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1.
The 4.45 m-thick pure ice lens have been discovered firstly at depth from 19.81 -24.26 m in the bore No.6, which locates in north bank of the Ngoring Lake. In source region of the Huanghe (Yellow) River, 14C dating, X -ray diffraction, pollen analysis, micropalaeontology, chemical components, environmental isotope 2H, 3H, 18O and freezing point of the ice and water samples from the bore have been tested and microorganism in the ice have been also appraised with microscope. Combined with the research on geomorphy and Quaternary around the lake, the ice lens are determined as a kind of deep-buried lake ice, formed in 35,030-45,209 yr.B.P., and annual mean air temperature was about -10℃ during that time. 相似文献
2.
Based on the new data of the Quaternary along the coast of Hainan Island, China, this paper puts forward that the Holocene in Hainan Island can be divided into four formations: Wanning formation (Q41), Sanya formation (Q42-1), Qiongshan formation (Q42-2) and Ledong formation (Q43). Spore-pollen analysis shows that there are 6 spore-pollen zones existed, reflecting two cycles of climatic fluctuation from warm-dry to hot-humid. The climax of hot-humid period occurred 6,000-5,000 years B.P.. Based on the 14C dating data of the 38 samples representing the positions of ancient sea level, a breakthrough curve representing the sea level change during the Holocone is obtained, in which , a sea level change caused by tectonic movement is subtracted. Two cycles of rise-drop of sea level with three periods of high sea level were found. The period with the highest sea level is some 6,000-5,000 years B.P.. According to the rise-drop rate of sea level, four periods of the sea level change can be distinguished in the 相似文献
3.
Trare amounts of benzene hydrocarbons obtained in Jiaozhou Bay (Qindao) were enriched bysorption on a GDX-102 column and eluted by carbon disulfide. The eluted was concenttaled and then de-temened by capillary column gas cbornatognphy.The contents of virious kinds of benzene hydrocarbons in Jiaozhou Bay coastal water were benzene(22.3-141.6)× 10～(-9)g/L, toluate (15.2-94.0) × 10~(-9) g/L, ethyl benzene(11.8-85.1)×10~(-9) g/L, p -xylene(15.2-78.5) ×10(-9) g/L, m-xylene (10.9-79.4) ×10(-9) g/L, o -xylene (12.4-80.1) x ×10(-9)g/L; iso-propyl(8.4- 73.1) x ×10(-9)g/L, n -propyl (6.9-76.4) ×10(-9) g/L, 1, 3, 5-trimethylbenzene (10.9- 35.9)×10(-9) g/L, 1,2, 4-trimethybenzene (10.0- 38.0)×10(-9) g/L, n - butydriare (8. 1 - 34.6) ×10(-9)g/L. The recovery of benzenehydrocarbons was (85.1 -95.6)%. 相似文献
4.
An 82 cm core was collected from Qinghai Lake in the Qinghai-Xizang Plateau, China and sectioned in intervals of 1 cm for
analysis of pigments (i. e. chlorophyll derivatives, carotenoids, myxoxanthophyll, oscillaxanthin) and210Pb.210Pb dating was used to establish the chronological sequence. The concentrations of myxoxanthophyll and oscillaxanthin from
the cyanophytes increase with temperature. There are four peak values at 0–14 cm (present−1891a), 25 cm (1786a), 45 cm (1581a),
60 cm (1416a) representing four warm and low water level periods during the past 700 years. This was confirmed by the high
concentration of carbonate and ∂13C in these stages. In these 700 years, there were also 4 periods of cold wet climate and high water level as indicated by
the tree ring index and high value of native chlorophyll and high, variable CD/TC ratios.
The project was supported by the Loess and Quaternary Research Lab, Academia Sinica. 相似文献
5.
Jinglu Wu 《中国地理科学(英文版)》1997,7(3):229-235
The hole RM, the deepest one fully obtained core in the Qinghai-Xizang Plateau, situated in the depositional center of the
Zoige Basin (33°57′N; 102° 21′E) in the northeastern Qinghai-Xizang Plateau with a depth of 310.46 m. From 14C dating and paleomagnetic stratigraphic study, the core RM can date back to 900 ka B.P.. In this paper we analyzed the compositions
of δ18O and δ13C in various carbonates can date (snail, obstrode, chemical carbonate) in core RM and discussed preferably the paleoclimatic
record by the proxies of δ18O and δ13C of chemical carbonate (authicarbonate) from core RM in the past 140 ka. The results showed that the values of δ18O in various carbonates are generally identical, and the values of δ13C in it are inconsistent, while there exist better relativity. The studies also demonstrated that there was a negative correlation
between δ18O and δ13C of authicarbonate in core RM in the past 140 ka, showing that the changes of δ18O values were mainly relative to the water temperature. According to above, the climatic evolutionary sequence were rebuilt
in the past 140 ka in the region. 相似文献
6.
