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CORRECTION article

Front. Mar. Sci., 26 June 2018
Sec. Marine Biogeochemistry
Volume 5 - 2018 | https://doi.org/10.3389/fmars.2018.00230

Corrigendum: Composition of Dissolved Organic Matter in Pore Waters of Anoxic Marine Sediments Analyzed by 1H Nuclear Magnetic Resonance Spectroscopy

This article is a correction to:

  1. Composition of Dissolved Organic Matter in Pore Waters of Anoxic Marine Sediments Analyzed by 1H Nuclear Magnetic Resonance Spectroscopy

    1. Read original article
\r\nChristina A. Fox&#x;Christina A. Fox1†Hussain A. AbdullaHussain A. Abdulla2David J. BurdigeDavid J. Burdige3James P. LewickiJames P. Lewicki4Tomoko Komada*Tomoko Komada1*
  • 1Estuary & Ocean Science Center, San Francisco State University, Tiburon, CA, United States
  • 2Department of Physical and Environmental Sciences, Texas A&M University-Corpus Christi, Corpus Christi, TX, United States
  • 3Department of Ocean, Earth & Atmospheric Sciences, Old Dominion University, Norfolk, VA, United States
  • 4Materials Science Division, Lawrence Livermore National Laboratory, Livermore, CA, United States

A corrigendum on
Composition of Dissolved Organic Matter in Pore Waters of Anoxic Marine Sediments Analyzed by 1H Nuclear Magnetic Resonance Spectroscopy

by Fox, C. A., Abdulla, H. A., Burdige, D. J., Lewicki, J. P., and Komada, T. (2018). Front. Mar. Sci. 5:172. doi: 10.3389/fmars.2018.00172

In the original article, there was a mistake in Figure 7 as published. The chemical shift range displayed for aliphatic CRAM protons should read 1.9-0.9 ppm, not 1.9-0.2 ppm. The corrected Figure 7 appears below. The authors apologize for this error and state that this does not change the scientific conclusions of the article in any way.

FIGURE 7
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Figure 7. (Left) 4 columns (8 panels): Fraction of CRAM protons that resonated in δH ranges corresponding to peaks and bands defined in Table 2. The sum of these sections accounted for ~94% of the total CRAM envelope (see section CRAM). Far (Right) column (2 panels): Fraction of CRAM protons that resonated in the aliphatic and functionalized δH ranges as defined in Table 1.

The original article has been updated.

Conflict of Interest Statement

The authors declare that the research was conducted in the absence of any commercial or financial relationships that could be construed as a potential conflict of interest.

Keywords: pore water, DOM, carbon, NMR, sediment, anoxic, marine, Santa Barbara Basin

Citation: Fox CA, Abdulla HA, Burdige DJ, Lewicki JP and Komada T (2018) Corrigendum: Composition of Dissolved Organic Matter in Pore Waters of Anoxic Marine Sediments Analyzed by 1H Nuclear Magnetic Resonance Spectroscopy. Front. Mar. Sci. 5:230. doi: 10.3389/fmars.2018.00230

Received: 13 June 2018; Accepted: 14 June 2018;
Published: 26 June 2018.

Edited and reviewed by: Frontiers in Marine Science Editorial Office, Frontiers Media SA, Switzerland

Copyright © 2018 Fox, Abdulla, Burdige, Lewicki and Komada. This is an open-access article distributed under the terms of the Creative Commons Attribution License (CC BY). The use, distribution or reproduction in other forums is permitted, provided the original author(s) and the copyright owner are credited and that the original publication in this journal is cited, in accordance with accepted academic practice. No use, distribution or reproduction is permitted which does not comply with these terms.

*Correspondence: Tomoko Komada, tkomada@sfsu.edu

†Present Address: Christina A. Fox, Materials Science Division, Lawrence Livermore National Laboratory, Livermore, CA, United States

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