共查询到20条相似文献，搜索用时 31 毫秒
1.
Redfield AC 《Science (New York, N.Y.)》1967,157(3789):687-692
Radioactive carbon determinations of the age of peat indicate that at Bermuda, southern Florida, North Carolina, and Louisiana the relative sea level has risen at approximately the same rate, 2.5 x 10(-3) foot per year (0.76 x 10(-3) meter per year), during the past 4000 years. It is proposed tentatively that this is the rate of eustatic change in sea level. The rise in sea level along the northeastern coast of the United States has been at a rate much greater than this, indicating local subsidence of the land. Between Cape Cod and northern Virginia, coastal subsidence of 13 feet appears to have occurred between 4000 and 2000 years ago and has continued at a rate of about 1 x 10(-3) foot per year since then. On the northeastern coast of Massachusetts, subsidence of 6 feet occurred between 4000 and 3000 years ago; since then sea level has risen at about the eustatic rate. Between 12,000 and 4000 years ago, sea level rose at an average of about 11 x 10(-3) foot per year. The part played by local subsidence or temporary departures from the average rate during this period is uncertain. 相似文献
2.
Randall JE 《Science (New York, N.Y.)》1973,181(4095):169-170
The maximum length of 36.5 feet (11.1 meters) attributed to the white shark (Carcharodon carcharias) by Günther and others is a mistake. Examination of the jaws and teeth of the specimen referred to by Günther and comparison with the jaws of white sharks of known length revealed a length of about 17 feet ( approximately 5 meters). The largest white shark reliably measured was a 21-foot (6.4-meter) individual from Cuba. Bites on whale carcasses found off southern Australia suggest that white sharks as long as 25 or 26 feet (7 (1/2) or 8 meters) exist today. The size of extinct Carcharodon has also been grossly exaggerated. Based on a projection of a curve of tooth size of Recent Carcharodon carcharias, the largest fossil Carcharodon were about 43 feet ( approximately 13 meters) long. 相似文献
3.
不同留叶数对优化烤烟等级结构的影响 总被引：5，自引：2，他引：3
通过烤烟采烤前去除部分顶叶、脚叶,对比研究其对优化烤烟等级结构的影响,结果表明:顶叶、脚叶各去除1~3片处理,烟株长势与烤后的烟叶差别不明显,易烘烤,产量也较接近,但顶叶、脚叶各去除1片比顶叶、脚叶各去除4~5片处理叶片稍薄;顶叶、脚叶各去除4~5片处理,叶片比较厚,但产量较低。顶叶、脚叶各去除4片处理,除第1烤田间成熟能够达到成熟的要求,第2烤开始,每烤推迟4~5 d才能呈现成熟的特征,烤后的烟叶有部分叶脉带青,颜色也比较暗;顶叶、脚叶各去除5片处理的烟株,无法达到成熟的要求,烤后的烟叶比较多青筋、青片现象,甚至烤黑,油分也比较少。因此,根据武平县的生态气候条件,正常栽培的烟叶留叶数应在18片左右为宜。 相似文献
4.
Faunal and lithologic evidence is used to reconstruct paleoceanographic events over the last 4.5 million years. The inception of perennial sea-ice cover is dated at about 0.7 million years. 相似文献
5.
大连市雷暴气候统计特征及趋势分析 总被引：2，自引：2，他引：0
利用大连国家基准气候观测站1951—2010年的逐日雷暴资料,通过气候倾向率、经验频率法等分析方法,揭示大连市雷暴气候变化特征。结果表明,大连市年雷暴日数总体呈逐年增加趋势,近60年来增加了约3 d;夏季雷暴出现最多,其次为秋季,冬季发生概率很小;雷暴初日呈下降趋势,气候倾向率为-3.482 d/10年,60年来提前了近21 d;雷暴终日呈上升趋势,气候倾向率为3.55 d/10年,60年来推迟了近22 d。4月雷暴初日发生的保证率迅速上升,雷暴终日在10月下旬至11月上旬上升较快,雷暴初、终日之间持续时间总体上呈增加趋势,气候倾向率为7.032 d/10年,近60年来延长了约42 d。 相似文献
6.
Early local last glacial maximum in the tropical Andes 总被引：1，自引：0，他引：1
The local last glacial maximum in the tropical Andes was earlier and less extensive than previously thought, based on 106 cosmogenic ages (from beryllium-10 dating) from moraines in Peru and Bolivia. Glaciers reached their greatest extent in the last glacial cycle approximately 34,000 years before the present and were retreating by approximately 21,000 years before the present, implying that tropical controls on ice volumes were asynchronous with those in the Northern Hemisphere. Our estimates of snowline depression reflect about half the temperature change indicated by previous widely cited figures, which helps resolve the discrepancy between estimates of terrestrial and marine temperature depression during the last glacial cycle. 相似文献
7.
