Beach Dune, Coastal Strand and Maritime Hammock
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A Quick Guide to Southeast Florida's Coral Reefs
A Quick Guide to Southeast Florida’s Coral Reefs DAVID GILLIAM NATIONAL CORAL REEF INSTITUTE NOVA SOUTHEASTERN UNIVERSITY Spring 2013 Prepared by the Land-based Sources of Pollution Technical Advisory Committee (TAC) of the Southeast Florida Coral Reef Initiative (SEFCRI) BRIAN WALKER NATIONAL CORAL REEF INSTITUTE, NOVA SOUTHEASTERN Southeast Florida’s coral-rich communities are more valuable than UNIVERSITY the Spanish treasures that sank nearby. Like the lost treasures, these amazing reefs lie just a few hundred yards off the shores of Martin, Palm Beach, Broward and Miami-Dade Counties where more than one-third of Florida’s 19 million residents live. Fishing, diving, and boating help attract millions of visitors to southeast Florida each year (30 million in 2008/2009). Reef-related expen- ditures generate $5.7 billion annually in income and sales, and support more than 61,000 local jobs. Such immense recreational activity, coupled with the pressures of coastal development, inland agriculture, and robust cruise and commercial shipping industries, threaten the very survival of our reefs. With your help, reefs will be protected from local stresses and future generations will be able to enjoy their beauty and economic benefits. Coral reefs are highly diverse and productive, yet surprisingly fragile, ecosystems. They are built by living creatures that require clean, clear seawater to settle, mature and reproduce. Reefs provide safe havens for spectacular forms of marine life. Unfortunately, reefs are vulnerable to impacts on scales ranging from local and regional to global. Global threats to reefs have increased along with expanding ART SEITZ human populations and industrialization. Now, warming seawater temperatures and changing ocean chemistry from carbon dioxide emitted by the burning of fossil fuels and deforestation are also starting to imperil corals. -
This Keyword List Contains Indian Ocean Place Names of Coral Reefs, Islands, Bays and Other Geographic Features in a Hierarchical Structure
CoRIS Place Keyword Thesaurus by Ocean - 8/9/2016 Indian Ocean This keyword list contains Indian Ocean place names of coral reefs, islands, bays and other geographic features in a hierarchical structure. For example, the first name on the list - Bird Islet - is part of the Addu Atoll, which is in the Indian Ocean. The leading label - OCEAN BASIN - indicates this list is organized according to ocean, sea, and geographic names rather than country place names. The list is sorted alphabetically. The same names are available from “Place Keywords by Country/Territory - Indian Ocean” but sorted by country and territory name. Each place name is followed by a unique identifier enclosed in parentheses. The identifier is made up of the latitude and longitude in whole degrees of the place location, followed by a four digit number. The number is used to uniquely identify multiple places that are located at the same latitude and longitude. For example, the first place name “Bird Islet” has a unique identifier of “00S073E0013”. From that we see that Bird Islet is located at 00 degrees south (S) and 073 degrees east (E). It is place number 0013 at that latitude and longitude. (Note: some long lines wrapped, placing the unique identifier on the following line.) This is a reformatted version of a list that was obtained from ReefBase. OCEAN BASIN > Indian Ocean OCEAN BASIN > Indian Ocean > Addu Atoll > Bird Islet (00S073E0013) OCEAN BASIN > Indian Ocean > Addu Atoll > Bushy Islet (00S073E0014) OCEAN BASIN > Indian Ocean > Addu Atoll > Fedu Island (00S073E0008) -
Brighton Beach Groynes
CASE STUDY: BRIGHTON BEACH GROYNES BRIGHTON, SOUTH AUSTRALIA FEBRUARY 2017 CLIENT: CITY OF HOLDFAST BAY Adelaide’s beaches are affected by a common phenomenon called ELCOROCK® longshore drift - the flow of water, in one direction, along a beach occurring as a result of winds and currents. In Adelaide longshore drift flows from south to north and it frequently erodes beaches The ELCOROCK system consists of sand- over time, particularly during storm events when tides are high and filled geotextile containers built to form sea is rough. a stabilising, defensive barrier against coastal erosion. Without sand replenishment, the southern end of Adelaide’s beaches will slowly erode and undermine existing infrastructure at The robustness and stability of Elcorock the sea/land interface. The objective of Elcorock sand container geotextile containers provide a solutions groynes, laid perpendicular to the beach, is to capture some of for other marine structures such as groynes and breakwaters. These the natural sand as well as dredged sand, that moves along the structures extend out into the wave zone coast. Over time, this process builds up the beach, particularly and provide marina and beach protection, between the groynes which results in the protection of the existing sand movement control and river training. infrastructure. The size of the container can easily be Geofabrics met with the city of Holdfast Bay in the early stages of selected based on the wave climate and the project to discuss the product, durability and previous projects other conditions ensuring stability under with a similar application. Due to recent weather events, the beach the most extreme conditions. -
