{'fraction_non_alphanumeric': 0.021970233876683204, 'fraction_numerical': 0.020552799433026223, 'mean_word_length': 5.008510638297873, 'pattern_counts': {'":': 0, '<': 0, '<?xml version=': 0, '>': 0, 'https://': 0, 'lorem ipsum': 0, 'www.': 0, 'xml': 0}, 'pii_count': 0, 'substrings_counts': 0, 'word_list_counts': {'cursed_substrings.json': 0, 'profanity_word_list.json': 0, 'sexual_word_list.json': 0, 'zh_pornsignals.json': 0}}
Procesos de sedimentación y resuspensión en un enclave coralígeno: el caso de la vinyeta

Coralligenous concretions considered as one of the most important hot spot of species biodiversity in Mediterranean Sea. The complex structure of this biogenic rock is contributed by coralline alga and also engineer organisms. This study took place at a coralligenous concretions called Vinyeta which emerged at about 2 nautical miles from Gandía and about 17 meters deep. Sedimentation and resuspension rate were investigated at four points above this formation, and one point outside the border above the muddy sandy sediment. Although not statistically significant, the resuspension rate differed between each point, especially the one outside the assemblage. The rate oscillated between 2,05 – 26,52 g m -2 d -1 on coralligenous assemblage, whereas on the muddy sandy sediment the value reach 17,01 – 708,94 g m -2 d -1 . Furthermore, the deposition of sediment outside the border of corraligenous assemblage could be more easily influenced by hydrodynamic and meteorological condition compare to others. Due to its rugosity, coralligenous habitat could retain 1,5–3,6 kg m -2 year -1 of sediment which later would become a part of this biogenic rock. The result of the study also indicated that there were higher organic fractions in settleable material than in resuspended material from their chlorophyll a content.