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991.
992.
Based on the published data of structure geology,geochronology,petrology and isotope geochemistry,the authors of this paper have conducted studies on the tectonic evolution history of Japan arc system and Kyushu-Palau ridge(KPR) . The studies show that the initial Japan arc system was resulted from the subduction of ancient Pacific plate beneath Eurasian Plate in Permian. It was part of an Andean-type continental volcanic arc which occurred in the offshore in the east of Asian during late Mesozoic era. The formation of tertiary back-arc basin(Japan Sea) resulted in the fundamental tectonic framework of the present arc system. Since Quaternary the system has been lying at E-W compression tectonic setting due to the eastward subduction of Amur Plate. It is expected that Japan arc system will be juxtaposed with Asian continent,which is similar to the present Taiwan arc system. The origin of Philippine Sea Plate(PSP) is still in debate. Some studies argued that it is a trapped oceanic crust segment,while the others insisted that it is a back-arc basin accompanied with ancient IBM arc. However,it is all agreed that the tectonic evolution of PSP started since 50 Ma,i.e.,PSP has drifted from the site around equator at 50 Ma to the present site,and the subduction of PSP along Nankai trough-Ryukyu Trench beneath the Japan arc system during 6-2 Ma led to the formation of the present Ryukyu arc system. Of the PSP,the KPR has been found with the oldest rocks formed at 38 Ma. Combining with its geochemical characteristics of oceanic arc tholeiite,it is suggested that KPR is an intraoceanic volcanic arc,more specifically,a relic arc(i.e.,rear arc of the ancient IBM) after rifting of ancient IBM. In addition,Amami-Daito province is of arc tectonic affinity,but has been affected by mantle plume. Therefore,based on their respective tectonic evolution history and geochemical characteristics of rock samples,it is inferred that there is no genetic relationship between Japan arc system and KPR. It is noted that rocks reflecting continental crust basement feature have been collected on the northern tip of KPR,which may be related to the process of KPR accreting on Japan arc,but the arc-continent accretion process are still at initial stage of modern continental crust accretion model. However,due to the scarcity of data of the northern tip of KPR,crustal structure of this location and its adjacent Nankai trough need to be further constrained by geophysical studies in the future. 相似文献
993.
994.
红树林海岸的沉积物输运和碳沉降特征 总被引:1,自引:0,他引:1
Mangroves play an important role in sequestering carbon and trapping sediments. However, the effectiveness of such functions is unclear due to the restriction of knowledge on the sedimentation process across the vegetation boundaries. To detect the effects of mangrove forests on sediment transportation and organic carbon sequestration, the granulometric and organic carbon characteristics of mangrove sediments were investigated from three vegetation zones of four typical mangrove habitats on the Leizhou Peninsula coast. Based on our results, sediment transport was often "environmentally sensitive" to the vegetation friction. A transition of the sediment transport mode from the mudflat zone to the interior/fringe zone was often detected from the cumulative frequency curve. The vegetation cover also assists the trapping of material, resulting in a significantly higher concentration of organic carbon in the interior surface sediments. However, the graphic parameters of core sediments reflected a highly temporal variability due to the sedimentation process at different locations. The sediment texture ranges widely from sand to mud, although the sedimentary environments are restricted within the same energy level along the fluvial-marine transition zone. Based on the PCA results, the large variation was mainly attributed to either the mean grain size features or the organic carbon features. A high correlation between the depth and δ13C value also indicated an increasing storage of mangrove-derived organic carbon with time. 相似文献
995.
广西钦州湾百年来红树林演变的有机碳同位素和孢粉示踪及其影响因素 总被引:1,自引:0,他引:1
气候变化和人类活动制约下的红树林演变是一种长时间尺度效应,而沉积物则是记录这种响应的最佳档案。采用古生态学研究思路,选择有效的示踪参数是解读这一档案的有效途径。本文通过广西钦州湾红树林区1根柱状沉积物中有机碳同位素(δ13C)、C/N分析和孢粉鉴定,以沉积物中的红树林源有机碳贡献和红树植物孢粉组合为示踪参数,在210Pb年龄框架构建的基础上,通过对比研究红树林源有机碳贡献和红树孢粉组合特征,揭示百年来钦州湾红树林兴衰和群落演替规律;进而重塑其红树林演变历史:兴盛期(1864-1918年)、衰退期(1918-1968年)和低谷期(1968-2007年),这与土地替代、遥感分析和现场勘测数据较为吻合。结合气候变化和人类活动资料,发现钦州湾红树林的近期衰退主要源于人类活动的影响,尤其是虾塘围垦;而与气候变化关系不大。 相似文献
996.
