Matches in SemOpenAlex for { <https://semopenalex.org/work/W4225409181> ?p ?o ?g. }
- W4225409181 abstract "Mangrove vegetation is strongly dependent on the climate, the physicochemical variables of the sediment, and the hydrological dynamics. These drivers regulate the distribution of different mangrove ecotypes and their ecosystem services, so the net sediment accumulation rates in different mangrove ecotypes in Celestun Lagoon, a karstic zone in the NW Yucatan Peninsula, SE Mexico, were estimated. The measurements considering mangrove ecotypes and their spatial variability concerning the lagoon's salinity gradient (inner, middle, and outer lagoon zones) in three climate seasons (dry, rain, and “nortes”) were realized. We registered the structural variables of the forest, interstitial water physicochemical characteristics, and sediment variables that could influence the net sediment deposition. Fringe mangroves are exposed to low hydrodynamism and show the highest sedimentation rate (3.37 ± 0.49 kg m −2 year −1 ) compared to basin (1.68 ± 0.22 kg m −2 year −1 ), dwarf (1.27 ± 0.27 kg m −2 year −1 ), and “peten” (0.52 ± 0.12 kg m −2 year −1 ) mangroves. The highest sedimentation rate was recorded in the rainy season (0.24 ± 0.08 kg m −2 month −1 ), while spatially, the highest value was registered in the outer zone (0.44 ± 0.09 kg m −2 month −1 ). If the extension of each mangrove ecotype is considered, dwarf mangroves have the highest annual sediment accumulation (1,465 t year −1 in 14,706 ha). The structural, physicochemical, and sediment variables of the sites by mangrove ecotype show that dwarf mangroves represent a distinct group from those formed by fringe, basin, and peten mangroves. However, the sedimentation is high in fringe mangroves at the front of the lagoon and diminishes inland where peten mangroves exist. The differences are given by tree density, but salinity, as a proxy variable of the freshwater influence, significantly influences the sedimentation rate. These results indicate that mangroves in karstic environments can have critical roles in confronting climate change, considering water and sediment flows are the basis of sediment accumulation. According to their hydrogeomorphological drivers, conserving, managing, and restoring the mosaic of mangrove ecotypes improves ecosystem services, including mitigation and adaptation to climate change." @default.
- W4225409181 created "2022-05-05" @default.
- W4225409181 creator A5052331032 @default.
- W4225409181 creator A5073489538 @default.
- W4225409181 creator A5075822250 @default.
- W4225409181 date "2022-05-04" @default.
- W4225409181 modified "2023-10-09" @default.
- W4225409181 title "Sedimentation as a Support Ecosystem Service in Different Ecological Types of Mangroves" @default.
- W4225409181 cites W1494431475 @default.
- W4225409181 cites W156610508 @default.
- W4225409181 cites W1895106052 @default.
- W4225409181 cites W1929181818 @default.
- W4225409181 cites W1964756163 @default.
- W4225409181 cites W1973438679 @default.
- W4225409181 cites W1978987129 @default.
- W4225409181 cites W1983768083 @default.
- W4225409181 cites W1990291281 @default.
- W4225409181 cites W1991686145 @default.
- W4225409181 cites W2032305662 @default.
- W4225409181 cites W2041319167 @default.
- W4225409181 cites W2041828289 @default.
- W4225409181 cites W2068061233 @default.
- W4225409181 cites W2078069214 @default.
- W4225409181 cites W2095240796 @default.
- W4225409181 cites W2099054953 @default.
- W4225409181 cites W2109884042 @default.
- W4225409181 cites W2116473628 @default.
- W4225409181 cites W2149269960 @default.
- W4225409181 cites W2149598174 @default.
- W4225409181 cites W2154282766 @default.
- W4225409181 cites W2154998026 @default.
- W4225409181 cites W2162040657 @default.
- W4225409181 cites W2170127820 @default.
- W4225409181 cites W2222223744 @default.