A great quartity of cosmic dust(spherules) was found in deep-sea sediments during May to July,1983manganese nodule investigations by the R/V“XIANGYANGHONG 16”in the area 7°-11°N,167°-178°Win the Pacific.Comprehensive study of the cosmic dust and determination with Laser Raman MolecularMicroprobe(LRMM) of the molecules in it showed that besides Fe-Fe,Fe~(3+)-O,Fe-Ni,Al-O,Fe-Obr-Si and Si-Onb,it also contained the organic molecules C-H-O and C-H-S-O,various no fixed form molecules of C,CH_2,CH_3 and volatile molecules CO_2,H_2O,OH~- and H_2S,etc…The study result has very important applications for exploring the origin of interplanetary dust parti-cles and life material. 相似文献
7.
On the origin of rice agriculture in southern China and its propagation in East Asia 总被引：1，自引：0，他引：1
Zhenguo Huang 《中国地理科学(英文版)》1994,4(4):289-294
Based on the archaeological rice cultivation with the14C dating of about 4000–5000 a B.P. the author holds that the plain at the lower reaches of the Changjiang (Yangtze) River
is one origin of rice cultivation in Asia and the other is Allahabad of India. The propagation of ancient rice cultivation
in China can be divided into three stages, namely 4000–3000, 2635–2420 and about 1000 a B.P. It is inferred that there were
two ways for propagating rice cultivation from China to Japan. One was from lower reaches of Changjiang River to Kyushu by
sea way and the other was from Shandong Peninsula to southern Korea and then to Kyushu. The age of propagating rice cultivation
into Vietnam from South China is about 1000 a B.P. Being influenced by climatic changes since about 5000 a B.P. the propagation
of rice cultivation was stagnated for two times at least, for example, the three warm climatic stages and the two cold stages
were quite in correspondence with the propagation and stagnation stages of rice cultivation, respectively, in China. During
the ancient times the development of paddy rice was directive related to the fluctuation of sea level which is in keeping
with the climatic changes. 相似文献
8.
Chen Zhiming 《中国海洋湖沼学报》1987,5(3):251-262
The author made an approximate dating of the highest shorelines of the three larger interior lakes and proved that during
late Q3 or early Q4, there existed a higher lake level in the plateau, reflecting that the climate then was much more moist than it is today.
It could be presumed from a study of these two ages that such higher lake levels correspond with both the last glacial epoch
(i. e., the latter half) and the lowest sea level of the East China Sea then.
Moreover, interpretations of aerial photos and an on-the-spot survey revealed that since then these lakes had 8–10 rhythms
of retreat, indicating that the climate in central Asia and the plateau at that time had 8–10 comparatively arid periods.
As the plateau is still in the faster process of upheaval, it is expected that on a longterm basis, the climate in this region
will tend to be continuously dry. However, should there be a neo-glacial epoch in the world, and if the higher lake level
really corresponds to the glacial epoch, then in the not distant future, the lake level will possibly rise again to some extent.
Thanks are due to the No. 2 Institute of Oceanography of SOA for its analyses of C14 dating specimens.
This paper was published in Chinese inOceanologia et Limnologia Sinica
17(3): 207–216, 1986. 相似文献
9.
ESR dating of aragonitic and calcitic corals , eolianite , calcrete , and corallineae from coral reefs in the South China Sea was applied to study of Quaternary reef geology . The ESR ages of calcitic corals correlated with the biostratigraphy , lithostratigraphy and geochemistry of Well Xi-Chen-1 and the oxygen-isotope stratigraphy of deep sea sediments, were reliable and up to 1.26 Ma. The selection of signals for dating and other related problems are discussed . 相似文献
10.
1 INTRODUCTIONA large-scale volcanic eruption can injectenormous amount of ash and dust into the atmos-phere, leading to local and short cooling due toshielding incoming radiation. During the past 2 to 3decades, accumulated evidence indicated thatlarge-scale volcano eruptions or series of volcanicactivity appears to coincide with climatologicaltransitions. For example, Robock (1979) indicatedthat volcanic eruptions played a role in forcing "Lit-tle Ice Age". Well-dated high-resolution co… 相似文献
11.
MEN Wu ) WEI Hao ) and LIU Guangshan ) * ) College of Oceanography Environmental Science Xiamen University State Key Laboratory of Marine Environmental Science 《中国海洋大学学报(英文版)》2006,5(3):228-234
1Introduction Therearefourradiumisotopesinnature,ofwhich224Ra,226Raand228Rahavebeenwidelyinvestigated inmarineresearch,butthespecificactivityof223Rais toolowtobemeasured,therefore,itsapplicationsarelimited(Moore,1969;Broeckeretal.,1976;KuandLin,1976;Nozak… 相似文献
12.
