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Literature DB >> 19049009

Marine biopolymer self-assembly: implications for carbon cycling in the ocean.

Pedro Verdugo¹, Monica V Orellana, Wei-Chun Chin, Timothy W Petersen, Ger van den Eng, Ronald Benner, John I Hedges.

Abstract

Dissolved organic matter is the largest reservoir of reduced carbon in the ocean and is primarily composed of small biopolymers. It is a critical substrate for the microbial community and plays a pivotal role in global carbon cycling.

Entities: Chemical

Mesh：

Substances：
Biopolymers
Carbon

Year: 2008 PMID： 19049009 DOI： 10.1039/b800149a

Source DB: PubMed Journal: Faraday Discuss ISSN： 1359-6640 Impact factor: 4.008

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Cited

6 in total

1. Filtration of submicrometer particles by pelagic tunicates.

Authors: Kelly R Sutherland; Laurence P Madin; Roman Stocker
Journal: Proc Natl Acad Sci U S A Date: 2010-08-09 Impact factor: 11.205

2. Polymer networks produced by marine diatoms in the northern Adriatic sea.

Authors: Vesna Svetličić; Vera Žutić; Tea Mišić Radić; Galja Pletikapić; Amela Hozić Zimmermann; Ranieri Urbani
Journal: Mar Drugs Date: 2011-04-21 Impact factor: 6.085

3. Effects of engineered nanoparticles on the assembly of exopolymeric substances from phytoplankton.

Authors: Chi-Shuo Chen; Jesse M Anaya; Saijin Zhang; Jessica Spurgin; Chia-Ying Chuang; Chen Xu; Ai-Jun Miao; Eric Y-T Chen; Kathleen A Schwehr; Yuelu Jiang; Antonietta Quigg; Peter H Santschi; Wei-Chun Chin
Journal: PLoS One Date: 2011-07-21 Impact factor: 3.240

Marine biopolymer self-assembly: implications for carbon cycling in the ocean.

1. Filtration of submicrometer particles by pelagic tunicates.

2. Polymer networks produced by marine diatoms in the northern Adriatic sea.

3. Effects of engineered nanoparticles on the assembly of exopolymeric substances from phytoplankton.

4. Carbonaceous particles reduce marine microgel formation.

5. Bacterial versus archaeal origin of extracellular enzymatic activity in the Northeast Atlantic deep waters.

6. Dragon kings of the deep sea: marine particles deviate markedly from the common number-size spectrum.