The "Old Red Sand" is widely distributed along the coast of Fujian Province, China. Most studies have been carried out from as- pects of the origin, age and laterization of the "Old Red Sand", but this paper focus...The "Old Red Sand" is widely distributed along the coast of Fujian Province, China. Most studies have been carried out from as- pects of the origin, age and laterization of the "Old Red Sand", but this paper focused on reconstructing the history of the Asian Winter Monsoon change. On the basis of granulometric analysis of high-resohition samples, we have obtained environmental sen- sitive grain size component (ESGSC) from the Qingfeng (QF) profile by using the grain size-standard deviation method, which proves that the selected ESGSC is an important climate proxy. The mean grain size of this ESGSC could be used to reconstruct the East Asian Winter Monsoon (EAWM) intensity. As such, the history of the EAWM change since 44.0 ka reconstructed here reveals three main phases based on chronology dates of previous researches: (1) 44.0-25.5 ka B.P., the EAWM is relatively weak but increases gradually with fluctuations; (2) 25.5-15.5 ka B.P., relatively strong with high frequency fluctuations; (3) 15.5-7.1 ka B.P., with a weaker winter monsoon, but during 11-10 ka B.P. is remarkably enhanced. The EAWM recorded by mean grain size of the two neighboring sections have a better repeatability, so the millennial scales oscillation should be a reliable signal of the EAWM intensity. The climate recorded by ESGSC of the QF "Old Red Sand" compared to 6-80 of Huhi Cave stalagmites and Greenland GISP2 ice cores shows a good consistency, especially in detail, the YD event and four Heinrich events are all recorded, but the signal of D-O cycles was relatively weak.展开更多
The Old Red Sand is composed of brown-red, red, or orange-yellow semi-cemented and medium-fine sand sediment, mainly dis- tributed along the southeast coast of China. Based on previous studies, this paper summarizes t...The Old Red Sand is composed of brown-red, red, or orange-yellow semi-cemented and medium-fine sand sediment, mainly dis- tributed along the southeast coast of China. Based on previous studies, this paper summarizes the distribution and forms, sedi- mentary characteristics, formation mechanism, developing age, reddening process and the paleo-environment, suggesting that the Old Red Sand is mainly aeolian sediment of Late Pleistocene Age. The reddening process is mainly the result of decomposition and oxidation of iron-containing minerals caused by hot and humid tropical and sub-tropical climate. In this study, existing prob- lems are discussed and the prospect of further research is presented as well.展开更多
The "Old Red Sands" are widely distributed and typically developed over the coastal areas of Southeast Fujian, but there are different views on their origin. Based on the overall field investigations and a s...The "Old Red Sands" are widely distributed and typically developed over the coastal areas of Southeast Fujian, but there are different views on their origin. Based on the overall field investigations and a series of lab studies, the paper suggests that the "Old Red Sands" are mainly formed by the beach wind-drift sands and ,locally, by slope wash and alluviation.展开更多
The sedimentary strata and deposition ages of the 'old red sand' distributed along the coasts of south Fujian and west Guangdong are determined by lithostratigraphy, magnetic stratigraphy and earth chemistry c...The sedimentary strata and deposition ages of the 'old red sand' distributed along the coasts of south Fujian and west Guangdong are determined by lithostratigraphy, magnetic stratigraphy and earth chemistry combined with TL, ESR and 14C-dating techniques. The research shows that the 'old red sand' was aeolian sediments deposited from 55 400 to 9 000 aBP, the last glacial period in the middle and later age of Late Pleistocene. Most of them deposited in two periods of 56-42 ka and 30-10 ka. The 'old red sand' deposited in the period of 30-10 ka, the later Wurm glacier substage (Q33), developed on the largest scale with the widest distribution.展开更多
The formation and development environment of the "old red sands" on South China coasts is discussed according to the investigation in the field and laboratory works. The authors believed that the "old r...The formation and development environment of the "old red sands" on South China coasts is discussed according to the investigation in the field and laboratory works. The authors believed that the "old red sands" are the aeolian sediments deposits in the last glacial period of late Pleistocene when the sea level was lower than the present, and the laterization took place under the hot and wet climate during the later interglacial and postglacial periods when the sea level was relatively high.展开更多
