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Titel Paleoenvironments and sea level changes of Holocene from Nakdong River Delta sediments, Korea
VerfasserIn Daekyo Cheong
Konferenz EGU General Assembly 2015
Medientyp Artikel
Sprache Englisch
Digitales Dokument PDF
Erschienen In: GRA - Volume 17 (2015)
Datensatznummer 250103339
Publikation (Nr.) Volltext-Dokument vorhandenEGU/EGU2015-2748.pdf
 
Zusammenfassung
The Holocene delta sediments(ND-01) which was acquired from the Nakdong River Delta as a rotary-style sediment core in southern Korea is divided into four sedimentary units based on sedimentary structure, texture, and occurrence of microfossils. Unit A(18.8∼33.54 m) is mostly homogeneous mud and shell fragments are well observed. Marine microfossils such as ostracods, diatoms, and sponge spicules decrease towards the top of the core sediments. Unit B(16.6∼18.8 m) is generally laminated mud and laminated sand. Marine microfossils disappear at the top of Unit B, but wood fragments contents increase towards the top. At Unit C(14.2∼16.6 m), mud content is lower than Unit B and laminated sand is well developed. Unit D(8∼14.2 m) is mostly homogeneous sand and shows better sorting than lower unit.. The sedimentary environments of the sequence are supposed to be a progradational delta system.