BENTHIC FORAMINIFERA AS BIOINDICATORS OF SALINITY VARIATION IN LAKE SHIHWA, SOUTH KOREA

2015 ◽  
Vol 45 (3) ◽  
pp. 235-249 ◽  
Author(s):  
Yeon Gyu Lee ◽  
Shin Kim ◽  
Yong Wan Kim ◽  
Da Un Jeong ◽  
Jung Sick Lee ◽  
...  
Keyword(s):  
South Korea ◽  
Benthic Foraminifera ◽  
Salinity Variation ◽  
Lake Shihwa

Effects of hypoxia caused by mussel farming on benthic foraminifera in semi-closed Gamak Bay, South Korea

2016 ◽  
Vol 109 (1) ◽  
pp. 566-581 ◽  
Author(s):  
Yeon Gyu Lee ◽  
Da Un Jeong ◽  
Jung Sick Lee ◽  
Yang Ho Choi ◽  
Moon Ok Lee
Keyword(s):  
South Korea ◽  
Benthic Foraminifera ◽  
Mussel Farming ◽  
Gamak Bay

Assessment of Organic Matter Sources in the Singil Stream Flowing into Lake Shihwa, South Korea

2020 ◽  
Vol 53 (2) ◽  
pp. 138-147
Author(s):  
Dahae Kim ◽  
◽  
Jung-Hyun Kim ◽  
Sujin Kang ◽  
Min-Seob Kim ◽  
...  
Keyword(s):  
Organic Matter ◽  
South Korea ◽  
Organic Matter Sources ◽  
Lake Shihwa

Spatial and temporal trends of melamine and its derivatives in sediment from Lake Shihwa, South Korea

2019 ◽  
Vol 373 ◽  
pp. 671-677 ◽  
Author(s):  
Hongkai Zhu ◽  
Sunggyu Lee ◽  
Hyo-Bang Moon ◽  
Kurunthachalam Kannan
Keyword(s):  
South Korea ◽  
Temporal Trends ◽  
Lake Shihwa ◽  
Spatial And Temporal Trends

Environmental and ecological effects of Lake Shihwa reclamation project in South Korea: A review

2014 ◽  
Vol 102 ◽  
pp. 545-558 ◽  
Author(s):  
Chang-Hee Lee ◽  
Bum-Yeon Lee ◽  
Won Keun Chang ◽  
Seongjin Hong ◽  
Sung Joon Song ◽  
...  
Keyword(s):  
South Korea ◽  
Ecological Effects ◽  
Reclamation Project ◽  
Lake Shihwa

PERFLUORINATED COMPOUNDS IN STREAMS OF THE SHIHWA INDUSTRIAL ZONE AND LAKE SHIHWA, SOUTH KOREA

2006 ◽  
Vol 25 (9) ◽  
pp. 2374 ◽  
Author(s):  
Pawel Rostkowski ◽  
Nobuyoshi Yamashita ◽  
Iris Man Ka So ◽  
Sachi Taniyasu ◽  
Paul Kwan Sing Lam ◽  
...  
Keyword(s):  
South Korea ◽  
Perfluorinated Compounds ◽  
Industrial Zone ◽  
Lake Shihwa

Benthic foraminiferal zonation in deep-water carbonate platform margin environments, northern Little Bahama Bank

1988 ◽  
Vol 62 (01) ◽  
pp. 1-8 ◽  
Author(s):  
Ronald E. Martin
Keyword(s):  
Deep Water ◽  
Benthic Foraminifera ◽  
Carbonate Platform ◽  
Sedimentary Facies ◽  
Depositional Environments ◽  
Near Surface ◽  
Sediment Gravity Flows ◽  
Gravity Flows ◽  
Platform Margin ◽  
Water Carbonate

The utility of benthic foraminifera in bathymetric interpretation of clastic depositional environments is well established. In contrast, bathymetric distribution of benthic foraminifera in deep-water carbonate environments has been largely neglected. Approximately 260 species and morphotypes of benthic foraminifera were identified from 12 piston core tops and grab samples collected along two traverses 25 km apart across the northern windward margin of Little Bahama Bank at depths of 275-1,135 m. Certain species and operational taxonomic groups of benthic foraminifera correspond to major near-surface sedimentary facies of the windward margin of Little Bahama Bank and serve as reliable depth indicators. Globocassidulina subglobosa, Cibicides rugosus, and Cibicides wuellerstorfi are all reliable depth indicators, being most abundant at depths >1,000 m, and are found in lower slope periplatform aprons, which are primarily comprised of sediment gravity flows. Reef-dwelling peneroplids and soritids (suborder Miliolina) and rotaliines (suborder Rotaliina) are most abundant at depths <300 m, reflecting downslope bottom transport in proximity to bank-margin reefs. Small miliolines, rosalinids, and discorbids are abundant in periplatform ooze at depths <300 m and are winnowed from the carbonate platform. Increased variation in assemblage diversity below 900 m reflects mixing of shallow- and deep-water species by sediment gravity flows.

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