Development of the East Asian summer monsoon: Evidence from the sediment record in the South China Sea since 8.5 Ma

128 samples from Ocean Drilling Program (ODP) Site 1143 in the southern South China Sea were analyzed for grain size, clay minerals, biogenic opal content and quartz in order to reconstruct changes in East Asian monsoon climate since 8.5 Ma. An abrupt change of terrigenous mass accumulation rate (MAR), clay mineral assemblage, median grain size and biogenic opal MAR about 5.2 Ma suggests that between 8.5-5.2 Ma the source of terrigenous sediment was mainly in the region of surface uplift and basaltic volcanism in southern Vietnam. A simple model of East Asian summer monsoon evolution was based on the clay/feldspar ratio, kaolinite/chlorite ratio and biogenic opal MAR. The summer monsoon has two periods of maximum strength at 8.5-7.6 Ma and 7.1-6.2 Ma. Subsequently, there was a relatively stable period at 6.2-3.5 Ma, continued intensification about 3.5-2.5 Ma, and gradually weakening after 2.5 Ma. Since 1 Ma the monsoon has intensified, with remarkable high-frequency and amplitude variability. Simultaneous increase in sedimentation rates at ODP Sites 1143, 1146 and 1148, as well as in MAR of terrigenous materials, quartz, feldspar and clay minerals at ODP Site 1143 at 3.5-2.5 Ma, may be the erosional response to both global climatic deterioration and the strengthening of the East Asian summer monsoon after about 3-4 Ma.     

Fluxes and isotopic composition of planktonic foraminifera off Hainan Island,northern South China Sea: Implications for paleoceanographic studies

Planktonic foraminifera collected from a sediment trap deployed off Hainan in the northwestern South China Sea (SCS-NW) between July 2012 and April 2013 were studied to evaluate their seasonal variability and ecology as well as to infer the factors controlling their shell fluxes. The total planktonic foraminifera flux, as well as the fluxes of the dominant species (Globigerinoides ruber, Globigerinoides sacculifer and Neogloboquadrina dutertrei), showed three distinct maxima during SW-monsoon in August 2012, the SW-NE intermonsoon in October 2012 and the NE-monsoon in December 2012–February 2013. These periods were characterized by upwelling, aerosol fallout, and intense wind mixing, respectively, from which the foraminiferal assemblages benefitted, as indicated by the close correlation between wind speed, sea surface temperature (SST), chlorophyll a concentration (Chl-a), δ¹⁸O of G. ruber and the shell fluxes. The correlation also suggests that temperature and food availability might have been the primary drivers of the observed changes in foraminiferal abundance. The offset between the SST deduced from flux-weighted of G. ruber δ¹⁸O and annual mean SST is only ∼0.3 °C, much lower than ∼5.2 °C between the summer and winter temperature, indicating a balanced seasonality bias in the shell flux. The linear regression between the satellite-derived sea surface temperature and G. ruber δ¹⁸O reveals the strong potential of this species, at least in the studied region, as an ecological indicator for past oceanic environments.     

Fatty acid composition indicating diverse habitat use in coral reef fishes in the Malaysian South China Sea

Background

In order to understand feeding ecology and habitat use of coral reef fish, fatty acid composition was examined in five coral reef fishes, Thalassoma lunare, Lutjanus lutjanus, Abudefduf bengalensis, Scarus rivulatus and Scolopsis affinis collected in the Bidong Island of Malaysian South China Sea.

Results

Proportions of saturated fatty acids (SAFA) ranged 57.2% 74.2%, with the highest proportions in fatty acids, the second highest was monounsaturated fatty acids (MUFA) ranged from 21.4% to 39.0% and the proportion of polyunsaturated fatty acids (PUFA) was the lowest ranged from 2.8% to 14.1%. Each fatty acid composition differed among fishes, suggesting diverse feeding ecology, habitat use and migration during the fishes’ life history in the coral reef habitats.

