T182 Novel Approaches for Constraining the Evolution of Essential Nutrient Cycling

Thursday, 29 October 2020
10:00 AM - 12:00 PM
Meeting Rooms


PRESERVATION AND POTENTIAL REMOBILIZATION OF RED TIDE TOXINS DEPOSITED IN SHALLOW SOUTHWEST FLORIDA COASTAL SEDIMENTS

Paper number: T182-7
Program: Technical Sessions
Time: 11:25 AM – 11:40 AM


Authors


Abstract

Florida red tide is a natural phenomenon caused by blooms of the dinoflagellate Karenia brevis, having been recorded by Spanish explorers as early as the 15th century. However, recently Red Tides appear to have become more frequent, intense and longer-lasting, leading to questions on potential roles of recent land development and changing water quality in bloom dynamics. Unfortunately, historic information on Red Tides is not available, and unbiased scientific data does not exist before approximately 50 years ago. Although the scientific record is short, it is possible to assess historic frequency of Red Tides by looking at chemical biomarkers (e.g., brevetoxin itself) in seafloor-sediments. This study quantifies brevetoxin in dated coastal-sediment cores to reconstruct historical Red Tide events, determine links between frequency of red tides and urbanization in Southwest Florida, and investigate whether historic blooms are related to other environmental factors. A total of 5 cores were first dated using a 210Pb-based approach, and subsamples were then solvent extracted and analyzed utilizing a GC/MS/MS for the four main analogs of brevetoxin; PbTx-1, PbTx-2, PbTx-3, and PbTx-C.A. The concentrations of toxins in the sediment cores ranged between 0.15 to 6.89 ng/g of wet sediments. The down-core variability of brevetoxin characterizes the past red tides events which is very important for tracking historical blooms utilizing the sedimentary record. This work is still in progress as dating sediment cores takes a significant length of time. The work will be finished and a paper prepared for review by the end of 2020.

Geological Society of America Abstracts with Programs. Vol. 52, No. 6

doi: 10.1130/abs/2020AM-359331

© Copyright 2020 The Geological Society of America (GSA), all rights reserved. Permission is hereby granted to the author(s) of this abstract to reproduce and distribute it freely, for noncommercial purposes. Permission is hereby granted to any individual scientist to download a single copy of this electronic file and reproduce up to 20 paper copies for noncommercial purposes advancing science and education, including classroom use, providing all reproductions include the complete content shown here, including the author information. All other forms of reproduction and/or transmittal are prohibited without written permission from GSA Copyright Permissions.