21 research outputs found

    Coral Gardens Reef, Belize: An \u3ci\u3eAcropora\u3c/i\u3e spp. Refugium under Threat in a Warming World

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    Live coral cover has declined precipitously on Caribbean reefs in recent decades. Acropora cervicornis coral has been particularly decimated, and few Western Atlantic Acropora spp. refugia remain. Coral Gardens, Belize, was identified in 2020 as a long-term refugium for this species. This study assesses changes in live A. cervicornis coral abundance over time at Coral Gardens to monitor the stability of A. cervicornis corals, and to explore potential threats to this important refugium. Live coral cover was documented annually from 2012– 2019 along five permanent transects. In situ sea-surface temperature data were collected at Coral Gardens throughout the study period and compared with calibrated satellite data to calculate Maximum Monthly Mean (MMM) temperatures and Degree Heating Weeks (DHW). Data on bathymetry, sediment, substrate, herbivore abundance, and macroalgal abundance were collected in 2014 and 2019 to assess potential threats to Coral Gardens. Live coral cover declined at all five transect sites over the study period. The greatest loss of live coral occurred between 2016 and 2017, coincident with the earliest and highest maxi- mum average temperatures recorded at the study site, and the passage of a hurricane in 2016. Structural storm damage was not observed at Coral Gardens, though live coral cover declined after the passage of the storm. Uranium-thorium (230Th) dating of 26 dead in situ fragments of A. cervicornis collected in 2015 from Coral Gardens revealed no correlation between coral mortality and tropical storms and hurricanes in the recent past. Our data suggest that several other common drivers for coral decline (i.e. herbivory, predation, sedimentation, pH) may likely be ruled out for Coral Gardens. At the end of the study period, Coral Gardens satisfied most criteria for refugium status. However, the early onset, higher mean, and longer duration of above-average temperatures, as well as intermittent temperature anomalies likely played a critical role in the stability of this refugium. We suggest that temperature stress in 2016 and perhaps 2015 may have increased coral tissue vulnerability at Coral Gardens to a passing hurricane, threatening the status of this unique refugium

    Geologic Analyses for Evaluating Watershed Heterogeneity: Implications for Otolith Chemistry Studies

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    Abstract: Studies using otolith chemistry to distinguish fish stocks in fresh waters have suggested that spatial heterogeneity in basin geology determines the scale of stock discrimination possible with this approach. However, no studies have illustrated an association between spatial variation in fish otolith chemistry and watershed geology. We consider this relationship in the context of a recent study describing within-and between-river variation in trace element chemistry of otoliths from YOY smallmouth bass (Micropterus dolomieu) from the Maury and James rivers (Virginia). Cluster analysis of multivariate geologic data for discrete river segment basins illustrates a phenomenological association between geologic heterogeneity and our ability to discriminate spatial groupings of fish from their otolith chemistry. This analysis provides two significant results: 1) a starting point for considering the mechanistic relationship between watershed geology and fish otolith chemistry; and, 2) a framework for assessing basin heterogeneity prior to designing studies that use otolith chemistry to distinguish fish stocks in river-tributary networks. The latter can be used a priori to determine the efficacy of otolith chemistry comparisons and to guide sample collection over large spatial areas. In approximately the last decade, significant advances were made in analysis of fish "hard parts" (e.g., bones, scales, and spines) as records of water chemistry in areas inhabited by fish during their lifetimes Our objective in this paper is to determine if differences in basin geology correspond with successful discrimination of fish origins in a recent study of otolith chemistry in riverine smallmouth bass (Micropterus dolomieu) populations. Trace element concentrations were used to successfully discriminate natal origins of age-0 smallmouth bass spawned in the James River or its tributary Maury River. The analysis was further able to differentiate among fish collected from different segments of the Maury River based on otolith chemistry. Here we compare the spatial resolution of fish origin discrimination in this previous study (summarized below for context) with patterns of land attribute variation across the study area as a first-order attempt to illustrate an association between otolith chemistry and basin geology. Using readily available spatial data analyzed in a GIS, we present a framework for characterizing geology of river segment basins and for quantifying dissimilarity among basins in the study area. We then use cluster analysis to group segment basins with similar geologic compositions, and compare results of clustering with our ability to distinguish fish origins among basins by otolith chemistry. We discuss our results in the context of applying these methods to guide experimental design and collection effort in future studies of otolith chemistry in river systems. Study Area and Otolith Chemistry Study The James River is a large (fifth order) river that runs from the Ridge and Valley physiographic province through the Coastal Plain. The Maury River is a smaller (fourth order) river that originates in the Ridge and Valley and terminates in the James River at the edge of the Blue Ridge province. The James River and its 13
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