Conclusions

Diets of the coral fish species might vary among species in spite of that each species are living sympatrically. Differences in fatty acid profiles might not just be considered with respect to the diets, but might be based on the habitat and migration.     

China,Vietnam, and the South China Sea: Disputes and Dispute Management

This article examines recent developments in the South China Sea; in particular, the China-Vietnam relationship. The developments are presented in the broader context of the Sino-Vietnamese approach to managing border disputes since full normalization of relations in late 1991. The challenges for China and Vietnam in managing their disputes and related tension in the South China Sea are also discussed.     

Temporal and spatial patterns in salinity and suspended solids in a reservoir influenced by the Asian monsoon

Between April 1993 and November 1994, conductivity, cations, anions and suspended solids were measured at multiple sites in Taechung Reservoir, Korea. The major mechanism regulating ionic composition was dilution by monsoon rain and a resulting interflow current; these forces caused marked spatial and temporal heterogeneity. Ionic dilution was most pronounced in the headwaters during an intense monsoon in 1993 and was accompanied by an increase in the proportion of Na⁺and Cl^–, presumably from rainwater. A decrease of >25% in conductivity and cations occurred during summer 1993 at the plunge-point due to a temperature difference between the lake water and an interflow. In contrast, the 1994 monsoon was weak, ionic dilution was not apparent, and spatial-temporal variation was modest. Overall reservoir salinity was a direct function of water residence time which is regulated by monsoon intensity. Differences in hydrology between years also influenced seston composition; inorganic suspended solids dominated total suspended solids in 1993, but in 1994 the organic fraction was the major component.     

Storm cycles in the last millennium recorded in Yongshu Reef, southern South China Sea

Large storm-relocated Porites coral blocks are widespread on the reef flats of Nansha area, southern South China Sea. Detailed investigations of coral reef ecology, geomorphology and sedimentation on Yongshu Reef indicate that such storm-relocated blocks originated from large Porites lutea corals growing on the spurs within the reef-front living coral zone. Because the coral reef has experienced sustained subsidence and reef development during the Holocene, dead corals were continuously covered by newly growing coral colonies. For this reason, the coral blocks must have been relocated by storms from the living sites and therefore the ages of these storm-relocated corals should approximate the times when the storms occurred. Rapid emplacement of these blocks is also evidenced by the lack of coral overgrowth, encrustation or subtidal alteration.U-series dating of the storm-relocated blocks as well as of in situ reef flat corals suggests that, during the last 1000 years, at least six strong storms occurred in 1064±30, 1210±5-1201±4, 1336±9, 1443±9, 1685±8-1680±6, 1872±15 AD, respectively, with an average 160-year cycle (110-240 years). The last storm, which occurred in 1872±15 AD, also led to mortality of the reef flat corals dated at ∼130 years ago. Thus, the storm had significant impacts on coral reef ecology and morphology.     

The spatial and temporal distribution of microalgae in the South China Sea: evidence from GIS-based analysis of 18S rDNA sequences

The purpose of this study was to estimate the spatial and temporal variation of microalgae in the South China Sea and to demonstrate the environmental factors controlling the diversity of microalgae by GIS (geographic information system)-based analysis of 18S rDNA sequences. Six 18S rDNA libraries were constructed from environmental samples collected at different sites in the study area, and more than 600 18S rDNA sequences were determined. The rDNA sequence data were then analyzed by DIVA-GIS software to display the spatial and temporal variation of phytoplankton’s composition. It was shown that the autotrophic eukaryotic plankton dominated over the heterotrophic cells in most of our clone libraries, and the dominating phytoplankton was Dinophyceae except for Bacillariophyta at the Xiamen harbor. The percentages of these two groups were controlled by water temperature and salinity. Our results also revealed that the species composition of Chlorophyta showed a close relationship with latitude, changing from Prasinophyceae at the high latitude to Trebouxiophyceae at the low latitude. Several newly classified picoplankton lineages were first uncovered in the South China Sea, including the pico-sized green alga Ostreococcus sp. and Picochlorum eukaryotum, and picobiliphytes, which was just discovered in 2007 with unknown affinities to other eukaryotes. Their spatial and temporal variation were also analyzed and discussed.     

