Florida Bay
![](http://upload.wikimedia.org/wikipedia/commons/thumb/a/a1/Evergladesareamap.png/300px-Evergladesareamap.png)
Florida Bay is the bay located between the southern end of the Florida mainland (the Florida Everglades) and the Florida Keys in the United States. It is a large, shallow estuary that while connected to the Gulf of Mexico, has limited exchange of water due to various shallow mudbanks covered with seagrass.[1] The banks separate the bay into basins, each with its own unique physical characteristics.
Description
[edit]![](http://upload.wikimedia.org/wikipedia/commons/thumb/b/b9/FloridaBaychart.png/300px-FloridaBaychart.png)
Encompassing roughly one-third of Everglades National Park,[2] Florida Bay is variously stated to be 800 square miles (2,100 km2),[3] or 850 square miles (2,200 km2),[4] or 1,000 square miles (2,600 km2).[5] Nearly all of Florida Bay is included in Everglades National Park. The southern edge, along the Florida Keys, is in the Florida Keys National Marine Sanctuary.
While there is no sharp boundary between Florida Bay and the Gulf of Mexico, the westernmost edge of Florida Bay can be approximated by a line drawn from Long Key to Cape Sable on the mainland, which is very close to the boundary line of Everglades National Park.[6][7] The northeastern edge of Florida Bay is at Jewfish Creek in Key Largo. Blackwater Sound, southwest of Jewfish Creek, is generally considered part of Florida Bay; Barnes Sound, on the other side of jewfish Creek, is not. Barnes Sound is generally considered part of the Biscayne Bay system.[8]
![](http://upload.wikimedia.org/wikipedia/commons/thumb/b/ba/JewfishCreek-p.jpg/220px-JewfishCreek-p.jpg)
The bay consists of more than 50 shallow (one to three meters deep) basins or lakes separated by mud banks and mangrove islands. Such basins include: Little Blackwater Sound, Blackwater Sound, Tarpon Basin, Buttonwood Sound, Duck Key Basin, Eagle Key Basin, Madeira Bay, Calusa Key Basin, Crane Key Basin, Rankin Lake, Whipray Basin, Twin Key Basin, Rabbit Key Basin, and Johnson Key Basin.[9][10][11]
Water flows between the basins in narrow channels and over the mud banks. The bay is open to the Gulf of Mexico to the west, but connection to the Atlantic Ocean to the east is restricted to narrow channels between the Florida Keys. The average tidal range along the western edge of the bay is 1 to 1.5 meters, but the tidal range diminishes quickly eastward in the bay due to the restricted flow of water between basins. Fresh water flow into the bay is restricted to Taylor Slough and Trout Creek in the northeast corner of the bay, and is only 10% of the freshwater supply to the bay (rainfall provides the rest of the fresh water). Due to the poor circulation of water within the bay, salinity increases rapidly away from the margins of the bay, except for the northeast part of the bay where it receives fresh water from rivers.[12]
Geology
[edit]Florida Bay is underlain by a flat oolitic limestone bedrock, the Miami Limestone. The top of the bedrock is about 1 metre (3 ft 3 in) below sea level in the northeast corner of the bay, and slopes to 2 to 3 metres (6 ft 7 in to 9 ft 10 in) below sea level in the southwest. Isolated high spots occur at East Key, Arsnicker Key, and Lignumvitae Key, which are underlain by patches of Pleistocene coral.[13]
The Miami Limestone of Florida Bay formed during the Sangamon interglacial between the most recent glacial period, the Wisconsin, and the preceding Illinoian, centered on about 125,000 years ago. The sea level stood higher then than at present, covering much of what is now southern Florida. A coral reef grew on the eastern edge of the Florida platform, while the shallow, protected waters west of the reef formed oolites or hosted large fields of bryozoans.[14][7]
The bay bottom is covered by a grey to black calcium carbonate mud, rich in hydrogen sulfide, that is composed primarily of marine worm fecal pellets. Under much of the mud is a layer of peat and caliche, believed to be remnants from when the sea level was lower and the floor of what is now Florida Bay was part of the Everglades.[15]
Flora and fauna
[edit]The bay's many basins that are broken up by banks serve as plentiful fishing grounds for snook (Centropomus undecimalis), redfish (Sciaenops ocellatus), spotted seatrout (Cynoscion nebulosus), tarpon (Megaflops atlanticus), bonefish (Albula vulpes), and permit (Trichinous falcatus), among others.[16]
The bay is home to many species of wading birds. Most notably, Roseate spoonbills (Platalea ajaja), Reddish egrets (Egretta rufescens), and Great White Herons (Ardea herodias occidentalis) have unique subpopulations that are largely restricted to Florida Bay.[17] Other bird species include Bald eagles, seagulls, pelicans, sandpipers, cormorants, ospreys, and flamingos.[18]
