John F. Meeder

ORCID: 0000-0002-0671-8342
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Research Areas
  • Coastal wetland ecosystem dynamics
  • Geology and Paleoclimatology Research
  • Coastal and Marine Dynamics
  • Marine and coastal plant biology
  • Coastal and Marine Management
  • Tropical and Extratropical Cyclones Research
  • Coral and Marine Ecosystems Studies
  • Geological formations and processes
  • Geophysics and Gravity Measurements
  • Plant and Fungal Species Descriptions
  • Soil erosion and sediment transport
  • Marine Biology and Ecology Research
  • Peatlands and Wetlands Ecology
  • Methane Hydrates and Related Phenomena
  • Marine and environmental studies
  • Hydrology and Sediment Transport Processes
  • demographic modeling and climate adaptation
  • Plant responses to water stress
  • Paleontology and Stratigraphy of Fossils
  • Reservoir Engineering and Simulation Methods
  • Tree Root and Stability Studies
  • Groundwater flow and contamination studies
  • Aquatic Ecosystems and Phytoplankton Dynamics
  • Forest ecology and management
  • Hydraulic flow and structures

Florida International University
1997-2024

Allegheny College
2013

Illinois Archaeological Survey
2002

National Audubon Society
1991

University of Miami
1982

Abstract. We examined the vegetation of Southeast Saline Everglades (SESE), where water management and sea level rise have been important ecological forces during last 50 years. Marshes within SESE were arranged in well‐defined compositional zones parallel to coast, with mangrove‐dominated shrub communities near coast giving way graminoid‐mangrove mixtures, then Cladium marsh. The gradient was accompanied by an interiorward decrease total aboveground biomass, increases leaf area index...

10.2307/3236781 article EN Journal of Vegetation Science 2000-02-01

10.1023/a:1008411103288 article EN Wetlands Ecology and Management 2001-01-01

Meeder, J.F. and Parkinson, R.W., 2018. SE Saline Everglades transgressive sedimentation in response to historic acceleration sea-level rise: A viable marker for the base of Anthropocene?Rate global eustatic rise during Holocene Epoch has been identified as principle cause observed changes or inferred evolution nontectonic coastal systems mid- low-latitude areas. The rate is now three times faster than it was past several thousand years similar values associated with middle marine...

10.2112/jcoastres-d-17-00031.1 article EN Journal of Coastal Research 2017-09-20

Abstract Aim and Questions Sea‐level rise has been responsible for extensive vegetation changes in coastal areas worldwide. The intent of our study was to analyze dynamics a South Florida watershed within an explicit spatiotemporal framework that might aid projecting the landscape's future response restoration efforts. We also asked whether recent transgression by mangroves other halophytes resulted reduced plant diversity at local or subregional scales. Location Florida’'s Southeast Saline...

10.1111/jvs.13267 article EN Journal of Vegetation Science 2024-05-01

Abstract The Miami Limestone is an oolite depositional body that used as analog model for geological interpretation of the rock record. Barrier‐bar complex, banks, extensive bryozoan flats and tidal creeks, referred to transverse glades, have been described. High‐resolution LiDAR data are produce unprecedented, detailed topographic maps glades in southern Atlantic Coastal Ridge. These were originally calculate historic discharge from Everglades but revealed features inconsistent with...

10.1002/dep2.84 article EN cc-by The Depositional Record 2019-07-24

Abstract A transgressive palustrine depositional model is described for the South‐east Saline Everglades, Florida. The origin, development and termination of freshwater carbonate mud (marl) deposition along very low gradient Late Pleistocene ramp are responses to changing rates rising sea level during Holocene. onset Holocene defined by a decrease in rate sea‐level rise from between 2 3 <1 mm year −1 . Freshwater marl began with this ca 3165 ± 187 BP, shallow (<0.3 m deep), ephemeral...

10.1002/dep2.314 article EN cc-by The Depositional Record 2024-10-09

Research Article| December 01, 1991 Mud-bank destruction and the formation of a transgressive sand sheet, southwest Florida inner shelf RANDALL W. PARKINSON; PARKINSON 1Department Oceanography, Ocean Engineering, Environmental Science, Institute Technology, Melbourne, 32901 Search for other works by this author on: GSW Google Scholar JOHN F. MEEDER 2National Audubon Society, Abbeville, Louisiana 70510 GSA Bulletin (1991) 103 (12): 1543–1551....

10.1130/0016-7606(1991)103<1543:mbdatf>2.3.co;2 article EN Geological Society of America Bulletin 1991-12-01
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