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| 1 | 末次冰消期以来巽他陆架高分辨率的孢粉记录显示文摘根据南海南部巽他陆坡上的柱状剖面SONNE18287的高分辨率的孢粉记录,重建16500a以来该地区植被和气候的变化历史.研究结果发现冰消期的16.5~13.9kaBP期间,植被是以低山雨林和低地雨林为主,蕨类的低含量及大量的低山雨林成分,反映了较为凉湿的气候.在13.9~10.2kaBP期间,热带低地雨林含量和蕨类植物含量的迅速增长说明了气温升高,而花粉沉积速率的降低反映海平面逐渐上升,研究点与植被源地的距离加大.全新世(10.2kaBP以来),花粉沉积速率进一步降低,仅约为冰消期的1/10,说明巽他陆架已完全被淹没,孢粉主要来自周围岛屿植被.10.2~7kaBP期间的早全新世,低含量的蕨类孢子反映了气温降低;到中全新世(7~3.6kaBP)蕨类孢子含量突然升高,反映了一个相对暖期. | 王晓梅 孙湘君 汪品先 Karl Stattegger | 2007 | 中国科学(D辑)2007，37，1： | 7 |
| 2 | Determination of tectonic background for sedimentary basin from sandstone geochemistry显示文摘The chemical composition of sedimentary rocks is mainly controlled by source rocks. Through examining chemical composition of terrigenous rocks, the tectonic evolution of a sedimentary basin can be modeled. The Turpan Basin belongs to a continental sedimentary basin and its source rocks are derived from the upper continental crust. | SHAO Lei 1, K. Stattegger 2 and LI Wenhou 3 1. Laboratory of Marine Geology, Tongji University, Shanghai 200092, China 2. Geological and Paleontological Institute, University of Kiel, 24118 Kiel, Germany 3. Department of Geology, Northwest Unive | 1998 | Chinese Science Bulletin1998，43，14： | 3 |
| 3 | 末次冰消期以来巽他陆架孢粉、藻类及其古环境意义显示文摘根据南海南部巽他陆坡上的柱状剖面SONNE18287的高分辨率的藻类和孢粉记录,探讨海平面变化和其反映的古环境,得到在16.5—13.9kaBP之间,较高的热带低山雨林百分含量和较低的热带低地雨林含量反映了当时仍较低的气温;各类陆相花粉和环纹藻浓度都很高,而沟鞭藻含量很低,说明当时巽他陆架处于低水位环境;13.9—10.2kaBP期间,热带低山雨林含量的减少和热带低地雨林的增加反映了气温的回升;各类陆相花粉和环纹藻浓度都大大降低,而沟鞭藻含量增加,说明巽他陆架逐渐被淹没;10.2—7kaBP热带低山雨林含量的持续减少和热带低地雨林的增加反映了气温继续缓慢回升;花粉浓度的降低说明陆架完全被淹没,花粉的物源区变远,同时环纹藻浓度的略有增加说明此时有淡水注入;7kaBP各类花粉的百分含量相对稳定,说明气温基本稳定,沟鞭藻浓度的突然降低,说明存在一个气候变冷事件使得海平面升高受到抑制,但接下来沟鞭藻浓度又继续回升,指示温度升高,海平面稳定升高。 | 王晓梅 孙湘君 汪品先 Stattegger K | 2008 | 古生物学报2008，47，3： | 2 |
| 4 | The records of coastline changes reflected by mangroves on the Sunda Shelf since the last 40ka显示文摘This paper presents a 40000-year-long high-resolution mangrove record from sediments of Core 18300,18302 and 18323 on the continental shelf of the southern South China Sea and reconstructs the coast-line changes on Sunda Shelf since the last 40000 years. In the period Marine Isotope 3,the old Sunda Shelf had low sea level,and it was partly exposed. Flourishing vegetations grew on the exposed old land. Mangroves developed along the coastline. On the Last Glacial Maximum,the sea level dropped greatly,coastline moved from inner shelf to outer shelf,the Old Sunda Land exposed further,and the lowering sea level induced the gradual disappearing of mangroves from the inner Sunda Shelf to the outer Sunda Shelf. And pioneer vegetation ferns covered the broadly exposed old land immediately. At the time of the last Deglaciation,sea level rose greatly,the coastline moved to the sea and the Sunda Shelf was drown again. Mangroves were emergent again from outer shelf to inner shelf and developed quickly. | WANG XiaoMei SUN XiangJun WANG PinXian Karl Stattegger | 2008 | Chinese Science Bulletin2008，53，13： | 2 |