Recent paleomagnetic-radiometric data from six rhyolite domes in the Valles Caldera, New Mexico, indicate that the last change in polarity of the earth's magnetic field from reversed to normal (the Brunhes-Matuyama boundary) occurred at about 0.7 million years ago. A previously undiscovered geomagnetic polarity event, herein named the "Jaramillo normal event," occurred about 0.9 million years ago. 相似文献
8.
Phillips JD 《Science (New York, N.Y.)》1967,157(3791):920-923
Ten magnetic profiles across the mid-Atlantic ridge near 27 degrees N show trends that are parallel to the ridge axis and symmetrical about the ridge axis. The configuration of magnetic bodies that could account for the pattern supports the Vine and Matthews hypothesis for the origin of magnetic anomalies over oceanic ridges. A polarity-reversal time scale inferred from models for sea-floor spreading in the Pacific-Antarctic ridge and radiometrically dated reversals of the geomagnetic field indicates a spreading rate of 1.25 centimeters per year during the last 6 million years and a rate of 1.65 centimeters per year between 6 and 10 million years ago. A similar analysis of more limited data over the mid-Atlantic ridge near 22 degrees N also indicates a change in the spreading rate. Here a rate of 1.4 centimeters per year appears to have been in effect during the last 5 million years; between 5 and 9 million years ago, an increased rate of 1.7 centimeters per year is indicated. The time of occurrence and relative magnitude of these changes in the spreading rate, about 5 to 6 million years ago and 18 to 27 percent, respectively, accords with the spreading rate change implied for the Juan de Fuca ridge in the northeast Pacific. 相似文献
9.
Lunar spherules are small glass beads that are formed mainly as a result of small impacts on the lunar surface; the ages of these impacts can be determined by the (40)Ar/(39)Ar isochron technique. Here, 155 spherules separated from 1 gram of Apollo 14 soil were analyzed using this technique. The data show that over the last approximately 3.5 billion years, the cratering rate decreased by a factor of 2 to 3 to a low about 500 to 600 million years ago, then increased by a factor of 3.7 +/- 1.2 in the last 400 million years. This latter period coincided with rapid biotic evolutionary radiation on Earth. 相似文献
10.
Varved sediments from a lake near the present forest-prairie border in northwestern Minnesota provide an annual record of climate change for the last 10,400 years. Climate-sensitive mineral, chemical, and biological components show that the mid-Holocene dry interval between 8500 and 4000 years ago is asymmetrical and actually consists of two distinct drier pulses separated by a moister interval that lasted about 600 years. Cyclic fluctuations with periods of several hundred years were abrupt and persistent throughout the Holocene and are most clearly recorded within the two drier pulses. 相似文献
11.
Four magnetic profiles across the Pacific-Antarctic Ridge reveal magnetic anomalies that show trends parallel with the ridge axis and symmetry about the ridge axis. The distribution of bodies that could cause these anomalies supports the Vine and Matthews hypothesis for the generation of patterns of magnetic anomalies associated with the midocean ridge system. The geometry of the bodies accords with the known reversals of the geomagnetic field during the last 3.4 million years, indicating a spreading rate of the ocean floor of 4.5 centimeters per year. If one assume that the spreading rate within 500 kilometers of the ridge axis has been constant, reversals of the geomagnetic field during the last 10.0 million years can be determined. This new, detailed history of field reversals accords with observed anomalies over Reykjanes Ridge in the North Atlantic if a spreading rate of 1 centimeter per year is assumed there. 相似文献
12.
Climate and groundwater recharge during the last glaciation in an ice-covered region 总被引：1，自引：0，他引：1
U Beyerle R Purtschert W Aeschbach-Hertig DM Imboden HH Loosli R Wieler R Kipfer 《Science (New York, N.Y.)》1998,282(5389):731-734
A multitracer study of a small aquifer in northern Switzerland indicates that the atmosphere in central Europe cooled by at least 5 degreesC during the last glacial period. The relation between oxygen isotope ratios (delta18O) and recharge temperatures reconstructed for this period is similar to the present-day one if a shift in the delta18O value of the oceans during the ice age is taken into account. This similarity suggests that the present-day delta18O-temperature relation can be used to reconstruct paleoclimate conditions in northern Switzerland. A gap in calculated groundwater age between about 17,000 and 25,000 years before the present indicates that during the last glacial maximum, local groundwater recharge was prevented by overlying glaciers. 相似文献
13.
