Aquatic Sciences

, Volume 77, Issue 2, pp 271–291

Environmental assessment of vegetation and hydrological conditions in Everglades freshwater marshes using multiple geochemical proxies

Research Article

DOI: 10.1007/s00027-014-0385-0

Cite this article as:
Saunders, C.J., Gao, M. & Jaffé, R. Aquat Sci (2015) 77: 271. doi:10.1007/s00027-014-0385-0


Paleoecological reconstructions of environmental changes provide important information for Everglades restoration targets. Traditionally this has been achieved using a combination of biological and physical indicators. However, as microfossils may be sporadically abundant in Everglades soils, organic geochemical methods can provide information at the molecular level. To reconstruct vegetation trends over the last century, soil cores from Shark to Taylor Sloughs, the primary flowpaths of the southern Everglades, were examined using several geochemical proxies. The n-alkane derived biomarker Paq effectively distinguished organic inputs from sawgrass and slough habitats. Other proxies examined include Kaurenes, cyclic diterpenoids unique to sawgrass roots; biomarkers of algae (highly branched isoprenoids (C20HBIs) and Botryococcenes); lignin phenols as vascular plant indicators; and macrofossils. At all sites, soil profiles from sawgrass marshes showed vegetation had shifted over the last 100 years, from sloughs to sawgrass-dominated marshes, reflecting decreased water levels (shorter hydroperiods) induced by water management. Paleo-assessments of modern sloughs, however, indicate these habitats remained deeper water habitats throughout the period of record, though shifts toward shorter hydroperiod vegetation were observed. In Taylor Slough, evidence of increasingly dry conditions in sloughs was confirmed by seed inputs from woody species. At 3 of the 5 sites, recent increases in C20HBIs and Botryococcene concentrations indicated greater periphyton abundance, coincidental with increased mineral concentrations observed in surface waters during the mid-20th Century. Bulk proxies such as organic content and carbon:nitrogen ratios also supported findings of changes in relative contributions of microbial and higher plants in this ecosystem.


Everglades Molecular Biomarkers Macrofossils Paleoecology Hydrology 

Supplementary material

27_2014_385_MOESM1_ESM.pdf (1.6 mb)
Supplementary material 1 (PDF 1618 kb)
27_2014_385_MOESM2_ESM.pdf (80 kb)
Supplementary material 2 (PDF 79 kb)
27_2014_385_MOESM3_ESM.pdf (98 kb)
Supplementary material 3 (PDF 97 kb)
27_2014_385_MOESM4_ESM.pdf (107 kb)
Supplementary material 4 (PDF 106 kb)
27_2014_385_MOESM5_ESM.pdf (94 kb)
Supplementary material 5 (PDF 94 kb)
27_2014_385_MOESM6_ESM.pdf (224 kb)
Supplementary material 6 (PDF 223 kb)
27_2014_385_MOESM7_ESM.pdf (88 kb)
Supplementary material 7 (PDF 87 kb)
27_2014_385_MOESM8_ESM.pdf (33 kb)
Supplementary material 8 (PDF 33 kb)
27_2014_385_MOESM9_ESM.pdf (129 kb)
Supplementary material 9 (PDF 129 kb)
27_2014_385_MOESM10_ESM.pdf (85 kb)
Supplementary material 10 (PDF 84 kb)
27_2014_385_MOESM11_ESM.pdf (82 kb)
Supplementary material 11 (PDF 82 kb)
27_2014_385_MOESM12_ESM.pdf (349 kb)
Supplementary material 12 (PDF 349 kb)

Copyright information

© Springer Basel 2014

Authors and Affiliations

  1. 1.Everglades Systems AssessmentSouth Florida Water Management DistrictWest Palm BeachUSA
  2. 2.Environmental Geochemistry Group, Southeast Environmental Research Center (SERC) and Department of Chemistry and BiochemistryFlorida International UniversityMiamiUSA

Personalised recommendations