Temporal variability in the biochemical composition of sedimentary organic matter in an intertidal flat of the Galician coast (NW Spain) |
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| Institution: | 1. Conservation Science, Royal Botanic Gardens, Kew, Richmond, Surrey, TW9 3AE, UK;2. Biodiversity Informatics and Spatial Analysis, Royal Botanic Gardens, Kew, Richmond, Surrey, TW9 3AE, UK;1. Department of Cardiovascular Medicine, Asyut University Hospital, Asyut, aEgypt;2. Department of Cardiovascular Medicine, Kokura Memorial Hospital, Kitakyushu, bJapan;1. Department of Cardiology, SVIMS, Tirupati, Andhra Pradesh;1. Sudan Heart Institute, Khartoum, Sudan;2. King Abdulaziz Cardiac Center, Riyadh, Saudi Arabia;1. Catheterization Laboratory and Cardiovascular Interventional Unit, Department of Clinical and Experimental Medicine, University of Catania, Catania, Italy;2. Faculty of Medicine of Tunis, University Tunis El Manar, Tunis, Tunisia |
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| Abstract: | Temporal variations and spatial distribution of sedimentary organic matter composition were investigated over a one year period in an intertidal flat of the NW Spain. Sediment samples were collected from 0 to 25 cm depth, every three months, from January 1997 to January 1998 at three tidal levels (high, medium and low). Changes in the elemental and biochemical composition were assessed to gather information on temporal and spatial fluctuations in quantity and quality of sedimentary organic matter potentially available to benthic deposit-feeder nutrition. Organic matter content was significantly higher at the medium tidal level, while minimum values were found at the high tidal level. The different biochemical classes of organic compounds exhibited different temporal patterns. Carbohydrate and lipid concentrations decreased with sediment depth. The biopolymeric fraction of organic carbon (i.e. the sum of lipid, carbohydrate and protein carbon) was dominated by proteins (61%), followed by lipids (26%) and carbohydrates (14%). Biopolymeric carbon accounted for only a small fraction (37% on average) of the total organic carbon. Refractory organic carbon (i.e. non biopolymeric) accounted for 50 to 80% of the total organic carbon and it tended to be buried into deeper sediment layers. The nutritional quality of the sedimentary organic matter, expressed as the biopolymeric carbon to total organic carbon ratio, was higher in January 1997, when also the higher protein to carbohydrate ratio values were observed and related to the presence of newly-produced organic matter. Low biopolymeric carbon to total organic carbon ratio and protein to carbohydrate ratio were recorded during the rest of the year, indicating a low-quality and aged organic matter. Results of the present study revealed an inverse relationship between the overall amount of organic matter and its potential availability to consumers. |
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