Evidence of sea ice-driven terrigenous detritus accumulation and deep ventilation changes in the southern Okhotsk Sea during the last 180ka

• Terrigenous detritus changes were reconstructed to 180ka in the southern Okhotsk Sea. • Sea ice expansion/contraction drives terrigenous detritus accumulation and deep ventilation in the Okhotsk Sea. • Mongolia High controlled the sea ice driven change of terrigenous detritus accumulation.

Gespeichert in:
Autor*in:

Zou, Jianjun [verfasserIn]

Shi, Xuefa

Zhu, Aimei

Chen, Min-Te

Kao, Shuhji

Wu, Yonghua

Selvaraj, Kandasamy

Scholz, Patrick

Bai, Yazhi

Wang, Kunshan

Ge, Shulan

Format:

E-Artikel

Sprache:

Englisch

Erschienen:

2015

Schlagwörter:

Okhotsk Sea

Rare earth elements

Terrigenous detritus

Mongolia High

Glacial–interglacial

Sea ice

Deep water ventilation

Umfang:

8

Übergeordnetes Werk:

Enthalten in: Comparison of the prevalence and changing resistance to nalidixic acid and ciprofloxacin of Shigella between Europe–America and Asia–Africa from 1998 to 2009 - 2012transfer abstract, Amsterdam [u.a.]

Übergeordnetes Werk:

volume:114 ; year:2015 ; day:15 ; month:12 ; pages:541-548 ; extent:8

Links:

Volltext

DOI / URN:

10.1016/j.jseaes.2015.07.020

Katalog-ID:

ELV028638840

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