Restricted terrestrial carbon input to the continental shelf during Cyclone Winifred: implications for terrestrial runoff to the Great Barrier Reef Province-Reference-Cited by-同舟云学术

Restricted terrestrial carbon input to the continental shelf during Cyclone Winifred: implications for terrestrial runoff to the Great Barrier Reef Province

Published:1987-10 Issue:2 Volume:6 Page:113-119
ISSN:0722-4028
Container-title:Coral Reefs
language:en
Short-container-title:Coral Reefs

Author:

Gagan Michael K.,Sandstrom Mark W.,Chivas Allan R.

Publisher

Springer Science and Business Media LLC

Subject

Aquatic Science

Link

http://link.springer.com/content/pdf/10.1007/BF00301380.pdf

Reference21 articles.

1. Boto K, Isdale P (1985) Fluorescent bands in massive corals result from terrestrial fulvic acid inputs to nearshore zone. Nature 315:396?397

2. Davies PJ, Hughes H (1983) High-energy reef and terrigenous sedimentation, Boulder Reef, Great Barrier Reef. BMR J Aust Geol Geophys 8:201?209

3. Degens ET (1969) Biogeochemistry of stable carbon isotopes. In: Eglington G, Murphy MTJ (eds) Organic geochemistry. Springer, Berlin Heidelberg New York, pp 304?328

4. Done TJ (1982) Patterns in the distribution of coral communities across the Central Great Barrier Reef. Coral Reefs 1:95?107

5. Frazer JW (1962) Simultaneous determination of carbon, hydrogen, and nitrogen. Part II. An improved method for solid organic components. Mikrochim Acta 1962:993?999

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