A weathered deposit in South China is widespread on the coastal areas of Fujian and Guangdong provinces,China.This deposit consists of slightly cemented,medium-to fine-grained sands,and is characterized by its colors ...A weathered deposit in South China is widespread on the coastal areas of Fujian and Guangdong provinces,China.This deposit consists of slightly cemented,medium-to fine-grained sands,and is characterized by its colors of red,brown red,light reddish brown or dark yellowish orange,and is usually called "Old Red Sand".The uncertainty in its formation age has been a major obstacle to the study of this type of deposit.In this paper,optically stimulated luminescence(OSL) techniques were used to date the "Old Red Sand" sediments from Jinjiang,Fujian Province,China.The effect of the geochemical behavior of uranium and thorium in sediment during chemical weathering on estimation of annual dose was investigated.The results show that the change in annual dose due to weathering poses a major problem for the optical dating of such weathered sediments.The optical dating of these weathered deposits will produce erroneous ages if average annual dose during burial cannot be correctly estimated.For the profiles studied,the OSL dates obtained on samples from the upper part do not represent the burial age of the samples.It is highly likely that they are underestimated due mainly to the accumulated radioactive elements as a result of chemical weathering.It is concluded that changes in annual dose due to chemical weathering must be considered when dating similar sediments in South China.With a detailed analysis of the OSL dating results,the chronology of the marine terraces in this area was suggested.The lowest terrace was formed at ~3.5 ka and the second terrace was dated to ~74 ka.The age of the highest terrace may not be established accurately,but is inferred to be older than the apparent OSL date of~77 ka and so is the Paleolithic artifacts from it.展开更多
先前研究认为老红砂是末次冰期沿海风沙沉积,近期发现老红砂形成于末次间冰期。在福建平潭青峰典型老红砂分布区采集114个老红砂样品,130冬季风沙样品,60个夏季风沙样品做粒度测量和光释光测年。粒度测量显示冬季风沙粒度频率峰值出现在...先前研究认为老红砂是末次冰期沿海风沙沉积,近期发现老红砂形成于末次间冰期。在福建平潭青峰典型老红砂分布区采集114个老红砂样品,130冬季风沙样品,60个夏季风沙样品做粒度测量和光释光测年。粒度测量显示冬季风沙粒度频率峰值出现在400μm、夏季风沙280μm,老红砂粒度频率峰值出现在300μm与冬季风沙不同。夏季风沙和冬季风沙以7∶3混合可拟合老红砂粒度分布,表明青峰老红砂沉积期夏季风历时或强度远大于冬季风,对应于气候暖期,而不是末次冰期。老红砂剖面4个自然层光释光测年自下而上为122.5±6.7 ka B.P.、97.7±6.1 ka B.P.、83.1±4.2 ka B.P.、61.9±3.4 ka B.P.,对应末次间冰期,青峰老红砂是暖期气候的风沙响应。展开更多
基金supported by the National Natural Science Foundation of China(Grant No.41271031)the Open Foundation of State Key Laboratory of Loess and Quaternary Geology,Institute of Earth Environment,CAS(Grant No.SKLLQG1113)
文摘The "Old Red Sand" is widely distributed along the coast of Fujian Province, China. Most studies have been carried out from as- pects of the origin, age and laterization of the "Old Red Sand", but this paper focused on reconstructing the history of the Asian Winter Monsoon change. On the basis of granulometric analysis of high-resohition samples, we have obtained environmental sen- sitive grain size component (ESGSC) from the Qingfeng (QF) profile by using the grain size-standard deviation method, which proves that the selected ESGSC is an important climate proxy. The mean grain size of this ESGSC could be used to reconstruct the East Asian Winter Monsoon (EAWM) intensity. As such, the history of the EAWM change since 44.0 ka reconstructed here reveals three main phases based on chronology dates of previous researches: (1) 44.0-25.5 ka B.P., the EAWM is relatively weak but increases gradually with fluctuations; (2) 25.5-15.5 ka B.P., relatively strong with high frequency fluctuations; (3) 15.5-7.1 ka B.P., with a weaker winter monsoon, but during 11-10 ka B.P. is remarkably enhanced. The EAWM recorded by mean grain size of the two neighboring sections have a better repeatability, so the millennial scales oscillation should be a reliable signal of the EAWM intensity. The climate recorded by ESGSC of the QF "Old Red Sand" compared to 6-80 of Huhi Cave stalagmites and Greenland GISP2 ice cores shows a good consistency, especially in detail, the YD event and four Heinrich events are all recorded, but the signal of D-O cycles was relatively weak.