A Code of Conduct for Human and Regional Security Around the South China Sea

In the past decade, there have been calls for a regional code of conduct for the South China Sea to ensure peace and stability in a region replete with conflicting territorial claims over offshore geographical features. This paper will distinguish between the process of codification of rules and principles in one document, on the one hand, and the process of implementing existing rules and principles, on the other hand. It will be argued that rules and principles governing conduct for human and regional security around the South China Sea already exist in many forms and that the South China Sea states are obligated by international law to implement them without waiting for their consolidation in one document.     

Vietnam and the Code of Conduct for the South China Sea

This article portrays and characterizes the Vietnamese position toward the settlement of the island disputes in the South China Sea. The situation in the South China Sea has become more complicated since 1988 when China made its steps toward the Spratlys. After analyzing the situation in the South China Sea, the author emphasizes the need to have a code of conduct for this disputed area.     

China's Nine Dotted Lines in the South China Sea: The 2011 Exchange of Diplomatic Notes Between the Philippines and China

Important events relating to the sovereignty dispute over the Spratly Islands have arisen by fits and starts since 2009, marking the start of a new phase in the legal battle over territorial and maritime claims in the South China Sea. While the exchange of legal arguments between the parties has gradually laid bare their maritime claims, much still remains shrouded in uncertainty. Among the obscure claims wanting clarification is China's infamous nine-dotted-line map, which in 2011 elicited a response and counterresponse between the Philippines and China. This article examines the maritime and territorial claims of the Philippines and China as revealed in the recent discord over the nine-dotted-line map.     

南海南沙海域沉积物中可培养微生物及其多样性分析

【目的】为了从南沙海域中分离获得微生物菌种资源,【方法】本文通过沉积物采样、可培养菌分离及16S rRNA鉴定,【结果】从22个站点的沉积物样品中获得349株细菌,分属于87个种。发现产芽孢细菌分布最广,并在10个站点的分离株中占多数;它们是Bacillus,Halobacillus,Brevibacillus,Paenibacillus,Pontibacillus和Thalassobacillus。其中芽孢杆菌（Bacillus）无论在数量上还是种类上都最多,分别属于34种,其中有8个可能的新种。此外,g-Proteobacteria是分离率较高的另一亚群;其中,假单胞菌（Pseudomonas）,海杆菌（Marinobacter）,食烷菌（Alcanivorax）属的细菌最多。统计还发现,在深度750~2000 m之间,低GC含量的细菌最丰富,而深度2000 m以下,分离株则全部为g-Proteobacteria。【结论】南沙沉积物可培养微生物中产芽孢细菌及 g-Proteobacteria比较丰富;其中,产芽孢细菌的多样性最高,具有进一步研究开发价值。     

南海西北部陆架区鱼类的种类组成与群落格局

根据2006-2007年在南海西北部陆架区海域进行的4航次底拖网调查数据,对该海域鱼类的种类组成和群落格局进行分析.调查共采获鱼类262种,隶属于20目102科.以冬季出现种类数最多,为166种;夏季和秋季次之,分别为161种和155种;春季最少,为135种.运用聚类分析和非度量多维标度(NMDS)方法分析了南海西北部陆架区鱼类群落结构的空间分布.研究表明,该海域鱼类可划分为5个群落,分别为粤西沿岸群落(群落Ⅰ)、海南岛东南沿岸群落(群落Ⅱ)、海南岛东部深海群落(群落Ⅲ)、过渡群落(群落Ⅳ)和混合群落(群落Ⅴ).ANOSIM检验表明,各群落间鱼类组成的差异极为显著(R=0.847-0.939,P＜0.001).鱼类群落格局的变化与海流和水深关系密切,有较明显的沿水深梯度分布的规律.咸淡水鱼类在雷州半岛东部的冷涡区域,形成群落Ⅰ;南海暖流控制区域内的深海鱼类,形成群落Ⅲ;在南海暖流最为强劲的冬季,研究区域内大部分鱼类集结为混合性群落Ⅴ;琼东南沿岸的上升流区内形成群落Ⅱ;沿岸流强劲的夏、秋季,在沿岸流和上升流交汇处,形成过渡性群落Ⅳ.     

