Banca de DEFESA: GABRIELLA CYNARA MINORA DA SILVA

Uma banca de DEFESA de DOUTORADO foi cadastrada pelo programa.
DISCENTE : GABRIELLA CYNARA MINORA DA SILVA
DATA : 23/02/2017
HORA: 14:30
LOCAL: Sala 05, DOL, CB
TÍTULO:

MAPPING OF SEAWEED AND SEAGRASS BEDS IN THE AREA OF ENVIRONMENTAL PRESERVATION OF REFEES OF CORAIS - RN USING GEOTECHNOLOGIES

PALAVRAS-CHAVES:

environmental management of reefs; seaweeds; geotechnologies

PÁGINAS: 130
GRANDE ÁREA: Outra
ÁREA: Ciências Ambientais
RESUMO:

Seaweeds and seagrasses associated with coral reefs comprise one of the most productive environments on the planet. Seaweeds have several roles in ecosystem services, including primary production, reef construction, facilitation of coral establishment and habitat formation for numerous other species. On the other hand, they are potentially sensitive to environmental changes, especially the impacts caused by climate change and the pressure of human activities. Because of these environmental changes, studies that can explain the impacts that these changes cause in these organisms and, thus, establish strategies for the conservation and restoration of these environments are needed. Remote sensing techniques combined with in situ observations have been widely used to map algal beds around the world. The Coral Reef Environmental Preservation Area / RN - APARC shelters a large diversity of algal species; however, although it is a conservation unit, its resources are likely to be depleted due to anthropic activities, such as tourism and fishing, and changes in global climate, such as changes in ocean temperature and acidity. In this sense, this study applied Advanced Land Observing Satellite (ALOS) satellite data, an Advanced Visible and Near Infrared Radiometer (AVNIR-2) instrument to verify the distribution of seaweeds and seagrasses in APARC, more precisely in the Maracajaú and Rio do Fogo reefs. For this, unsupervised classifications and a series of soft and hard supervised classifications were performed. Moreover, cluster analyzes were performed to verify the similarity of the benthic compositions among the studied stations in each of the reefs. Finally, the Digital Bathymetric Model (MDB) and the Digital Terrain Model (MDT) were also generated in order to understand the relationship between seaweed and seagrass establishment and development with the water depth and the slope of the reef body.The supervised classification Maxlike generated the thematic maps of both reefs. In the Maracajaú reef, the Maxlike identified seven classes: (1) Dense seaweed; (2) Sand; (3) Sparse seagrass; (4) Dense seagrass; (5) Calcareous seaweed; (6) Sparse seaweed; and (7) Fine sand. The Kappa coefficient (0.84) was considered excellent. Concerning Rio do Fogo reef, the Maxlike identified six classes: (1) Seaweed; (2) Calcareous seaweed concretions; (3) Sand; (4) Sand with limestone; (5) Seagrass; and (6) Coral Reefs. The Kappa coefficient (0.75) was considered substantial. In both reefs, seaweeds are predominantly in the central area, mainly between isobaths -1 and -3 m. This region is a relatively flat area, with a 2% slope in Maracajaú and a 3% slope in Rio do Fogo. Calcareous seaweed, forming or not concretions, are located mainly in the reef extremities, especially in the reef front, in depths of up to -5 m. Seagrasses occur mainly in the back reef, between isobaths -2 and -6 m. The edges of the reefs are the regions with the highest slopes, up to 5% in Maracajaú reef and up to 7% in Rio do Fogo reef. In both reefs, the following morphofunctional groups were recorded: foliose, leathery, corticated, articulated calcareous and crustose seaweed. This work may provide support for the planning and management of APARC, leading to the increasingly sustainable use of this conservation unit.

MEMBROS DA BANCA:
Presidente - 1279472 - ELIANE MARINHO SORIANO
Interno - 1149351 - JORGE EDUARDO LINS OLIVEIRA
Externo ao Programa - 2938129 - LAURA EMMANUELLA ALVES DOS SANTOS SANTANA DE OLIVEIRA
Externo à Instituição - MARCELLA ARAUJO DO AMARAL CARNEIRO - UNIFACEX
Externo à Instituição - RODRIGO GUIMARÃES DE CARVALHO - UERN