Bay land animals include raccoons, opossums, bobcats, and fox squirrels.[18]
Environmental issues
[edit]Florida Bay has undergone a series of ecological changes beginning in the late 1980s that have severely altered the ecosystem.[19] Originally, clean freshwater flowed south through the state into the Florida Bay. To support the state's agricultural water needs, namely for sugar cultivation, the water was rerouted and no longer flows into the Bay. The flow of fresh water is believed to have caused environmental issues and loss of native wildlife.[20] However, examination of the paleontology of biota in cores from bay muds in Florida Bay have found that historically the salinity of water in Florida Bay has been primarily dependent on rainfall rather than flow from the Everglades.[21]
Seagrass die-off
[edit]![](http://upload.wikimedia.org/wikipedia/commons/thumb/7/7d/Rafts_of_dead_seagrass_in_Florida_Bay.png/249px-Rafts_of_dead_seagrass_in_Florida_Bay.png)
The rerouting of the flow of freshwater to the Bay coupled with periods of drought have caused massive seagrass die-offs.[22] The first major die-off occurred from 1987 to 1991 as thousands of hectares of turtlegrass beds (Thalassia testudinum) were devastated by high levels of toxic dissolved sulfide.[23] 10,000 acres died in the central and western bay, and almost 60,000 additional acres suffered reduced productivity and biomass as a result.[24] Then, following the 2015 drought, extreme temperatures and heightened salinity reduced the amount of oxygen that could remain dissolved in the water, causing periods of anoxia during nighttime and thereby damaging the health of the turtlegrass in the bay. During the summer and fall of 2015, approximately 40,000 acres of seagrass died.[25]
![](http://upload.wikimedia.org/wikipedia/commons/thumb/3/33/Area_of_Florida_Bay_turtle_grass_die-off_event_in_July_2015_through_February_2016.png/220px-Area_of_Florida_Bay_turtle_grass_die-off_event_in_July_2015_through_February_2016.png)
Hyper-salinity
[edit]The 2015 drought period of low precipitation combined with high temperatures and calm winds that produced rapid evaporation caused salinity to increase in the semi-enclosed basins in north-central Florida Bay. Without the freshwater, the water has become stagnant and salty with excess nitrogen from the fertilizer.[26] This hyper-salinity contributes to the massive seagrass die-offs and algal blooms, and kills submerged aquatic vegetation.[24]
Algae blooms
[edit]Cyanobacterial harmful algae blooms (also known as blue-green algae) have flourished in the bay due to a variety of environmental stressors: Agricultural fertilizer run-off increases nutrients in the delicately balanced environment and the excess increases the bacteria's rate of growth; The newly hyper-saline environment provides an ideal breeding ground for cyanobacteria;[27] Rafts of dead seagrass floating on the surface of the water as well as decaying on the bay bottom leads to anoxia and in turn, algal blooms.[1]
Blue-green algae causes numerous severe health consequences for the marine ecosystem as well surrounding human populations. Blooms result in reduced dissolved oxygen concentrations, alterations in aquatic food webs, algal scum lining the shores, the production of compounds that cause distasteful drinking water and fish flesh, and the production of toxins severe enough to poison aquatic as well as terrestrial organisms.[28] Blooms have been reported throughout the continental United States, and resulting cyanotoxins have been associated with human and animal illness and death in at least 43 states.[29] Most cyanobacteria produce the neurotoxin beta-N-methylamino-l-alanine (BMAA) that has been implicated as a significant environmental risk in the development of neurodegenerative diseases such as Alzheimer's disease, Parkinson's disease, and amyotrophic lateral sclerosis (ALS).[30] The cyanobacteria has also been linked to liver cancer, chronic fatigue illness, skin rashes, abdominal cramps, nausea, diarrhea and vomiting.[31]
The 2002 algal bloom in the central portion of the Florida Bay was associated with high concentrations of dissolved organic nitrogen and organic phosphorus, whereas the eastern bay regions bloom was associated with high concentration of inorganic nutrients.[32]
Loss of native wildlife
[edit]By the mid 1930s, the three main species of wading birds in the bay (Roseate spoonbills, Reddish egrets, Great herons) were driven to near extinction by human harvesting for food and feathers.[17]
The cyanobacteria create an oxygen-free environment teaming with toxic gases, creating an unsuitable living environment for many marine and terrestrial animal species.[33] As a result, seasons during which algal blooms flourish cause a temporary loss in wildlife.
