bioRxiv Science⌕ Search

Biology subjects

Lizcano-Sandoval, L.

Publications and source records attributed to Lizcano-Sandoval, L..

2 recordsLinked to original sources

Seagrass Extent Expansion in the Gulf of Mexico and Northwestern Caribbean (1987-2021)

Historically, the areal extent of seagrass beds in the Gulf of Mexico, Florida peninsula, and Northwestern Caribbean (Mexico and Cuba) have been estimated to cover approximately 35,510 km2. However, the absence of regular monitoring limits our ability to detect interannual variability and up-to-date health conditions, and to respond to stressors, such as degraded water quality. Seagrass areal extent is one of the core Essential Ocean variables (EOV) of the Global Ocean Observing System (GOOS). Resource managers and researchers are interested in how this seagrass extent and the distribution of this habitat changes over time to focus possible action to mitigate impacts of various stressors, such as degraded water quality. In this study, we mapped 19,405 km2 of seagrasses for the region for the period 2019-2021, using satellite imagery from Landsat 5, Landsat 7, Landsat 8, and Sentinel-2. Interannual changes in seagrass areal extent at 17 representative sites indicated that seagrass habitats increased by 12.3% between 1987 and 2021. Sites off the West Florida coast showed the highest increasing rates in seagrass extent (up to 3.1% yr-1) and lowest rate (-0.43% yr-1) was observed in Biscayne Bay, South Florida. Seagrasses in the Mexican Caribbean showed positive extent expansion rates (1.3-1.8% yr-1), while in Texas were stable over the period of study. Continuous observations of seagrasses like these help managers to understand spatial and temporal patterns of change and encourage further studies on seagrass ecology and carbon stocks.

ecology↗

Accelerated growth of the scleractinian coral Orbicella faveolata under turbid and polluted water conditions

Cartagena Bay, Colombia, experienced historical changes in water quality, mainly due to dredging and channelization of the Canal del Dique, which connects the bay with the Magdalena River. In 1981 the largest dredging events occurred in the Canal del Dique, which negatively affected the water quality in the bay. In this bay, the coral reef of Varadero depicts high coral diversity and large coral colonies, showing apparent signs of a healthy ecosystem, under highly turbid and polluted waters. Here, we evaluated the potential effects of historical water quality changes and environmental variables on the coral skeletal growth of Orbicella faveolata. We obtained coral growth information from 65 years in the period 1951-2015. Coral skeletal density was 0.73 g cm-3, linear extension 1.02 cm yr-1, and calcification 0.74 g cm-2 yr-1. After 1981, significant changes in coral growth and luminescence were found: skeletal density decreased (9.9%), linear extension increased (6.6%), and skeletal luminescence was less intense (1.6%). In overall, Atlantic Multidecadal Oscillation (AMO) data explained changes in skeletal density (8-10%) and linear extension (7-19%). Air temperature explained changes in skeletal luminescence (22-45%). Water flow of the Canal del Dique did not contribute significantly to any coral growth and luminescence variables. The growth of O. faveolata in Varadero Reef was characterized by low density skeletons and an accelerated linear extension, apparently influenced by the dredging events of 1981. Further research is required to understand coral growth responses and resilience to the conditions of high turbidity, pollution, and low light in Cartagena Bay.

ecology↗