997.
Codium, one of the largest marine green algal genera, is difficult to delimit species boundary accurately based on morphological identification only. DNA barcoding is a powerful tool for discriminating species of seaweeds. The plastid elongation factor TU(tuf A) is considered as maker to perform DNA barcoding of green algal species than rbc L gene due to universality and rapid evolution rate. We conducted DNA barcoding application to Codium specimens from the Jeju Island, Korea to overcome the limit of morphological identification and to confirm the species diversity. As a result of applying tuf A marker, we newly generated fifty-five tuf A barcodes to resolve eight species. Tuf A marker exhibited 6.1%–21.8% interspecific divergences, wider than the gap of rbc L exon 1,3.5%–11.5%. Molecular analysis of rbc L exon 1 sequences of Codium revealed eight distinct species like tuf A analysis separated in five phylogenetic groups. DNA barcoding of the genus Codium using tuf A marker is more helpful to overcome the limit of morphological identification, and this is more potential to reveal cryptic species and to resolve the relationships among subspecies than rbc L analysis alone. The complement of tuf A barcoding and rbc L analyses including morphology for the genus Codium in the northwestern Pacific will give much more reliable achievement for discovering species diversity and resolving the phylogenetic relationships. 相似文献
998.
为提高鱿鱼加工下脚料的利用率,以秘鲁鱿鱼肝脏为研究对象,采用生物酶解技术和凝胶蛋白分离技术等对其进行研究。研究结果表明:鱿鱼肝脏蛋白酶解液经过超滤处理后(分子质量为20k Da),用Sephadex G-100初步分离,得到五个组分,对分离的组分进行研究,结果表明降血压活性能力最强的是组分二,测定其半抑制浓度(IC50)为1.8mg/m L。对组分二进行活性条件分析,结构表明其ACE抑制活性在温度0—100°C、p H 1—12之间基本没有变化。最后用DEAE阴离子交换柱和Sephadex LH-20对组分二继续分离纯化,得到组分六和组分七,测定其半抑制浓度(IC50)分别达到1.52 mg/m L和2.16 mg/m L。本研究可为利用鱿鱼加工下脚料开发降血压活性肽产品提供理论基础。 相似文献
999.
条子泥一期工程对条子泥发育影响及工程防护措施 总被引:2,自引:0,他引:2
通过历史和现场观测资料并结合遥感卫片资料,对条子泥匡围一期工程两年多的建设过程中,由工程所引起对条子沙洲西大港、东大港、条鱼港等主要的潮沟,及相应的潮盆系统和二分水的剧烈变化进行了分析研究,总结了潮沟摆动治理经验。治理方法主要为丁坝群结合砼连锁块镇压排布防护技术等。 相似文献
1000.
水杨酸对蛋白核小球藻(Chlorella pyrenoidosa) 生长及抗逆相关基因的影响 总被引:1,自引:0,他引:1
以蛋白核小球藻(Chlorella pyrenoidosa)为研究对象, 首先克隆了热激蛋白70(HSP70)和磷 酸甘油酸激酶(PGK)基因全长序列, 然后研究了0-20μg/mL 水杨酸对高温胁迫下HSP70 和PGK 基 因表达, 以及蛋白核小球藻生长、可溶性糖和蛋白含量的影响。结果获得了蛋白核小球藻HSP70 基 因的cDNA 序列2405 bp, 包括60 bp 的5'-非编码区(UTR)、1959 bp 的开放阅读框(ORF)和386 bp 的3'-UTR 和PGK 基因的cDNA 序列1664 bp, 包括35 bp 的5'-UTR, 1398 bp ORF 和231 bp 3'-UTR. 序列比较和分析表明该蛋白核小球藻HSP70 序列与其它绿藻的同源性高达83%-91%, PGK 为 70%-75%.荧光定量PCR 结果显示随着水杨酸浓度的增加, HSP70 和PGK 的表达量在12h 和24h 均有所增加, 而在10 μg/mL 水杨酸浓度下表达量最大, 12h 时分别为对照组的2.57 倍和1.56 倍, 24h 则为1.71 倍和1.79 倍。1-20μg/mL 水杨酸可促进该藻的比生长速率、可溶性糖和蛋白含量的升高。 本文结果表明一定浓度水杨酸对高温胁迫蛋白核小球藻有缓解作用, 且5 和10 μg/mL 水杨酸的效果 最显著。 相似文献