Sources of organic carbon and depositional environment in the Bengal delta plain sediments during the Holocene period-Reference-Cited by-同舟云学术

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Sources of organic carbon and depositional environment in the Bengal delta plain sediments during the Holocene period

Published:2009-11-12 Issue:2 Volume:11 Page:133-142
ISSN:1439-8621
Container-title:Limnology
language:en
Short-container-title:Limnology

Author:

Anawar Hossain M.,Yoshioka Takahito,Konohira Eiichi,Akai Junji,Freitas M. C.,Tareq Shafi M

Publisher

Springer Science and Business Media LLC

Subject

Water Science and Technology,Aquatic Science,Ecology

Link

http://link.springer.com/content/pdf/10.1007/s10201-009-0301-9.pdf

Reference42 articles.

1. Alberdi-Genolet M, Tocco R (1999) Trace metals and organic geochemistry of the Machiques Member (Aptian–Albian) and La Luna Formation (Cenomanian–Campanian), Venezuela. Chem Geol 160:19–38

2. Anawar HM, Akai J, Komaki K, Terao H, Yoshioka T, Ishizuka T, Safiullah S, Kato K (2003) Geochemical occurrence of arsenic in groundwater of Bangladesh: sources and mobilization processes. J Geochem Explor 77:109–131

3. Banakar VK, Parthiban G, Pattan JN, Jauhari P (1998) Chemistry of surface sediment along a north-south transect across the equator in the Central Indian Basin: an assessment of biogenic and detrital influences on elemental burial on the seafloor. Chem Geol 147:217–232

4. Bernasconi SM, Barbieri A, Simona M (1997) Carbon and nitrogen isotope variations in sedimenting organic matter in Lake Lugano. Limnol Oceanogr 42:1755–1765

5. Boldrin A, Langone L, Miserocchi S, Turchetto M, Acri F (2005) Po River plume on the Adriatic continental shelf: dispersion and sedimentation of dissolved and suspended matter during different river discharge rates. Mar Geol 222–223:135–158

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