1996
DOI: 10.1016/0341-8162(96)00013-6
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Mangroves as indicators of coastal change

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Cited by 258 publications
(168 citation statements)
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References 24 publications
(22 reference statements)
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“…Kakenauwe is the only transect that contains a large number of the species Sonneratia, which is to be found at the front of the Rhizophora stand, in line with the zonations suggested by Blasco ( 1996) and Woodroffe (2000) and hence justifying its inclusion so that all the suggested dominant mangrove species are present in the regional dataset. Grindrod ( 1988) states that Northern Australia mangroves are dominated by Rhizophora, Ceriops and Bruguiera, in line with the major species present in the transects studied.…”
Section: Ceriops Lumnitzerasupporting
confidence: 66%
See 1 more Smart Citation
“…Kakenauwe is the only transect that contains a large number of the species Sonneratia, which is to be found at the front of the Rhizophora stand, in line with the zonations suggested by Blasco ( 1996) and Woodroffe (2000) and hence justifying its inclusion so that all the suggested dominant mangrove species are present in the regional dataset. Grindrod ( 1988) states that Northern Australia mangroves are dominated by Rhizophora, Ceriops and Bruguiera, in line with the major species present in the transects studied.…”
Section: Ceriops Lumnitzerasupporting
confidence: 66%
“…Blasco ( 1996) suggests that eastern hemisphere mangroves all occupy a broadly similar pattern of zonation moving seaward to landward of Rhizophora (though Sonneratia and…”
Section: The Relationship Between Pollen and The Environmental Variabmentioning
confidence: 99%
“…The highest percentage of Rhizophoraceae, between 8,500 and 7,500 years BP, was related to the start of the Godavari delta development between 8,400-8,000 cal years BP (Rao et al, 2012). According to Blasco et al (1996), at geological time scales, mangrove expansion is mainly a function of sea level dynamics rather than rainfall variations, even if this ecological community also needs strong fluvial inputs. This seems to be particularly the case of the mangrove increase during the 8,400 and 8,000cal years BP interval when the North Atlantic 8.2 ka cold event should have led to a southward migration of the ITCZ, and consequently a reduction in the Indian monsoon (Dixit et al, 2014).…”
Section: Orbital and Millennial-scale Variability Of The Indian Monsomentioning
confidence: 99%
“…Mangroves are the trees most capable of tolerating saline conditions in tropical and subtropical intertidal areas (McKee 1995, Blasco et al 1996, Saenger 2002, Spalding et al 2010. Mangrove forests are important because they have the ability to improve ecological aspects such as organic carbon dynamics (Flores-Verdugo et al 1987, Bashan and Holguin 2002, Kristensen et al 2008) and primary productivity (Holguin et al 2001, Dittmar et al 2006, and they provide protection against hurricanes and tropical storms (Raven et al 1992, Gilman et al 2008, Komiyama et al 2008.…”
Section: Introductionmentioning
confidence: 99%