Cold event at 5 500 a BP recorded in mud sediments on the inner shelf of the East China Sea 总被引：2，自引：0，他引：2
A 700-year record (1.0–1.5 a resolution) of the East Asian winter monsoon (EAWM), based on grain-size analysis and AMS14C dating of Core EC2005 from the inner-shelf mud wedge of the East China Sea (ECS), was compared with the Dongge stalagmite
δ18O record during the mid-Holocene. The upper muddy section of Core EC2005 has been formed mainly by suspended sediments derived
from the Changjiang (Yangtze) River mouth since 7.3 ka BP. High precipitation and a strengthened EAWM might have played key
roles in the high sedimentation rate (1 324–1 986 cm/ka) between 5.9–5.2 ka BP. The EAWM strengthened when the Asian summer
monsoon weakened, especially around 5 500 a BP, which corresponded to a worldwide cold event. The EAWM during the mid-Holocene
shows statistically significant solar periodicities at 62 and 11 a. The 5 500 a BP cold event might be resulted from orbital
forcing and changes in solar activity. 相似文献
13.
Effects of Fe and Mn on the growth of a red tide dinoflagellateScrippsiella trochoidea (Stein) Loeblch III 总被引：1，自引：0，他引：1
Batch culture experiments were conducted with a red tide dinoflagellateScrippsiella trochoidea (Stein) Loeblch III collected from Jiaozhou Bay, Shangdong, China. Growth rates and oellular Chl—a were measured in media
with iron and manganese ion concentrations controlled at different levels using EdTA-trace metal buffer systems. Cell density
increased 3.2 times to 6.5 times over the range of lowest (0 mol/L) to highest (10−5 mol/L) iron and manganese ion concentrations. The range of cell density response was much lower than the range of total available
iron and manganese, which was >100—fold that of Fe. This nonlinear relationship indicates that the cells adapt to make more
efficient use of iron and manganese under limiting conditions. The cellular Chl—a content maximized after 3 days incubation
and then decreased gradually under either iron or manganese limitation conditions. It indicated that the algae gained higher
photosynthesis ability when transferred to a new environment. Growth responses to iron and manganese limitation can be both
modeled according to the equation of Monod. The half—saturation constant for growth,k, is 4.6×10−8 mol/L for Fe and 5.1×10−8 mol/L for Mn. Our results showed that the iron availability in Jiaozhou Bay does not limit the growth ofS. trochoidea.
Contribution No. 2831 from the Institute of Oceanology, Chinese Academy of Sciences.
Project 9389008 supported by NSFC; Study supported by PDB6. 相似文献
14.
施雅风 《中国地理科学(英文版)》1994,4(2):186-192
ＰＲＯＦＥＳＳＯＲ ＺＨＵ ＫＥＺＨＥＮ ＯＰＥＮＩＮＧ ＵＰ Ａ ＰＡＴＨ ＦＯＲ ＲＥＳＥＡＲＣＨ ＯＮ ＣＬＩＭＡＴＩＣ ＣＨＡＮＧＥ ＩＮ ＣＨＩＮＡ ＳｈｉＹａｆｅｎｇ（施雅风）（ＬａｎｚｈｏｕＩｎｓｔｉｔｕｔｅｏｆＧｌａｃｉｏｌｏｇｙａｎ... 相似文献
15.
Ｉｔｉｓｏｎｅｏｆｔｈｅｆｒｏｎｔｉｅｒｆｏｃｕｓｅｓｉｎｔｈｅｆｉｅｌｄｏｆｇｌｏｂｌｅｅｎｖｉｒｏｎｍｅｎｔａｌｃｈａｎｇｅｓｔｏｅｘｔｒａｃｔｑｕａｎｔｉｔａｔｉｖｅｌｙｐａｓｔｃｌｉｍａｔｉｃｓｉｇｎａｌｓｆｒｏｍｌａｋｅｓｅｄｉｍｅｎｔｒｅｃｏｒｄｓ．Ｉｎｔｈｅｒｅ-ｃｅｎｔｄｅｃａｄｃｉｏｕｓｙｅａｒｓａｓｅｒｉｅｓｏｆａｃｈｉｅｖｅｍｅｎｔｓｏｎｒｅ-ｂｕｉｌｄｉｎｇｔｈｅｓｅｑｕｅｎｃｅｓｏｆｃｌｉｍａｔｉｃａｎｄｅｎｖｉｒｏｎｍｅｎｔａｌｅｖｏｌｕｔｉｏｎｓａｔｖａｒｉｏｕｓｓ… 相似文献
16.