Regional Cooperation in the South China Sea: Analysis of Existing Practices and Prospects

This article identifies potential areas of cooperation in the South China Sea, particularly on ocean-related matters. Several regional mechanisms related to marine and coastal environments have been established and, to an extent, have achieved their goals. Nevertheless, some improvements to existing mechanisms are highly desirable. Recommended is a regional mechanism that involves all bordering parties; limits its geographic scope to the South China Sea; is initiated and operates without the assistance of global organizations; is embodied in a legally binding instrument; and broadens the scope of cooperation to include marine living resources, maritime safety, and maritime security.     

Coastal States in the South China Sea and Submissions on the Outer Limits of the Continental Shelf

The purpose of this article is to examine the outer continental shelf submissions made by the coastal states of the South China Sea and their potential impact on legal and political developments in the South China Sea. In accordance with the United Nations Convention on the Law of the Sea of 1982 and the guidelines of the Commission on the Limits of the Continental Shelf, coastal states are to establish the outer limits of their continental shelf where it extends beyond 200 nautical miles. Meeting this obligation is complicated in enclosed or semienclosed seas where there are maritime disputes such as in the South China Sea.     

南海南部悬浮颗粒物脂肪酸组成

中国水产科学研究院南海水产研究所"南锋号"科考船在2012年2月22日—3月20日调查期间,对南海南部海域0 m、75 m和150 m层水体悬浮颗粒物进行了脂肪酸(FA)组成的研究。FA含量在表层、75 m层和150 m层的变化范围分别为9.9—15.65μg/L,10.45-14.45μg/L和9.65—16.45μg/L。FA与叶绿素a的比值垂向变化非常大,在表层和150 m层都大于70,而在75 m层小于30(除A7)。悬浮颗粒物的FA组成以饱和脂肪酸和单不饱和脂肪酸为主,而多不饱和脂肪酸含量较低。饱和脂肪酸主要包括C16:0和C18:0,其次是C12:0,单不饱和脂肪酸主要包括C14:1n3、C16:1n7和C16:1n9,多不饱和脂肪酸主要为C18:2n6和C22:2n6。主成分分析表明,第一主成分主要与C16:0、C18:0、C20:0等正相关,可认为第一主成分主要表征浮游植物和碎屑,而第二主成分所表征的可能与浮游动物等有关的信息。悬浮颗粒物的脂肪酸标记物中,C16:1n7/C16:0和∑C16:1/∑FA之间呈显著正相关,同时C16:1n7/C16:0与∑C18/∑FA呈显著负相关,将C16:1n7/C16:0和C16:1/∑FA结合起来适宜于指示硅藻类的组成,∑C18/∑FA可用来指示甲藻类组成。     

Archaeal Diversity and Spatial Distribution in the Surface Sediment of the South China Sea

Archaea represent a significant portion of biomass in the marine sediments and may play an important role in global carbon cycle. However, the identity and composition of deep sea sediment Archaea are unclear. Here, we used the archaeal 16S rRNA gene primers to determine the diversity and community structure of Archaea from shallow water (<100 m) and deep water (>1500 m) sediments in the South China Sea. Phylogenetically the archaeal community is separated between the shallow- and deep sea sediments, with the former being dominated by the Thaumarchaeota and the latter by the Marine Benthic Group B, E and the South African GoldMine Euryarchaeotal Group as well as Thaumarchaeota. Sand content showed significant correlation with Thaumarchaeota, suggesting that the porous media may create an oxic environment that allowed these aerobic organisms to thrive in the surface sediments. The carbon isotope composition of total organic carbon was significantly correlated to the distribution of archaeal groups, suggesting that Archaea overall may be constrained by the availability or sources of organic carbon in the sediments of the South China Sea.     