- W4225409181 cites W2479753188 @default.
- W4225409181 cites W2546570948 @default.
- W4225409181 cites W26050582 @default.
- W4225409181 cites W2625084306 @default.
- W4225409181 cites W2747875404 @default.
- W4225409181 cites W2771317050 @default.
- W4225409181 cites W2892817268 @default.
- W4225409181 cites W2905441664 @default.
- W4225409181 cites W2913089583 @default.
- W4225409181 cites W3018625857 @default.
- W4225409181 cites W3048612570 @default.
- W4225409181 cites W3091582083 @default.
- W4225409181 cites W3122853200 @default.
- W4225409181 cites W3124863932 @default.
- W4225409181 cites W3133211856 @default.
- W4225409181 doi "https://doi.org/10.3389/ffgc.2022.733820" @default.
- W4225409181 hasPublicationYear "2022" @default.
- W4225409181 type Work @default.
- W4225409181 citedByCount "4" @default.
- W4225409181 countsByYear W42254091812022 @default.
- W4225409181 countsByYear W42254091812023 @default.
- W4225409181 crossrefType "journal-article" @default.
- W4225409181 hasAuthorship W4225409181A5052331032 @default.
- W4225409181 hasAuthorship W4225409181A5073489538 @default.
- W4225409181 hasAuthorship W4225409181A5075822250 @default.
- W4225409181 hasBestOaLocation W42254091811 @default.
- W4225409181 hasConcept C100970517 @default.
- W4225409181 hasConcept C10860467 @default.
- W4225409181 hasConcept C110872660 @default.
- W4225409181 hasConcept C114793014 @default.
- W4225409181 hasConcept C127313418 @default.
- W4225409181 hasConcept C129513315 @default.
- W4225409181 hasConcept C187320778 @default.
- W4225409181 hasConcept C18903297 @default.
- W4225409181 hasConcept C205649164 @default.
- W4225409181 hasConcept C2816523 @default.
- W4225409181 hasConcept C29941650 @default.
- W4225409181 hasConcept C39432304 @default.
- W4225409181 hasConcept C68874143 @default.
- W4225409181 hasConcept C76886044 @default.
- W4225409181 hasConcept C86803240 @default.
- W4225409181 hasConceptScore W4225409181C100970517 @default.
- W4225409181 hasConceptScore W4225409181C10860467 @default.
- W4225409181 hasConceptScore W4225409181C110872660 @default.
- W4225409181 hasConceptScore W4225409181C114793014 @default.
- W4225409181 hasConceptScore W4225409181C127313418 @default.
- W4225409181 hasConceptScore W4225409181C129513315 @default.
- W4225409181 hasConceptScore W4225409181C187320778 @default.
- W4225409181 hasConceptScore W4225409181C18903297 @default.
- W4225409181 hasConceptScore W4225409181C205649164 @default.
- W4225409181 hasConceptScore W4225409181C2816523 @default.
- W4225409181 hasConceptScore W4225409181C29941650 @default.
- W4225409181 hasConceptScore W4225409181C39432304 @default.
- W4225409181 hasConceptScore W4225409181C68874143 @default.
- W4225409181 hasConceptScore W4225409181C76886044 @default.
- W4225409181 hasConceptScore W4225409181C86803240 @default.
- W4225409181 hasFunder F4320321739 @default.
- W4225409181 hasLocation W42254091811 @default.
- W4225409181 hasOpenAccess W4225409181 @default.
- W4225409181 hasPrimaryLocation W42254091811 @default.
- W4225409181 hasRelatedWork W1556044011 @default.
- W4225409181 hasRelatedWork W1983027832 @default.
- W4225409181 hasRelatedWork W2294041471 @default.
- W4225409181 hasRelatedWork W2331071324 @default.
- W4225409181 hasRelatedWork W2351447334 @default.
- W4225409181 hasRelatedWork W2357096884 @default.