Effects of the middle Holocene high sea-level stand and climate on Amazonian mangroves     

Marcelo C. L. Cohen  Paloma Maria Pinto Camargo  Luiz C. R. Pessenda  Flávio Lima Lorente  Adriana V. De Souza  José Augusto Martins Corrêa  José Bendassolli  Marianne Dietz 《第四纪科学杂志》2021,36(6):1013-1027

The high sea-level stand during the mid-Holocene is a benchmark in mangrove dynamics along the north-east/south-east coast of Brazil and provides a reference point for landward and seaward mangrove migrations corresponding to changes in relative sea level (RSL). However, evidence of the impacts associated with RSL fall on the northern Brazilian coast is scarce. Multi-proxy data from the highest tidal flats of the Bragança Peninsula in northern Brazil revealed modern herbaceous areas were occupied by mangroves Rhizophora and Avicennia from ~6250 to ~5850 cal a bp , and only Avicennia between ~5850 and ~5000 cal a bp . The same tidal flats were vegetation-free between ~5000 and ~4300 cal a bp . A combination of a high sea-level stand (0.6 ± 0.1 m) at ~5000 cal a bp and a dry early–middle Holocene in the Amazon probably caused an increase in porewater salinity of tidal flats, which resulted in a mangrove succession from Rhizophora to Avicennia dominance. RSL fall accentuated this process, contributing to mangrove degradation between ~5000 and ~4300 cal a bp . RSL fall, and a wetter period over the past ~4300 cal a bp caused a mangrove migration from highest to lowest flats, followed by expansion of herbaceous vegetation on the highest flats.  相似文献   

Structural,metamorphic and geochronological record in the Goszów quartzites of the Orlica–Śnieżnik Dome (SW Poland): implications for the polyphase Variscan tectonometamorphism of the Saxothuringian terrane     

Miros&#x;aw Jastrz&#x;bski  Bartosz Budzy&#x;  Wojciech Stawikowski 《Geological Journal》2016,51(3):455-479

This integrated study on the pressure–temperature–deformation‐time record of the Goszów light quartzites from the Młynowiec–Stronie Group (Sudety Mts., SW Poland) provides new data that improve our understanding of the structure and geodynamic development of the Orlica–Śnieżnik Dome (OSD) as a Gondwana‐derived unit involved in the formation of the Variscan orogen. The structural and metamorphic record of the Goszów light quartzites, when compared to the under‐ and overlying rock formations, indicates that the whole Młynowiec–Stronie Group in the eastern part of the Saxothuringian terrane functioned as a single, integral lithotectonic unit with no visible structural or metamorphic discontinuities. The sequence of structures and thermodynamic modelling indicate that the light quartzites underwent the same polyphase tectonometamorphic evolution as the adjacent rocks belonging to the Młynowiec–Stronie Group. The development of tight, N–S‐trending folds and axial penetrative metamorphic foliation was related to metamorphic progression from 500 °C to 640 °C at 6–7 kbar. Subsequently, under the retrogressive conditions below 540 °C, the foliation was reactivated as a result of subsequent N–S‐directed ductile shearing and extension. Therefore, the study of the light quartzites exemplifies the penetrative structures in the OSD, and the metamorphic foliation and N–S‐trending lineation are composite structures. The monazite metamorphic ages of ca. 364 Ma and 335 Ma may be related to the approximately E–W‐ and N–S‐oriented tectonic movements, respectively, which occurred during the amalgamation of the Saxothuringian terrane with Brunovistulia. In contrast, the previously unknown early Palaeozoic monazite age of ca. 494 Ma is interpreted as the protolith age of the light quartzites. Copyright © 2015 John Wiley & Sons, Ltd.  相似文献   