Approved Plant List 10/04/12
FLORIDA The best time to plant a tree is 20 years ago, the second best time to plant a tree is today. City of Sunrise Approved Plant List 10/04/12 Appendix A 10/4/12 APPROVED PLANT LIST FOR SINGLE FAMILY HOMES SG xx Slow Growing “xx” = minimum height in Small Mature tree height of less than 20 feet at time of planting feet OH Trees adjacent to overhead power lines Medium Mature tree height of between 21 – 40 feet U Trees within Utility Easements Large Mature tree height greater than 41 N Not acceptable for use as a replacement feet * Native Florida Species Varies Mature tree height depends on variety Mature size information based on Betrock’s Florida Landscape Plants Published 2001 GROUP “A” TREES Common Name Botanical Name Uses Mature Tree Size Avocado Persea Americana L Bahama Strongbark Bourreria orata * U, SG 6 S Bald Cypress Taxodium distichum * L Black Olive Shady Bucida buceras ‘Shady Lady’ L Lady Black Olive Bucida buceras L Brazil Beautyleaf Calophyllum brasiliense L Blolly Guapira discolor* M Bridalveil Tree Caesalpinia granadillo M Bulnesia Bulnesia arboria M Cinnecord Acacia choriophylla * U, SG 6 S Group ‘A’ Plant List for Single Family Homes Common Name Botanical Name Uses Mature Tree Size Citrus: Lemon, Citrus spp. OH S (except orange, Lime ect. Grapefruit) Citrus: Grapefruit Citrus paradisi M Trees Copperpod Peltophorum pterocarpum L Fiddlewood Citharexylum fruticosum * U, SG 8 S Floss Silk Tree Chorisia speciosa L Golden – Shower Cassia fistula L Green Buttonwood Conocarpus erectus * L Gumbo Limbo Bursera simaruba * L -
"National List of Vascular Plant Species That Occur in Wetlands: 1996 National Summary."
Intro 1996 National List of Vascular Plant Species That Occur in Wetlands The Fish and Wildlife Service has prepared a National List of Vascular Plant Species That Occur in Wetlands: 1996 National Summary (1996 National List). The 1996 National List is a draft revision of the National List of Plant Species That Occur in Wetlands: 1988 National Summary (Reed 1988) (1988 National List). The 1996 National List is provided to encourage additional public review and comments on the draft regional wetland indicator assignments. The 1996 National List reflects a significant amount of new information that has become available since 1988 on the wetland affinity of vascular plants. This new information has resulted from the extensive use of the 1988 National List in the field by individuals involved in wetland and other resource inventories, wetland identification and delineation, and wetland research. Interim Regional Interagency Review Panel (Regional Panel) changes in indicator status as well as additions and deletions to the 1988 National List were documented in Regional supplements. The National List was originally developed as an appendix to the Classification of Wetlands and Deepwater Habitats of the United States (Cowardin et al.1979) to aid in the consistent application of this classification system for wetlands in the field.. The 1996 National List also was developed to aid in determining the presence of hydrophytic vegetation in the Clean Water Act Section 404 wetland regulatory program and in the implementation of the swampbuster provisions of the Food Security Act. While not required by law or regulation, the Fish and Wildlife Service is making the 1996 National List available for review and comment. -
Thrinax Radiata Family: Arecaceae Florida Thatch Palm, Jamaican Thatch, Thatch Palm, Chit
Stephen H. Brown, Horticulture Agent Donna Cressman, Master Gardener Lee County Extension, Fort Myers, Florida (239) 533-7513 [email protected] http://lee.ifas.ufl.edu/hort/GardenHome.shtml Thrinax radiata Family: Arecaceae Florida thatch palm, Jamaican thatch, thatch palm, chit Florida Thatch Palm Synonyms (Discarded names): Cocothrinax martii, C. radiate, Thrinax floridana, T. martii, T. multiflora; T. wendlandiana Origin: Extreme southern mainland coast of Florida, Florida Keys, Bahamas, western Cuba, Cayman Islands, Jamaica, Hispaniola, Puerto Rico, Yucatan Peninsula, Honduras, Nicaragua U.S.D.A. Zone: 10A-12B (28°F leaf damage) Growth Rate: Slow Typical Height: 20’ Habit: Solitary; canopy of 12-20 leaves Crownshaft: None Leaf: Palmate, induplicate, circular, slightly folded; divided about halfway into segments that are split at the tips; pointed hastula Leaf Size: 4-5’ wide; segments 2.5’ long, 2” wide Salt Tolerance: High Drought Tolerance: High Wind Tolerance: High Light Requirements: Moderate, high Soil: Widely adaptable Nutritional Requirements: Low Potential Insect Pests: Aphids; scales Propagation: Seeds Human hazards: None Uses: Small gardens; containers; outdoors patios; roadways; parking lots; seasides; specimen Left: The infructescence (fruited stems) hang in a circle around the trunk, sometimes extending beyond the leaf. Natural Geographic Distribution The Florida Thatch Palm, Thrinax radiata, is indigenous to the extreme southern mainland coast of Florida, the Florida Keys, Bahamas, western Cuba, The Cayman Islands, Jamaica, Hispaniola, Puerto Rico, Honduras, Nicaragua, and the eastern coast of the Yucatan Peninsula in Mexico and Belize. In na- ture, this palm almost always grows within the range of salt-laden winds near coastal areas. It grows naturally in sandy or calcareous soils. -