A new kinetic spectrophotometric method is developed for the measurement of manganese (II) in water. The method is based on
the catalytic effect of manganese (II) with the oxidation of weak acid brilliant blue dye (RAWL) by KIO4 using the Nitrilo triacetic acid (NTA) as an activation reagent. The optimum conditions obtained are 40 mgL−1 RAWL, 1×10−4molL−1 KIO4, 2×10−4 molL−1 Nitrilo triacetic acid (NTA), pH = 5.8, the reaction time of 3.00 min and the temperature of 20.0 °C. Under the optimum conditions,
the proposed method allows the measurement of manganese (II) in a range of 0–50.0 ng mL−1 and with a detection limit of down to 0.158 ng mL−1. The recovery efficiency in measuring the standard manganese (II) solution is in a range of 98.5%–102%, and the RSD is in
a range of 0.76%–1.25%. The new method has been successfully applied to the measurement of manganese (II) in both fresh water
and seawater samples with satisfying results. Moreover, few cations and anions interfere with the measurement of manganese
(II). Compared with other kinetic catalytic methods and instrumental methods, the proposed method shows fairly good selectivity
and sensitivity, low cost, cheapness, low detection limit and rapidity. It can be applied on boats easily. 相似文献
17.
The Huanghe (Yellow) River, with annual sediment discharge about 11 ×108tons, contributes about 17% of the fluvial sediment discharge of world's 21 major rivers to the ocean because its middle reaches flow across the great Loess Plateau of China. Sediment discharge of the Huanghe River has a widespread and profound effect on sedimentation of the sea. The remarkable shift of its outlet in 1128-1855 A.D. to the South Yellow Sea formed a large subaqueous delta and provided the substrate for an extensive submarine ridge field.The shift of its outlet in the modern delta every 10 years is the main reason why with an extremely heavy sediment input and a micro- tidal environment, the Huanghe River has not succeeded in building a birdfoot delta like the Mississippi. The Huanghe River has consistently brought heavy sediment input to sea at least since 0.7 myr.B.P. Paleochannels, paleosols, cheniers and fossils on the sea bottom indicate that the Yellow Sea was exposed during the late Quaternary glacial low-sea l 相似文献
18.
A new kinetic spectrophotometric method has been developed for the determination of iron (Ⅲ). The method is based on the catalytic effect of iron (Ⅲ) on the oxidation of weak acid brilliant blue dye (RAWL) by KIO4 in acid medium. The advantages of the proposed method are that it is sensitive, accurate, rapid, inexpensive, can be operated under room temperature and has a large determination concentration range compared to other techniques. The obtained optimum conditions are pH 3.15, RAWL (200 mgL-1) 5.00mL, Potassium periodate solution (0.01 molL-1) 0.30mL, phenanthroline (0.02molL-1) 1.00mL, reaction temperature 25℃ and reaction time 7 miu. With this method iron could quantitively be determined in the range 0.00-0.02 mgL-1, the detection limit being 4.10×10-10mL-1. The relative standard deviations (RSD) in five replicate determinations for 3 μgL-1 and 5μgL-1 iron (Ⅲ) are 3.1% and 1.9%, respectively. The method has been applied to the determination of iron (Ⅲ) in tap water samples and seawater samples (from the South China Sea), the recovery rates being 98.0% and 100.5%, respectively. 相似文献
19.
STUDY OF OKINAWA TROUGH SEDIMENTATION RATES AND PALEOENVIRONMENT BASED ON URANIUM SERIES ISOTOPE 总被引：1，自引：0，他引：1
Spectrometry of ~(238)U, ~(234)U, ~(230)Th and, ~(232)Th in three Okinawa Trough cores showed that, based on the~(230)Th/~(232)Th activity ratio, the sedimentation rates were about 2.5 cm/ka, 2.8 cm/ka and 8.5 cm/ka respectivelyduring the Holocene and about 20.1 cm/ka, 12.29 cm/ka, 8.8 cm/ka and 12.6 cm/ka respectively during theWurm glacial. To examine the past global climatic and oceanographic changes, the stable oxygen isotopesδ~(18)O and CaCO_3 were measured. The Th content and Th/U ratio showed that variations of terrigenous materialinput from the continental shelf were associated with glacial and interglacial changes and sea level 相似文献
20.
ＲＥＬＡＴＩＯＮＳＨＩＰＢＥＴＷＥＥＮＱＩＮＧＨＡＩＬＡＫＥＬＥＶＥＬＤＥＳＣＥＮＤＩＮＧＡＮＤＡＲＴＩＦＩＣＩＡＬＷＡＴＥＲ－ＣＯＮＳＵＭＰＴＩＯＮ￥ＰｅｎｇＭｉｎ（彭敏）ＣｈｅｎＧｕｉｃｈｅｎ（陈桂琛）ＺｈｏｕＬｉｈｕａ（周立华）（Ｎｏｒｔｈｗｅ... 相似文献