基金supported by National Natural Science Foundation of China (No. 40971007)
文摘The Old Red Sand is composed of brown-red, red, or orange-yellow semi-cemented and medium-fine sand sediment, mainly dis- tributed along the southeast coast of China. Based on previous studies, this paper summarizes the distribution and forms, sedi- mentary characteristics, formation mechanism, developing age, reddening process and the paleo-environment, suggesting that the Old Red Sand is mainly aeolian sediment of Late Pleistocene Age. The reddening process is mainly the result of decomposition and oxidation of iron-containing minerals caused by hot and humid tropical and sub-tropical climate. In this study, existing prob- lems are discussed and the prospect of further research is presented as well.
文摘The "Old Red Sands" are widely distributed and typically developed over the coastal areas of Southeast Fujian, but there are different views on their origin. Based on the overall field investigations and a series of lab studies, the paper suggests that the "Old Red Sands" are mainly formed by the beach wind-drift sands and ,locally, by slope wash and alluviation.
文摘The sedimentary strata and deposition ages of the 'old red sand' distributed along the coasts of south Fujian and west Guangdong are determined by lithostratigraphy, magnetic stratigraphy and earth chemistry combined with TL, ESR and 14C-dating techniques. The research shows that the 'old red sand' was aeolian sediments deposited from 55 400 to 9 000 aBP, the last glacial period in the middle and later age of Late Pleistocene. Most of them deposited in two periods of 56-42 ka and 30-10 ka. The 'old red sand' deposited in the period of 30-10 ka, the later Wurm glacier substage (Q33), developed on the largest scale with the widest distribution.
文摘The formation and development environment of the "old red sands" on South China coasts is discussed according to the investigation in the field and laboratory works. The authors believed that the "old red sands" are the aeolian sediments deposits in the last glacial period of late Pleistocene when the sea level was lower than the present, and the laterization took place under the hot and wet climate during the later interglacial and postglacial periods when the sea level was relatively high.
基金Supported by the National Natural Science Foundation of China (Grant Nos. 40471010 and 49925307)
文摘A weathered deposit in South China is widespread on the coastal areas of Fujian and Guangdong provinces,China.This deposit consists of slightly cemented,medium-to fine-grained sands,and is characterized by its colors of red,brown red,light reddish brown or dark yellowish orange,and is usually called "Old Red Sand".The uncertainty in its formation age has been a major obstacle to the study of this type of deposit.In this paper,optically stimulated luminescence(OSL) techniques were used to date the "Old Red Sand" sediments from Jinjiang,Fujian Province,China.The effect of the geochemical behavior of uranium and thorium in sediment during chemical weathering on estimation of annual dose was investigated.The results show that the change in annual dose due to weathering poses a major problem for the optical dating of such weathered sediments.The optical dating of these weathered deposits will produce erroneous ages if average annual dose during burial cannot be correctly estimated.For the profiles studied,the OSL dates obtained on samples from the upper part do not represent the burial age of the samples.It is highly likely that they are underestimated due mainly to the accumulated radioactive elements as a result of chemical weathering.It is concluded that changes in annual dose due to chemical weathering must be considered when dating similar sediments in South China.With a detailed analysis of the OSL dating results,the chronology of the marine terraces in this area was suggested.The lowest terrace was formed at ~3.5 ka and the second terrace was dated to ~74 ka.The age of the highest terrace may not be established accurately,but is inferred to be older than the apparent OSL date of~77 ka and so is the Paleolithic artifacts from it.
文摘先前研究认为老红砂是末次冰期沿海风沙沉积,近期发现老红砂形成于末次间冰期。在福建平潭青峰典型老红砂分布区采集114个老红砂样品,130冬季风沙样品,60个夏季风沙样品做粒度测量和光释光测年。粒度测量显示冬季风沙粒度频率峰值出现在400μm、夏季风沙280μm,老红砂粒度频率峰值出现在300μm与冬季风沙不同。夏季风沙和冬季风沙以7∶3混合可拟合老红砂粒度分布,表明青峰老红砂沉积期夏季风历时或强度远大于冬季风,对应于气候暖期,而不是末次冰期。老红砂剖面4个自然层光释光测年自下而上为122.5±6.7 ka B.P.、97.7±6.1 ka B.P.、83.1±4.2 ka B.P.、61.9±3.4 ka B.P.,对应末次间冰期,青峰老红砂是暖期气候的风沙响应。