基准站的网形对机载差分GPS定位测速结果的影响     

宋雪源  马国元  贾赞杰  史线龙  孙中豪 《测绘信息与工程》2011,36(4):28-31

采用实测数据,进行了事后处理比较与分析,讨论了单基站差分和多基站差分的关系,分析了基准站的网形对多基站差分的影响,得出了一些有益的结论。  相似文献   

福建建阳井后钼矿地质特征及成因探讨   总被引：1，自引：0，他引：1  

章振国 《福建地质》2011,30(3):211-217

建阳井后钼矿位于闽西北隆起带东缘,浦城一永泰南北向构造岩浆活动带中部。矿床形成于燕山晚期,主要受区域上南北向断裂构造带控制的隐伏斑岩体控制。矿体以线脉一细脉及石英大脉型为主,围岩为中一晚元古代马面山群大岭组变质岩与加里东期二长花岗岩。  相似文献   

A possible generation mechanism of the strong current over northwestern shelf of the South China Sea     

WANGGang  QIAOFangli  DAIDejun  HOUYijun 《海洋学报(英文版)》2011,30(3)

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Statistical characteristics of long waves nearshore     

Ira Didenkulova  Efim Pelinovsky  Anna Sergeeva 《Coastal Engineering》2011

The random long wave runup on a beach of constant slope is studied in the framework of the rigorous solutions of the nonlinear shallow water theory. These solutions are used for calculation of the statistical characteristics of the vertical displacement of the moving shoreline and its horizontal velocity. It is shown that probability characteristics of the runup heights and extreme values of the shoreline velocity coincide in the linear and nonlinear theory. If the incident wave is represented by a narrow-band Gaussian process, the runup height is described by a Rayleigh distribution. The significant runup height can also be found within the linear theory of long wave shoaling and runup. Wave nonlinearity nearshore does not affect the Gaussian probability distribution of the velocity of the moving shoreline. However the vertical displacement of the moving shoreline becomes non-Gaussian due to the wave nonlinearity. Its statistical moments are calculated analytically. It is shown that the mean water level increases (setup), the skewness is always positive and kurtosis is positive for weak amplitude waves and negative for strongly nonlinear waves. The probability of the wave breaking is also calculated and conditions of validity of the analytical theory are discussed. The spectral and statistical characteristics of the moving shoreline are studied in detail. It is shown that the probability of coastal floods grows with an increase in the nonlinearity. Randomness of the wave field nearshore leads to an increase in the wave spectrum width.  相似文献   

Paleoenvironmental changes in the northern South China Sea over the past 28,000 years: A study of TEX₈₆-derived sea surface temperatures and terrestrial biomarkers   总被引：1，自引：0，他引：1  

Tomoya Shintani  Masanobu Yamamoto  Min-Te Chen 《Journal of Asian Earth Sciences》2011,40(6):87-1229

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南海北部初级生产力的物理-生物海洋学耦合特征及其对固碳量的影响     

郝锵  宁修仁  蔡昱明  刘诚刚  乐凤凤 《海洋学研究》2011,29(2):46-57

通过修订的VGPM模型,利用南海北部7年平均SeaWiFS和AVHRR遥感资料,分析了该海域河口上升流及反气旋涡等生境表层叶绿素浓度和初级生产力的周年变化,结果表明,季风驱动下的物理一生物海洋学耦合过程是控制研究海域浮游植物生物量和初级生产力时空变化的主导因素.浮游植物生物量和初级生产力随着季风、环流以及中尺度涡等物理...  相似文献   

2007/2008年和2008/2009年夏季南大洋以及普里兹湾POC的分布与变化   总被引：2，自引：0，他引：2       下载免费PDF全文

韩正兵  扈传昱  薛斌  潘建明  张海生 《极地研究》2011,23(1):11-18

在中国第24次和第25次南极科学考察期间,利用航渡表层水观测和普里兹湾定点观测,对颗粒有机碳(POC)的分布及其影响因素进行了研究.结果表明,南大洋表层水体的颗粒有机碳分布具有明显的区域性特征,表层水体POC的含量与营养盐和叶绿素a有着明显的相关分布趋势.南极水、亚南极水的表层POC浓度明显高于亚热带水和热带水,第24...  相似文献   

黑龙江省五林洞幅中生代地层特征简述     

张午 《吉林地质》2014,(1):11-13

在大量野外资料基础上,本文对五林洞幅中生代各地层特征进行描述,并描述各地层单元地质特征、出露地点、接触关系及划分依据。  相似文献