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10 results for “Key Largo”
Radiation measurements at Key Largo Ranger Station, South Florida (FCE) for July 2001
Basic radiation data, including Infra-red canopy temperatures, collected as 1 minute averages from a 5 m tower at Key Largo Ranger Station, South Florida, near Everglades National Park.
Meteorological measurements at Key Largo Ranger Station, South Florida (FCE) for July 2001 to August 2001
Basic radiation data, including Infra-red canopy temperatures, collected as 1 minute averages from a 5 m tower at Key Largo Ranger Station, South Florida, near Everglades National Park.
Mangrove leaf physiological response to local climate at Key Largo, Watson River Chickee, Taylor Slough, and Little Rabbit Key, South Florida (FCE) from July 2001 to August 2001
Determine the red mangrove leaf physiological response to the local climate to understand the local controls on plant physiology. Data were collected in the Key Largo Ranger Station, Watson River Chickee and Taylor Slough research Sites, South Florida.
Rubisco limited photosynthesis rates of Red mangrove leaves at Key Largo, Watson River Chickee, Taylor Slough, and Little Rabbit Key, South Florida (FCE) from July 2001 to August 2001
Determine the Rubisco limited carboxylation rates of red mangrove ( species Rhizophora mangle) leaves. This information will be used to model carbon sequestration by Red mangroves.
Light limited carboxylation rates of Red mangrove leaves at Key Largo, Watson River Chickee, Taylor Slough, and Little Rabbit Key, South Florida (FCE) from July 2001 to August 2001
Our goal is to determine light limited carboxylation rates of red mangrove (specie sRhizophora mangle) leaves. This information will be used to model carbon sequestration by Red mangroves.
Mangrove soil phosphorus addition experiment from June 2013 to August 2013 at the mangrove peat soil mesocosms (FCE), Key Largo, Florida - Nutrients in Porewater, Soil and Roots
Sea levels in South Florida are conservatively predicted to rise by 0.60 m by 2060. The key mechanisms that maintain coastal peatland elevation against increasing sea level are organic matter accumulation via plant production and mineral sedimentation rates (Smoak et al. 2013). Although coastal mangrove soils are regularly inundated with seawater, little is know about the drivers of carbon sequestration (above or below ground) versus atmospheric efflux under different conditions of salinity and elevated phosphorus (P) associated with sea-level rise and storm surge. A recent study using mangrove peat soils found that seawater inundation reduced soil carbon efflux losses and salinity concentration had little effect on carbon retention or loss pathways. The next logical steps are to understand how plant-soil interactions affect above and below ground carbon processes, as well as how increases in P associated with storm surge from the Gulf of Mexico will influence physical, chemical and biological components of mangrove soils that are associated with above and belowground carbon processes. We will manipulate P in inundated peat soil mesocosms with disturbed and undisturbed red mangrove (Rhizophora mangle) seedlings to identify some of the fundamental mechanisms of soil elevation and carbon cycling given expected increases in seawater-based P availability in South Florida coastal mangroves.
Mangrove soil phosphorus addition experiment from July 2013 to August 2013 at the mangrove peat soil mesocosms (FCE), Key Largo, Florida - Nutrients in Surface Water and Aboveground Biomass
Sea levels in South Florida are conservatively predicted to rise by 0.60 m by 2060. The key mechanisms that maintain coastal peatland elevation against increasing sea level are organic matter accumulation via plant production and mineral sedimentation rates (Smoak et al. 2013). Although coastal mangrove soils are regularly inundated with seawater, little is know about the drivers of carbon sequestration (above or below ground) versus atmospheric efflux under different conditions of salinity and elevated phosphorus (P) associated with sea-level rise and storm surge. A recent study using mangrove peat soils found that seawater inundation reduced soil carbon efflux losses and salinity concentration had little effect on carbon retention or loss pathways. The next logical steps are to understand how plant-soil interactions affect above and below ground carbon processes, as well as how increases in P associated with storm surge from the Gulf of Mexico will influence physical, chemical and biological components of mangrove soils that are associated with above and belowground carbon processes. We will manipulate P in inundated peat soil mesocosms with disturbed and undisturbed red mangrove (Rhizophora mangle) seedlings to identify some of the fundamental mechanisms of soil elevation and carbon cycling given expected increases in seawater-based P availability in South Florida coastal mangroves.
Subspecies and Distribution. N.f.floridanusOrd,1818—fromSEtipofNorthCarolinaStoCFlorida(SEUSA). N.f.attwateriMearns,1897—restrictedtoECTexas(SUSA). N.f.baileyiMerriam,1894—restrictedtoasmallareaalongtheSouthDakota—Ne-braskaborder(NCUSA). N.f.campestris|.A.Allen,1894—SWNebraska,EColorado,andWKansas(CUSA). N.f.haematoreiaA.H.Howell,1934—SWNorthCarolinatoNGeorgia(SEUSA). N.f.illinoensisA.H.Howell,1910—fromSIllinoisStoLouisianaandextremeNWFlorida(SEUSA). N.f.osagensisBlair,1939—fromCKansasandCMissouriStoNETexas(SCUSA). N.f.rubidaBangs,1898—fromETexasEtoextremeSWAlabama(SEUSA). N. f. smalli Sherman, 1955 — restricted to Key Largo, Florida (SE USA). in Cricetidae
Subspecies and Distribution. N.f.floridanusOrd,1818—fromSEtipofNorthCarolinaStoCFlorida(SEUSA). N.f.attwateriMearns,1897—restrictedtoECTexas(SUSA). N.f.baileyiMerriam,1894—restrictedtoasmallareaalongtheSouthDakota—Ne-braskaborder(NCUSA). N.f.campestris|.A.Allen,1894—SWNebraska,EColorado,andWKansas(CUSA). N.f.haematoreiaA.H.Howell,1934—SWNorthCarolinatoNGeorgia(SEUSA). N.f.illinoensisA.H.Howell,1910—fromSIllinoisStoLouisianaandextremeNWFlorida(SEUSA). N.f.osagensisBlair,1939—fromCKansasandCMissouriStoNETexas(SCUSA). N.f.rubidaBangs,1898—fromETexasEtoextremeSWAlabama(SEUSA). N. f. smalli Sherman, 1955 — restricted to Key Largo, Florida (SE USA).
Supplementary material 1 from: Boehmler M, Murray HL, DeMay DJ, Rogers AN, Hribar LJ (2023) Dataset for mosquitoes (Diptera, Culicidae) from State Route 905-Mile Marker 2, Key Largo, Monroe County, Florida, USA. Research Ideas and Outcomes 9: e101286. https://doi.org/10.3897/rio.9.e101286
Route 905 MM2 2003-2021
Supplementary material 1 from: Boehmler MB, DeMay DJ, Rogers AN, Murray HL, Hribar LJ (2023) Dataset for mosquitoes (Diptera, Culicidae) from Gun Club Road, Key Largo, Monroe County, Florida, USA. Research Ideas and Outcomes 9: e99607. https://doi.org/10.3897/rio.9.e99607
Gun Club Rd dataset 2003-2021
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