2018
DOI: 10.3390/rs10111787
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Does Sea Surface Temperature Contribute to Determining Range Limits and Expansion of Mangroves in Eastern South America (Brazil)?

Abstract: Low Sea Surface Temperature (SST) is a climate barrier because it may inhibit and reduce seedling growth of mangrove propagules upon dispersal through seawater. Our objective is to analyze the spatio-temporal series of daily SST data from the Multi-scale Ultra-high Resolution (MUR)-SST in order to identify the occurrence of chilling events for mangrove plants at the Eastern South America mangrove limit and beyond. We focus our study on three key sites: (i) the Rhizophora mangle L. distribution limit (Praia do … Show more

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Cited by 27 publications
(22 citation statements)
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“…The latitude of mangrove range limits varies strongly among regions and has been associated with climatic factors (Quisthoudt et al , ; Osland et al , ; Cavanaugh et al , ), geomorphological characteristics (Ellison, ), as well as oceanographic conditions and factors such as dispersal limitation (Soares et al , ) or combinations of these (e.g. Ximenes et al , ).…”
Section: Introductionmentioning
confidence: 99%
“…The latitude of mangrove range limits varies strongly among regions and has been associated with climatic factors (Quisthoudt et al , ; Osland et al , ; Cavanaugh et al , ), geomorphological characteristics (Ellison, ), as well as oceanographic conditions and factors such as dispersal limitation (Soares et al , ) or combinations of these (e.g. Ximenes et al , ).…”
Section: Introductionmentioning
confidence: 99%
“…S3, PAR caused the most significant effect on LUE, which is consistent with previous studies 14,30,32 . The impact of SST has not been quantitatively assessed, however, SST is a critical control that determines the upper latitudinal range of mangrove ecosystems 12,33 . In our study, the effects of SST and salinity on the mangrove LUE were quantified and helped improve LUE modeling.…”
Section: Discussionmentioning
confidence: 99%
“…S3) indicated that salinity and SST have little influence on mangrove productivity 51 . To date, the quantitative impact of SST has not been comprehensively unfolded, but it is a global control that determines the upper limit of the latitudinal range of mangroves 12,33 . The weak relationships between salinity, SST, and mangrove GPP could be due to the uncertainty caused by tidal inundation.…”
Section: Discussionmentioning
confidence: 99%
“…Precipitation is another pivotal factor, especially important for mangrove trees, which develop better in areas with precipitation above 1,500 mm yr –1 and reach their maximum in areas receiving more than 2,500 mm yr –1 ( Schaeffer-Novelli et al, 1990 ). Nevertheless, southern mangroves are usually composed of shorter trees and less structurally complex mangrove swamps ( Lana et al, 2001 ), due to lower sea surface temperature ( Ximenes et al, 2018 ). Our data indicate that the microbial community responded similarly, as samples from the south (PAR-S and GUA-S) consisted in less diverse and complex microbial communities.…”
Section: Discussionmentioning
confidence: 99%