine sites mentioned in this study 5 Figure 2.2 The map and the photos of the collection site 6 Figure 2.3 Monthly average rainfall and temperature data 6 Figure 2.4 The photo of halved and polished stalagmite with subsamples marks 7 Figure 3.1 The plot of sample depth versus age 14 Figure 3.2 Hendy test results 15 Figure 3.3 The plot of the Observatoire OV12-5 δ18O time series 16 Figure 4.1 Comparison of Observatoire OV12-5 with adjacent Campanet CAM-1 records 19 Figure 4.2 Comparison of Observatoire OV12-5 δ18O series with regional proxy records and relative sea level (RSL) record 22 Figure 4.3 Comparison of Observatoire OV12-5 δ18O series with global proxy records 24 Figure 4.4 Comparison of Observatoire OV12-5 δ18O series with adjacent Holocene stalagmite record. 26 Figure 4.5 The wavelet analyses of Observatoire OV12-5 and Toirano BA14-1 δ18O series 27 Table 1 U-Th isotopic measurements for Observatoire OV12-5 on MC-ICP-MS 13 | |
| dc.language.iso | en | |
| dc.title | 海洋同位素階5a時期南歐地區的氣候震盪 | zh_TW |
| dc.title | Southern Europe climate oscillations at marine isotope stage 5a | en |
| dc.type | Thesis | |
| dc.date.schoolyear | 107-2 | |
| dc.description.degree | 碩士 | |
| dc.contributor.oralexamcommittee | 米泓生(Horng-Sheng Mii),李時雨(Shih-Yu Lee),張詠斌(Yuan-Pin Chang) | |
| dc.subject.keyword | 海洋同位素階5a,南歐,氣候震盪,石筍, | zh_TW |
| dc.subject.keyword | marine isotope stage 5a,southern Europe,hydroclimatic oscillations,stalagmite, | en |
| dc.relation.page | 36 | |
| dc.identifier.doi | 10.6342/NTU201901262 | |
| dc.rights.note | 未授權 | |
| dc.date.accepted | 2019-07-10 | |
| 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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