Dynamics of soil properties in forests of Rhizophora mangle L. (Rhizophoraceae) in Margarita Island, Venezuela. Biochemical and microbiological properties of soils can provide information related to ecosystems environmental status. With the aim to determine the response of microbial biomass, and enzymatic and microbial activity in hypersaline (IS≥55ups) and saline (IS<55ups) mangrove soils exposed to interstitial salinities (IS) greater than 36ups, these properties were measured in mono-specific forests of Rhizophora mangle at Laguna de la Restinga National Park (Margarita Island, Venezuela). During three seasons (dry, wet and transition), a total of 120 soil samples were collected from ten (5 hypersaline and 5 saline) randomly-selected sites of 1000m 2 each. Four soil samples (400-500g) per plot were randomly collected with a corer at a depth of 10cm using a 1m 2 quadrat; each sample consisted in the combination of 8 sub-samples (50-60g ea.). Physical, chemical, enzymatic, biochemical and microbiological properties of soil samples were determined using standard laboratory protocols. The response of microbial biomass and microbial and enzymatic activity was analyzed taking into account spatial and climatic factors and interstitial salinity. Microbial biomass was linked to each locality conditions, and was not sensitive to seasonal or salinity differences. Microbial activity remained functionally active during the study period and presented variable responses. Dehydrogenase activity proved to be a good indicator for flooded and anoxic environments, and arginine ammonification resulted to be the more sensitive microbial activity to changes in salinity. Regarding enzyme activities, spatial variability was the most widespread response. We did not find a unique general pattern between enzymatic activities and spatio-temporal variation; and only the enzyme phosphatase was negatively affected by salinity. We conclude that microbial populations of mangrove soils and their activities have functional adaptations to flooded and highly-saline environments typical of a negative estuary, subjected to drastic changes due to weather and water dynamics. Future studies are needed to determine the relation between the "health" of mangrove forest and microbial populations, and their activities in mangroves soils.
Palaeoenvironments of Rhizophora mangle (Rhizophoraceae) in Castilletes, Alta Guajira, Venezuela according to paleoconchas of Crassostrea rhizophorae (Ostreoida: Ostreidae). Shell middens are a very characteristic feature of coastal human adaptations. Component and variability analysis offer clues to subsistence of ancient human populations, formation processes and information of environmental changes.In this study, we tested the use of paleoshells found in shell midden to infer paleoenviroment conditions of R. mangle forest. We presented data of paleoshells from shell middens, located on Castilletes-Alta Guajira, Venezuela, dated from 3 580 ± 30 años B.P years, and we included data of actual shells from mangrove forests located on Cocinetas laggon (Castilletes) and Maracas Island (Maracaibo lagoon). We examined 185 samples of fixing traces marked by mangrove roots on paleoshells (n = 109) and actual shells (n = 76) of C. rhizophorae. Subsequently, we estimated paleoroot and modern root diameter using a geometric model using shell´s trace. To validate this model, we directly measured modern roots. Furthermore, a physiognomic study was made in both sites to associate mangrove forest with roots diameter and shells information. Results showed that there were no significant differences between estimated root diameter values obtained from traces of modern shells and the ones recorded by direct measurement of roots (Castilletes P = 0.160854; Maracas P = 0.617271); allowing the use of geometric model to obtain estimated values of paleoroots. Shell measurements showed that paleoshells were larger than modern shells. Paleoroot diameters showed no significant differences with modern Castilletes's mangrove roots (exposed zone) (P = 0.303518), contrasting with Maracas´s roots (protected zone) (P = 0.017771). Physiognomic study showed that modern Castilletes forests had diameter at breast height (DBH) and tree height (11.10 m and 4.90 m, respectively) lower than Maracas (34.86 cm and 10.62 m), responding to the wind exposure and salinity. Diameters and quantity of roots per tree were higher in Castilletes (3.01 cm y 11 roots/tree) than Maracas (2.39 cm y 7 roots/tree). We determined that paleoforests and modern forests from Castilletes have similar characteristics associated to arid environment with stronger wind exposition. We concluded that paleoshells trace analysis is a low cost and novel method that allows obtaining information about paleoenvironment of R. mangle forests. Rev. Biol. Trop. 63 (4): 1223-1233. Epub 2015 December 01.
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