2013
DOI: 10.1016/j.palaeo.2012.12.020
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Impact of Late Holocene climate variability and anthropogenic activities on Biscayne Bay (Florida, U.S.A.): Evidence from diatoms

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Cited by 12 publications
(9 citation statements)
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“…Changes in sedimentary diatom assemblages in shallow marine environments in Florida have also been related with extreme climatic conditions associated with large-scale climatic oscillations like ENSO or the Pacific Decadal Oscillation (PDO) events (Wachnicka et al 2013). In these environments the changes in diatom assemblages have been mostly triggered by the cold phases of these events, and they have been irreversible.…”
Section: Historical Perspectivementioning
confidence: 99%
“…Changes in sedimentary diatom assemblages in shallow marine environments in Florida have also been related with extreme climatic conditions associated with large-scale climatic oscillations like ENSO or the Pacific Decadal Oscillation (PDO) events (Wachnicka et al 2013). In these environments the changes in diatom assemblages have been mostly triggered by the cold phases of these events, and they have been irreversible.…”
Section: Historical Perspectivementioning
confidence: 99%
“…Post 1950, diatom communities in most cores show a significant increase in abundance of epiphytic communities and in taxa with wider salinity tolerances (Wachnicka and Wingard, 2015). The frequency and magnitude of shifts in diatom species composition also increased post-1950s (Wachnicka et al, 2013c;Wachnicka and Wingard, 2015), which agrees with research that has indicated the rate of biological change usually increases with continuous changes to environmental conditions (Folke et al, 2004). The diatom analyses are consistent with paleoecologic analyses of other benthic organisms (mollusks, ostracodes, foraminifers) that detected significant shifts between the 1940s and 1960s in cores from south Florida's estuaries (Brewster-Wingard and Ishman, 1999;Alvarez Zarikian et al, 2001;BrewsterWingard et al, 2001;Cronin et al, 2001;Wingard et al, 2003Wingard et al, , 2004.…”
Section: Understanding Biotic Responses To Sea Level Climate and Anmentioning
confidence: 94%
“…Major shifts in the structure of ostracode and diatom assemblages often coincide with shifts in the intensity of ENSO, AMO, and the Pacific Decadal Oscillation (PDO). Wachnicka et al (2013c) showed that the occurrence of severe and prolonged droughts associated with a combination of extreme cold phases of ENSO, AMO, and PDO, or a combination of warm phases of AMO and cold phases of PDO, corresponded to significant changes in the structure of diatom assemblages in cores from Biscayne Bay (Figure 6). For example, the largest shifts in diatom assemblage structure in Card Sound Bank and No Name Bank cores in the late 1950s coincided with changes in precipitation from below average to above average.…”
Section: Understanding Biotic Responses To Sea Level Climate and Anmentioning
confidence: 99%
“…Evaporation in south Florida is high in the summer months, but total annual rainfall exceeds annual evaporation. In addition to discrete storm events, multi-decadal oscillations such as El Niño Southern Oscillation (ENSO), Atlantic Multidecadal Oscillation (AMO), and North Atlantic Oscillation (NAO), combined with millennial scale forcing like the mean position of the Intertropical Convergence Zone (ITCZ), have a significant role in shaping the south Florida climate (Bernhardt, 2011;Cronin et al, 2012;Wachnicka et al, 2013b). These climatic oscillations are a factor in periodic flooding and droughts in the Everglades ecosystem, and affect water level, flow and hydroperiod (DeAngelis and White, 1994).…”
Section: Regional Setting and Site Locationsmentioning
confidence: 99%