Paleoatmospheric signatures in neogene fossil leaves 总被引：1，自引：0，他引：1
Van Der Burgh J Visscher H Dilcher DL Kürschner WM 《Science (New York, N.Y.)》1993,260(5115):1788-1790
An increase in the atmospheric carbon dioxide (CO(2)) concentration results in a decrease in the number of leaf stomata. This relation is known both from historical observations of vegetation over the past 200 years and from experimental manipulations of microenvironments. Evidence from stomatal frequencies of fossil Quercus petraea leaves indicates that this relation can be applied as a bioindicator for changes in paleoatmospheric CO(2) concentrations during the last 10 million years. The data suggest that late Neogene CO(2) concentrations fluctuated between about 280 and 370 parts per million by volume. 相似文献
14.
15.
40年来我国粮食产量历史演变特征的初步分析 总被引：1，自引：0，他引：1
分析探讨40年来我国粮食生产的波动特征。对粮食产量的预测预报以及逐年稳定增长具有重要的现实意义。全国和部分省（区）单产序列的分析表明：
1. 近40年来,我国粮食单产的增产年多于减产年,增产持续时间和增产幅度亦均大于减产年;
2. 各省（区）的增减产年频数呈准正态分布,其累积频率曲线可分为稳定、不稳定和中间型三类;
3. 增向转移概率大于减向转移概率,尤以减转增的概率为最大,减转减最小;
4. 40年来我国粮食生产的发展经历了低产缓慢发展—波动发展—高速增长不稳定发展的3个阶段;
5. 增减产年的历史演变具有较明显的准4年及其倍数周期的波动特征,各地主要波动周期的变化说明了粮食生产稳定性在地区上的差异。 相似文献
16.
The evolution of climate over the last millennium 总被引：9，自引：0，他引：9
Knowledge of past climate variability is crucial for understanding and modeling current and future climate trends. This article reviews present knowledge of changes in temperatures and two major circulation features-El Ni?o-Southern Oscillation (ENSO) and the North Atlantic Oscillation (NAO)-over much of the last 1000 years, mainly on the basis of high-resolution paleoclimate records. Average temperatures during the last three decades were likely the warmest of the last millennium, about 0.2 degrees C warmer than during warm periods in the 11th and 12th centuries. The 20th century experienced the strongest warming trend of the millennium (about 0.6 degrees C per century). Some recent changes in ENSO may have been unique since 1800, whereas the recent trend to more positive NAO values may have occurred several times since 1500. Uncertainties will only be reduced through more extensive spatial sampling of diverse proxy climatic records. 相似文献
17.
Information on responses of higher organisms to climate change is dominated by events in spring. Far less is known about autumnal events and virtually nothing about communities of microorganisms. We analyzed autumnal fruiting patterns of macrofungi over the past 56 years and found that average first fruiting date of 315 species is earlier, while last fruiting date is later. Fruiting of mycorrhizal species that associate with both deciduous and coniferous trees is delayed in deciduous, but not in coniferous, forests. Many species are now fruiting twice a year, indicating increased mycelial activity and possibly greater decay rates in ecosystems. 相似文献
18.
目前,呼和浩特作为首府城市经济发展迅速,房地产业更是以前所未有的速度和规模向前发展。本文作者以近几年呼和浩特市城区房地产市场价格资料为依据,分析了目前呼和浩特市城区住宅房地产价格结构,并探讨目前呼和浩特市城区近两年住宅房地产市场价格上涨原因。 相似文献
19.
20.
Stein R Nam SI Schubert C Vogt C Futterer D Heinemeier J 《Science (New York, N.Y.)》1994,264(5159):692-696
Oxygen isotope records of cores from the central Arctic Ocean yield evidence for a major influx of meltwater at the beginning of the last deglaciation 15.7 thousand years ago (16,650 calendar years B.C.). The almost parallel trends of the isotope records from the Arctic Ocean, the Fram Strait, and the east Greenland continental margin suggest contemporaneous variations of the Eurasian Arctic and Greenland (Laurentide) ice sheets or increased export of low-saline waters from the Arctic within the East Greenland Current during the last deglaciation. On the basis of isotope and carbon data, the modern surface- and deep-water characteristics and seasonally open-ice conditions with increased surface-water productivity were established in the central Arctic at the end of Termination lb about 7.2 thousand years ago or 6,000 calendar years B.C.). 相似文献