Adams, R.S. and Bustin, R.M. (2001) The effects of surface area, grain size and mineralogy on organic matter sedimentation and preservation across the modern Squamish Delta, British Columbia: The potential role of sediment surface area in the formation of petroleum source rocks. International Journal of Coal Geology, 46, 93-112. doi:10.1016/S0166-5162(01)00019-2

has been cited by the following article:

• TITLE: Distributions of pigments in reef sediments, contribution of phytoplankton to organic matter budget in coral reef

  AUTHORS: Mohammed Rasheed, Tariq Al-Najjar, Said Damhoureyeh

  KEYWORDS: Pigment; Calcareous Sediments; Terrigenous Sediments

  JOURNAL NAME: Natural Science, Vol.3 No.5, May 17, 2011

  ABSTRACT: The temporal distributions of pigment on bio-genic calcareous and terrigenic reef sediments, chlorophyll a, chlorophyll b, chlorophyll c, fuco- xanthin, and porphine concentrations were mea- sured monthly in two sediment columns (0 - 15 cm) for one year. Pigment concentrations in-creased significantly during winter (Novem-ber-April) in both sediment types particularly in the upper layers of the sediments. Phytoplankton contributions to organic matter were found to be 8 ± 3 and 6 ± 2% in calcareous and terrigenous sediments respectively. The accumulation and the successive degradation of phytoplankton detritus to inorganic nutrients in calcareous sand may partly sustain the productivity of the coral reef communities which live in nutrient-poor environments.