2015
DOI: 10.1002/rcm.7435
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Water cycle and salinity dynamics in the mangrove forests of Europa and Juan de Nova Islands, southwest Indian Ocean

Abstract: On the drier Europa Island, the salinity of all the water points is equal to or higher than that of the seawater, and on Juan de Nova the groundwater salinity is lower (5 to 20 PSU). This preliminary study shows that the karstic pothole mangroves exist due to the sea connection through the fractured coral and the high tidal dynamics.

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Cited by 11 publications
(8 citation statements)
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“…Tropical coastal areas are typically characterized by rain water with δ 18 O of about -3 ± 1 ‰ (GNIP database) and the groundwater of several tropical coasts and islands reflect similar mean δ 18 O values (Lambs et al, 2016(Lambs et al, , 2018. This is also the case for the west coast of South India, with similar groundwater stable isotope ratios at Udupi (δ 18 O = -3.09 ± 0.05 ‰, n=34; Tripti et al, 2016).…”
Section: Rainfall Amount Effectmentioning
confidence: 61%
“…Tropical coastal areas are typically characterized by rain water with δ 18 O of about -3 ± 1 ‰ (GNIP database) and the groundwater of several tropical coasts and islands reflect similar mean δ 18 O values (Lambs et al, 2016(Lambs et al, , 2018. This is also the case for the west coast of South India, with similar groundwater stable isotope ratios at Udupi (δ 18 O = -3.09 ± 0.05 ‰, n=34; Tripti et al, 2016).…”
Section: Rainfall Amount Effectmentioning
confidence: 61%
“…A narrow and shallow lagoon of about 7 km 2 extends far inland and opens to the sea over the northern reef flat ([ 41 ], Fig 1 ). Saltwater mangrove formations dominate the lagoon’s shoreline [ 42 ], while sandy beaches occur along its western shore.…”
Section: Methodsmentioning
confidence: 99%
“…However, foliar δ 15 N signature of the non-mangroves showed that they relied mostly on naturally originated N sources. Even though both mangroves and non-mangroves can use different sources of N from precipitation along with soil solution depending on micrometeorological conditions on sites [73][74][75][76][77], mangroves are capable of using alternate nutrient sources of groundwater, river water, and tidal seawater [78,79] accordingly due to their unique root systems, distribution along the water vicinity of the rivers, and salt-tolerant plant physiology. Despite being tactful to relatively higher N availability on human-affected sites, the non-mangroves showed negative to nearly zero values of foliar δ 15 N values.…”
Section: Foliar δ 15 N Of Mangroves and Non-mangroves Under Anthropogmentioning
confidence: 99%