| 5 | Spectrum: spectral analysis of unevenly spaced paleoclimAtic time series 显示文摘 | SCHULZ M STATTEGGER K | 1997 | Computers & Geosciences1997，23，9： | 1 |
| 6 | Major and trace element of stream sediments from the lowermost Amazon River 显示文摘 | Vital H Stattegger K | 2000 | Chemical Geology2000，168，： | 1 |
| 7 | Clay mineral sedimentation in high northern latitude deep-sea basins since the Middle Mio- cene (ODP Leg 151, NAAG) 显示文摘 | Winkler A Wolf-Welling T C W Stattegger K | 2002 | International Journal of Earth Sciences2002，91，： | 1 |
| 8 | Rapid flooding of the Sunda shelf: a late-glacial sea-level record显示文摘 | Hanebuth T Stattegger K Crootes M | 2000 | Science2000，288，： | 1 |
| 9 | Deglacial and Holocene evolution of the Vietnam shelf: stratigraphy, sediments and sea-level change显示文摘 | SCHIMANSKI A STATTEGGER K | 2005 | Marine Geology2005，214，： | 1 |
| 10 | Synchronous Tropical South China Sea SST Change and Greenland Warming During Deglaciation显示文摘 | Kienast M Steinke S Stattegger K | 2001 | Science2001，291，5511： | 1 |
| 11 | Synchronous tropical South China Sea SST change and Greenland warming during deglaciation显示文摘 | Kienast M Steinke S Stattegger K | 2001 | Science2001，291，： | 1 |
| 12 | Composition and trace-element geochemistry of detrital clay and heavy-mineral suites of the lowermost Amazon River: a provenance study 显示文摘 | Vital H Stattegger K Garbe-Schonberg C D | 1999 | Journal of Sedimentary Research1999，69，： | 1 |
| 13 | Clay mineral sedimentation in high northern latitude deep-sea basins since the Middle Miocene (ODP Leg 151, NAAG) 显示文摘 | Winkler A Wolf Welling T C W Stattegger K | 2002 | lntJEarth Sci2002，91，1： | 1 |
| 14 | Late Pleistocene forced regressive deposits on the Sunda Shelf (Southeast Asia)显示文摘 | Hanebuth T J J Stattegger K Schimanski A | 2003 | Marine Geology2003，199，： | 1 |
| 15 | Rapid flooding of the Sunda Shelf-a late glacial sea-level record显示文摘 | Hanebuth T Stattegger K Grootes P | 2000 | Science2000，288，： | 1 |
| 16 | Clay mineral sedimentation in high northern latitude deep sea basins since the middle Miocene (ODP Leg 151, NAAG)显示文摘 | Winkler A Wolf-Welling T C W Stattegger K | 2002 | International Journal of Earth Science2002，91，1： | 1 |
| 17 | Exploring the structure of the mid-Pleistocene revolution with advanced methods of time-series analysis显示文摘 | M. Mudelsee K. Stattegger | 1997 | Geologische Rundschau1997，，2： | 1 |
| 18 | Rapid flooding of the Sunda Shelf: a late-glacial sea-level record显示文摘 | HANEBUTH Till STATTEGGER Karl GROOTES Pieter | 2000 | Science2000，288，： | 1 |
| 19 | Composition and trace-element geochemistry of detrital clay and heavy-mineral suites of the lowermost Amazon River: A provenance study显示文摘 | Vital H Stattegger K Gar-Schoenberg C D | 1999 | J Sediment Res1999，69，3： | 1 |
| 20 | Depositional style and subsidence history of the Turpan Basin(NWChina)显示文摘 | Shao lei Stattegger Karl Li Wenhou | 1999 | Sedimentary Geology1999，128，12： | 1 |
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