Lignin phenol-based evidence of rapid 8 cm sediment deposition from a hurricane flooding event in continental margin San Blas Basin, Mexico

Emmet Bush1, Jacquelyn A Neibauer1, Garrett A. Raemhild1, Loic J. B. Barbara2, Megan Duffy1, Jamee Adams3, Khadijah K. Homolka4, Jose D. Carriquiry2 and Richard G Keil1, (1)University of Washington, School of Oceanography, Seattle, WA, United States, (2)Autonomous University of Baja California, Ensenada, BJ, Mexico, (3)Scripps Institution of Oceanography, La Jolla, United States, (4)University of Washington, School of Oceanography, Seattle, United States
Abstract:
A 45 cm sediment core from San Blas Basin on the continental shelf of pacific Mexico, 50 km off the coast and north-west of Puerto Vallarta, was taken and analysed for lignin, a biomarker for terrestrial organic matter (TOM). The total amount of lignin phenols ranges between 1.5 to 4.5 mg lignin phenol/10 g sediment except for an order of magnitude increase between 18 cm and 26 cm which was 20 to 40 mg lignin phenol/10g sediment. Acid to aldehyde ratios of vanillin-type lignin (Ad/Al (v)), a proxy for degradation, had a range of 0.36 to 0.58 while the section between 18 cm to 26 cm was fresher with a range of 0.26 to 0.28. S/V to C/V analysis indicated that the lignin is sourced from angiosperms. The section between 18 cm to 26 cm had statistically similar values ranging between S/V of 0.85 to 0.95 and C/V of 0.19 to 0.21. S/V to Ad/Al (v) analysis had a negative slope indicating S-type lignin is preferentially degraded and the background lignin signal could look more like the fresher 18-26 cm section if degradation had not occurred. We conclude a large hurricane flooding event brought fresh TOM off of the land and the sediment deposition between 18 to 26 cm was deposited in one event due to the S/V and C/V values overlapping.