南海南部陆坡表层沉积物细菌和古菌多样性

从南海南部陆坡表层沉积物中扩增了细菌和古菌16S rDNA序列,并对克隆子文库进行系统发育分析.细菌序列以变形杆菌(Proteobacteria)居多,其次是浮霉菌(Planctomycete)、酸杆菌(Acidobacteria)和candidate division OP10,另外还有少量铁还原杆菌(Deferrobacteres)、candidate division OP3、OP11、OP8、TM6、疣微菌(Verrucomicrobia)和螺旋体(Spirochaetes).古菌序列分别来自泉古生菌(Crenarchaeota)和广古生菌(Euryarchaeota),以Marine Benthic Group B(MBGB)、MarineCrenarchaeotic Group Ⅰ(MGⅠ)、Marine Benthic Group D(MBGD)和South African Gold Mine Euryarchaeotic Group(SAGMEG)为主.少量序列为C3、甲烷杆菌(Methanobacteriales)和Novel Euryarchaeotic Group(NEG).结果表明海底表层沉积物中有丰富多样的微生物群落.     

南海环境微生物对聚球藻有机物质的响应

【背景】海洋浮游植物产生的有机物质与异养细菌之间的相互作用是上层海洋物质和能量循环过程中的重要组成部分。【目的】探究寡营养海域微生物群落对聚球藻有机物(Synechococcus-derived organic matter,SOM)的响应和代谢利用过程,加深对海洋微生物介导的生物地球化学循环过程的认识。【方法】利用南海海域微生物群落,添加聚球藻有机物质后黑暗培养,对培养过程中有机碳、营养盐和活性微生物群落结构的变化进行追踪。【结果】在短期的培养过程中,有60%-73%的SOM被微生物所利用。γ-变形菌(Gammaproteobacteria)在培养过程中响应最快,也是最优势微生物类群。SOM的加入改变了原位微生物群落结构,并且随着活性有机物质逐步被消耗,微生物群落结构也发生了演替。【结论】SOM中的大部分物质都属于活性有机物质,可以快速地被微生物所降解利用。不同微生物类群响应不同生物可利用性有机物质,推动了海洋物质和能量的循环。     

The U-Shaped Line and a Categorization of the Ocean Disputes in the South China Sea

A principal aspect of the territorial and boundary delimitation disputes in the South China Sea is the so-called U-shaped line. This article addresses the genesis and substantiation of the U-shaped line claims as well as the possible change in positions of the governments of the Republic of China and the People's Republic of China with respect to the historical waters claim, which is an integral part of their U-shaped line positions. A legal analysis of the various communications of the South China Sea players with respect to the U-shaped line helps to clarify and identify the nature of four kinds of legal disputes. It is also possible to differentiate the various degrees of difficulty involved in settling each of these disputes.     

中国南中国海海岸湿地的保护和管理

中国南中国海湿地是中国各类生态系统中生物多样性最为丰富的地区之一,也是中国人口稠密、经济发达的地区。范围包括广东省、香港特别行政区、澳门特别行政区、广西壮族自治区和海南省等5个行政区。该区海岸湿地总面积约为1.54×104km2。海岸湿地处于海陆的交错地带,是脆弱的生态敏感区。由于受人口增加和经济发展的巨大压力,中国南中国海湿地破坏严重,退化趋势明显。本文在对中国南中国海地区海岸湿地的现状、类型及湿地退化的主要原因进行分析的基础上,提出中国南中国海地区海岸湿地资源保护与管理的建议,以便切实保护中国南中国海沿海多样化的湿地类型,持续发挥其生态服务功能。