Spotted seatrout populations in the coasted Everglades are declining.[34] As the second most commonly caught species of fish in the Florida Bay, spotted seatrout comprise a large portion of the fishing industry and are integral to the ecosystem as well as surrounding economy. Water temperature of less than 80 °F (27 °C) and salinity levels below 37.5 parts per thousand (ppt) are ideal for seatrout spawning; however, water management stations in the Everglades and Florida Bay reported salinity levels of 64.4 ppt in July 2015 and recorded water temperatures of up to 92 °F (33 °C).[34] These environmental conditions are far from ideal for the seatrout and add additional difficulties for the survival of juveniles as well as important prey such as larval shrimp and small fish.[34]
Economy
[edit]The bay is an economic and environmental asset. As of 2017[update], the recreational fishing industry in Florida Bay had an estimated value of $7.1 billion, and generated $73 million in federal, state and local taxes annually, while the bay's commercial fishing industry had an estimated value of $400 million, and generated $3 million in taxes.[35]
Water management projects
[edit]Various projects are funded by the government in an attempt to manage the hydrology issues present in the Florida Bay, including the C-111 South Dade, Modified Water Deliveries, and C-111 Spreader Canal Western Project from the Comprehensive Everglades Restoration Plan (CERP).[20] These projects seek to distribute more freshwater into the sloughs but do not deliver additional water to the bay.
Navigation
[edit]The U.S. Atlantic Intracoastal Waterway goes through Florida Bay, generally following the southern boundary of the Everglades National Park.[10] Florida Bay is a Marine protected area designated as a "Particularly Sensitive Sea Area" by the International Maritime Organization in 2002.[36] Boating in Florida Bay off the Intracoastal Waterway is considered challenging, because of shallow depths, mud, and seagrass.[37]
References
[edit]- ^ a b SeaGrass 2016.
- ^ Chris Mooney. "This massive seagrass die-off is the latest sign we're failing to protect the Everglades". The Washington Post. Retrieved 2016-12-13.
- ^ Everglades National Park Archived 2020-11-10 at the Wayback Machine, Park Vision
- ^ Florida Bay, Encyclopædia Britannica Online
- ^ The Ecology of Florida Bay Archived 2020-12-13 at the Wayback Machine, by Daniel Phirman
- ^ "Florida Bay Marine Basin Region (map)". ArcGIS Online. December 1, 2021. Retrieved May 4, 2024.
- ^ a b Shinn & Lidz 2018, p. 24.
- ^ Smith, Ned P. (Summer 2001). "Tides of Biscayne Bay, Card Sound, Little Card Sound, Barnes Sound, and Manatee Bay, Florida". Florida Scientist. 64: 224. JSTOR 24321024.
- ^ Durako, Morgan J. (2012). "Using PAM fluorometry for landscape level assessment of Thalassia testudinum:Can diurnal variation in photochemical efficiency be used as an ecoindicator of seagrass health?". Ecological Indicators. 18: 244. doi:10.1016/j.ecolind.2011.11.025 – via ResearchGate.
- ^ a b OCS 1983.
- ^ Shinn & Lidz 2018, pp. 21, 113.
- ^ Lee, Thomas N.; Johns, Elizabeth; Smith, Ryan H.; Ortner, Peter; Smith, Dewitt (2006). "On Florida Bay Hypersalinity and Water Exchange". Bulletin of Marine Science. 79 (2): 302.
- ^ Shinn & Lidz 2018, p. 25.
- ^ Mitchell-Tapping, Hugh J. (Spring 1980). "Depositional History of the Oolite of the Miami Limestone Formation". Florida Scientist. 43 (2): 116–125. JSTOR 24319647.
- ^ Shinn & Lidz 2018, pp. 24–25.
- ^ "Florida Bay and Everglades National Park: Flats-Fishing Paradise". Salt Water Sportsman. Retrieved 2017-06-27.
- ^ a b Powell, George V. N.; Bjork, Robin D.; Ogden, John C.; Paul, Richard T.; Powell, A. Harriett; Robertson, William B. (1989). "Population Trends in Some Florida Bay Wading Birds". The Wilson Bulletin. 101 (3): 436–457. JSTOR 4162751.
- ^ a b National Park Service. "Florida Bay Bistro" (PDF). National Park Service.
- ^ Hanson, Matthew R.; Baldwin, John D. (2017-03-01). "Adjusted Diets of Bald Eagles (Haliaeetus leucocephalus) Breeding In An Altered Estuary". Journal of Raptor Research. 51 (1): 1–14. doi:10.3356/JRR-16-00005.1. ISSN 0892-1016. S2CID 89631326.
