2008
DOI: 10.1016/j.csr.2008.09.005
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Principal component analysis (PCA) and mineral associations of litoraneous facies of continental shelf carbonates from northeastern Brazil

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Cited by 16 publications
(11 citation statements)
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“…In both sampling campaigns, the highest levels of OM occurred in the mid-estuary (P4-P7). However, all along the JPE, OM levels were within the range expected for tropical estuaries from northeastern Brazil (0.76-38.9%) (Freire et al, 2004;Lacerda and Marins, 2005;Marques et al, 2008;Nascimento et al, 2010). The distribution of OM in the sediments presented a pattern similar to that exhibited by the fine sediments, a finding which reinforces the possibility that the lower and mid-estuarine zones are depositional areas.…”
Section: Sediment Propertiessupporting
confidence: 71%
“…In both sampling campaigns, the highest levels of OM occurred in the mid-estuary (P4-P7). However, all along the JPE, OM levels were within the range expected for tropical estuaries from northeastern Brazil (0.76-38.9%) (Freire et al, 2004;Lacerda and Marins, 2005;Marques et al, 2008;Nascimento et al, 2010). The distribution of OM in the sediments presented a pattern similar to that exhibited by the fine sediments, a finding which reinforces the possibility that the lower and mid-estuarine zones are depositional areas.…”
Section: Sediment Propertiessupporting
confidence: 71%
“…Calcium carbonates and organic matter levels presented high levels at the deeper stations, especially in sheltered areas, which can be associated with the deposition in both harbors induced by the jetty. These results corroborate the characteristic of sediments from terrigenous facies of this region (Freire et al 2004;Marques et al 2008). The sediments collected in navigation channel of Port of Santos presented a predominance of very fine sands, with increasing fine particles (coarse silt) towards the inner estuary not considering the predominance of fine particles in S1.…”
Section: Resultssupporting
confidence: 79%
“…The climate in coastal zone of Brazilian semi-arid is influenced by the Intertropical Convergence Zone (ITCZ) conditions, with average temperatures ranging from 24°C to 30°C and the predominance of trade winds blowing from the E-SE, controlling thus the sediment transport in the region (Maia et al, 1998;Paula et al, 2013). The sedimentology of Ceará coast is characterized by organogenic facies with elevated deposition of calcium carbonate from calcareous algae and terrigenous facies marked by clastic rocks and clay (Lacerda & Marins, 2006;Marques et al, 2008). A predominance of coarser sediments is found in the outer shelf contrasting with sandy particles with low amounts of mud that cover the inner shelf (Freire et al, 2004).…”
Section: Study Area and Sediment Samplingmentioning
confidence: 99%