Methylmercury in fish from the South China Sea: Geographical distribution and biomagnification

2013 ◽  
Vol 77 (1-2) ◽  
pp. 437-444 ◽  
Author(s):  
Aijia Zhu ◽  
Wei Zhang ◽  
Zhanzhou Xu ◽  
Liangmin Huang ◽  
Wen-Xiong Wang
Keyword(s):  
South China Sea ◽  
Geographical Distribution ◽  
South China ◽  
The South China Sea ◽  
The South ◽  
China Sea

scholarly journals GEOGRAPHICAL DISTRIBUTION AND STATUS OF SCADS POPULATION IN THE WATERS OF THE SOUTHERN PART OF THE SUNDA SHELF

2017 ◽  
Vol 11 (1) ◽  
pp. 1
Author(s):  
Suherman Banon Atmaja ◽  
Duto Nugroho
Keyword(s):  
South China Sea ◽  
Geographical Distribution ◽  
South China ◽  
The South China Sea ◽  
Purse Seine ◽  
The South ◽  
Offshore Water ◽  
Sunda Shelf ◽  
China Sea

The scads population have long been exploited in ldonesia Exploitation to the offshore water started when purse seine was introdused in 1970. The exploitation extends eastwards to the Macassar Strait and nonhwards to the southern part of the south china sea.

scholarly journals Supplemental Material: Crustal and upper mantle structure beneath the South China Sea and Indonesia

2020 ◽  
Author(s):  
V. Corchete
Keyword(s):  
South China Sea ◽  
Geographical Distribution ◽  
South China ◽  
Upper Mantle ◽  
The South China Sea ◽  
Mantle Structure ◽  
Inversion Process ◽  
The South ◽  
China Sea ◽  
Upper Mantle Structure

Figure S1: Geographical distribution of the 1-sigma errors arisen in computation of the S-velocities shown in Figure 3. The interval between isolines is 0.01 km/s; Figure S2. Resolution maps of the inversion process performed to calculate the S-velocities shown in Figure 3, plotted from 0 (not resolved) to 1 (perfect resolution). The interval between isolines is 0.1.

Weltneria acanthostoma sp. nov., a burrowing barnacle (Cirripedia: Acrothoracica) from the deep-waters of the South China Sea

Zootaxa ◽  
2017 ◽  
Vol 4290 (3) ◽  
pp. 591 ◽  
Author(s):  
GREGORY A. KOLBASOV ◽  
BENNY K.K. CHAN ◽  
YU-RONG CHENG
Keyword(s):  
South China Sea ◽  
Geographical Distribution ◽  
South China ◽  
Deep Water ◽  
The South China Sea ◽  
Blue Ridge ◽  
The South ◽  
Single Female ◽  
China Sea ◽  
Deep Waters

A new deep water acrothoracican species, Weltneria acanthostoma sp. nov., has been discovered from the area of the Blue Ridge Seamount, South China Sea, at a depth of 534 m. A single female was found in a burrow in the scleractinian Madrepora oculata. This specimen is assigned to the genus Weltneria due to the possession of six pairs of cirri and two-joined caudal appendages. Weltneria acanthostoma differs from its congeners in the morphology of the slightly sinusoid opercular bars having hooked posterior processes and four or five curved, conspicuous, simple teeth, and by the absence of a calcareous formation of the attachment disk. The genus Weltneria exhibits a Tethyan relictual pattern in its geographical distribution. The diagnosis of Weltneria is based on symplesiomorphies and the genus may be a non-monophyletic taxon. 

Species composition and geographical distribution of fishes in Tungsha Island and Taiping Island in the South China Sea

2012 ◽  
Vol 19 (6) ◽  
pp. 737-763
Author(s):  
Shao Kwang-Tsao ◽  
Chen Jeng-Ping ◽  
Chen Ching-Yi ◽  
Huang Cheing-Hua ◽  
Kuo Jen-Wei
Keyword(s):  
South China Sea ◽  
Species Composition ◽  
Geographical Distribution ◽  
South China ◽  
The South China Sea ◽  
The South ◽  
China Sea

scholarly journals Supplemental Material: Crustal and upper mantle structure beneath the South China Sea and Indonesia

2020 ◽  
Author(s):  
V. Corchete
Keyword(s):  
South China Sea ◽  
Geographical Distribution ◽  
South China ◽  
Upper Mantle ◽  
The South China Sea ◽  
Mantle Structure ◽  
Inversion Process ◽  
The South ◽  
China Sea ◽  
Upper Mantle Structure

Figure S1: Geographical distribution of the 1-sigma errors arisen in computation of the S-velocities shown in Figure 3. The interval between isolines is 0.01 km/s; Figure S2. Resolution maps of the inversion process performed to calculate the S-velocities shown in Figure 3, plotted from 0 (not resolved) to 1 (perfect resolution). The interval between isolines is 0.1.

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