- ^ a b Solution 2016.
- ^ "Digging Up the Past". National Park Service. Archived from the original on August 12, 2006. Retrieved August 31, 2024.
- ^ National Park Service U.S. Department of the Interior (May 2016). "2015 Florida Bay Seagrass Die-Off" (PDF). South Florida Natural Resources Center.
- ^ Yarbro, L.; Carlson, P. R. Jr. (2016-02-01). "Recurrence of Seagrass Mortality in Florida Bay: The Role of Climate Change and Implications for Carbon Sequestration". AGU Fall Meeting Abstracts. 54: EC54A–1309. Bibcode:2016AGUOSEC54A1309Y.
- ^ a b Sklar, Fred H. (October 8, 2015). "Florida Bay: Current Conditions". South Florida Water Management District.
- ^ National Park Service (May 2016). "2015 Florida Bay Seagrass Die-Off" (PDF). South Florida Natural Resources Center.
- ^ Robert Mcclure And Don Melvin. (1993). "The Dead Zone Once A Teeming Marine Nursery, Florida Bay Today Is Dying". SunSentinel
- ^ "General Information| Harmful Algal Blooms | CDC". www.cdc.gov. Retrieved 2017-06-27.
- ^ Jennifer L. Graham, Neil M. Dubrovsky, Sandra M. Eberts (2016). "Cyanobacterial Harmful Algal Blooms and U.S. Geological Survey Science Capabilities" (PDF). USGS. Archived from the original (PDF) on March 4, 2017. Retrieved 2017-06-27.
{{cite web}}
: CS1 maint: multiple names: authors list (link) - ^ Hudnell, H.K., ed., 2008, Cyanobacterial harmful algal blooms– State of the science and research needs: Advances in Experi- mental Medicine and Biology, v. 619, 950 p.
- ^ Brand, Larry E.; Pablo, John; Compton, Angela; Hammerschlag, Neil; Mash, Deborah C. (2010-09-01). "Cyanobacterial blooms and the occurrence of the neurotoxin, beta-N-methylamino-l-alanine (BMAA), in South Florida aquatic food webs". Harmful Algae. 9 (6): 620–635. doi:10.1016/j.hal.2010.05.002. PMC 2968748. PMID 21057660.
- ^ Guest, David (November 9, 2006). "The Lake Okeechobee Pollution Crisis and the St. Lucie River and Estuary" (PDF). EarthJustice.org.
- ^ Glibert, P. M.; Heil, C. A.; Hollander, D.; Revilla, M.; Hoare, A.; Alexander, J.; Murasko, S. (2004). "Evidence for dissolved organic nitrogen and phosphorus uptake during a cyanobacterial bloom in Florida Bay". Marine Ecology Progress Series. 280: 73–83. Bibcode:2004MEPS..280...73G. doi:10.3354/meps280073. JSTOR 24867855.
- ^ David Biello, (2008). "Oceanic Dead Zones Continue to Spread". Scientific American
- ^ a b c Trout 2015.
- ^ Stainback, Andrew (April 17, 2017). "The Economic Significance of Florida Bay" (PDF). conference.ifas.ufl.edu. Everglades Foundation via the University of Florida’s Institute of Food and Agricultural Sciences Office of Conferences & Institutes. Archived (PDF) from the original on May 14, 2018. Retrieved November 13, 2018.
- ^ International Maritime Organization, "Particularly Sensitive Sea Areas." https://www.imo.org/en/ourwork/environment/pages/pssas.aspx
- ^ U.S. National Park Service. "Florida Bay, Everglades National Park." https://www.nps.gov/places/florida-bay.htm
Sources
[edit]- Shinn, Eugene A.; Lidz, Barbara H. (2018). Geology of the Florida Keys. Gainesville, Florida: University Press of Florida. ISBN 978-0-8130-5651-7.
- "Got Trout? Spotted seatrout vanishing from Florida Bay". Everglades Foundation. Archived from the original on September 10, 2015.
- National Park Service (May 2016). "2015 2015 Florida Bay Seagrass Die-Off" (PDF). NPS.gov.
- "Florida Bay: What is The Solution?". Everglades Foundation. Archived from the original on July 31, 2020. Retrieved 2017-06-27.
- OCS (June 1983). Fowey Rocks to American Shoal (Chart 11450) (Navigation chart). 1:180,000. United States Department of Commerce, National Oceanic and Atmospheric Administration.
External links
[edit]Media related to Florida Bay at Wikimedia Commons
- U.S. Geological Survey Geographic Names Information System: Florida Bay