What is it about?
This study examines the impact of physical and chemical oceanographic forces on the sedimentology and geomorphology of nearshore carbonate ramps. By combining field measurements, remote sensing data, and hydrodynamic modeling, the research investigates how oceanographic processes shape the distribution and characteristics of sediments in the modern northeastern Yucatán Shelf, Mexico. The study emphasizes the role of hydrodynamics, upwelling, and nutrient levels in influencing the variability of nearshore carbonate ramp environments.
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Why is it important?
Understanding the relationship between oceanographic processes and carbonate ramp geology is crucial for deciphering sedimentary patterns and reconstructing ancient environments. Carbonate ramps are common features in the geological record, but their facies patterns and sedimentary dynamics are less well understood compared to other carbonate systems. This study provides valuable insights into the complex interactions of physical, chemical, and biological processes on nearshore carbonate ramps, contributing to improved models for both modern and ancient ramp systems.
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This page is a summary of: Hydrodynamic influences on sedimentology and geomorphology of nearshore parts of carbonate ramps: Holocene, NE Yucatán Shelf, Mexico, Journal of Sedimentary Research, October 2021, Society for Sedimentary Geology,
DOI: 10.2110/jsr.2020.103.
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