Range Expansion of the Whitenose Shark, Nasolamia Velox, and Migratory Movements to the Oceanic Revillagigedo Archipelago
Journal of the Marine Biological Association of the United Kingdom, page 1 of 5. # Marine Biological Association of the United Kingdom, 2017 doi:10.1017/S0025315417000108 Range expansion of the whitenose shark, Nasolamia velox, and migratory movements to the oceanic Revillagigedo Archipelago (west Mexico) frida lara-lizardi1,2, mauricio hoyos-padilla2,3, james t. ketchum2,4 and felipe galva’ n-magan~a1 1Instituto Polite´cnico Nacional, Centro Interdisciplinario de Ciencias Marinas, Av. IPN s/n. C.P. 23096. La Paz, B.C.S, Mexico, 2Pelagios-Kakunja´ A. C. 1540 Sinaloa, C.P. 23070, La Paz, B.C.S., Mexico, 3Fins Attached, 19675 Still Glen Way, Colorado Springs, CO 80908, USA, 4Centro de Investigaciones Biolo´gicas del Noroeste, Playa Palo de Santa Rita Sur, 23096 La Paz, B.C.S, Mexico Current literature considers that Nasolamia velox has a limited distribution along the coastline of the Eastern Pacific with sporadic sightings in the Galapagos Archipelago. This study provides evidence of the occurrence of this species at the Revillagigedo Archipelago (18899′186′′N 112808′44′′W), Mexico, using acoustic telemetry and videos taken from 2014 to 2016. We report here movements from a coastal location (National Park Cabo Pulmo) to a group of oceanic islands (Revillagigedo Archipelago) by one single individual, supporting the idea of the potential connectivity of sharks between the Gulf of California and the Revillagigedo Archipelago. This report extends the known distribution of N. velox to 400 km off the mainland coast of the Americas, thereby increasing the knowledge of the distribution of a species commonly reported in fishery landings of the Eastern Pacific. -
A New Application for Phylogenetic Marker Development Using Angiosperm Transcriptomes Author(S): Srikar Chamala, Nicolás García, Grant T
MarkerMiner 1.0: A New Application for Phylogenetic Marker Development Using Angiosperm Transcriptomes Author(s): Srikar Chamala, Nicolás García, Grant T. Godden, Vivek Krishnakumar, Ingrid E. Jordon- Thaden, Riet De Smet, W. Brad Barbazuk, Douglas E. Soltis, and Pamela S. Soltis Source: Applications in Plant Sciences, 3(4) Published By: Botanical Society of America DOI: http://dx.doi.org/10.3732/apps.1400115 URL: http://www.bioone.org/doi/full/10.3732/apps.1400115 BioOne (www.bioone.org) is a nonprofit, online aggregation of core research in the biological, ecological, and environmental sciences. BioOne provides a sustainable online platform for over 170 journals and books published by nonprofit societies, associations, museums, institutions, and presses. Your use of this PDF, the BioOne Web site, and all posted and associated content indicates your acceptance of BioOne’s Terms of Use, available at www.bioone.org/page/terms_of_use. Usage of BioOne content is strictly limited to personal, educational, and non-commercial use. Commercial inquiries or rights and permissions requests should be directed to the individual publisher as copyright holder. BioOne sees sustainable scholarly publishing as an inherently collaborative enterprise connecting authors, nonprofit publishers, academic institutions, research libraries, and research funders in the common goal of maximizing access to critical research. ApApplicatitionsons Applications in Plant Sciences 2015 3 ( 4 ): 1400115 inin PlPlant ScienSciencesces S OFTWARE NOTE M ARKERMINER 1.0: A NEW APPLICATION FOR PHYLOGENETIC 1 MARKER DEVELOPMENT USING ANGIOSPERM TRANSCRIPTOMES S RIKAR C HAMALA 2,12 , N ICOLÁS G ARCÍA 2,3,4 * , GRANT T . G ODDEN 2,3,5 * , V IVEK K RISHNAKUMAR 6 , I NGRID E. -
Sand Dunes Computer Animations and Paper Models by Tau Rho Alpha*, John P
Go Home U.S. DEPARTMENT OF THE INTERIOR U.S. GEOLOGICAL SURVEY Sand Dunes Computer animations and paper models By Tau Rho Alpha*, John P. Galloway*, and Scott W. Starratt* Open-file Report 98-131-A - This report is preliminary and has not been reviewed for conformity with U.S. Geological Survey editorial standards. Any use of trade, firm, or product names is for descriptive purposes only and does not imply endorsement by the U.S. Government. Although this program has been used by the U.S. Geological Survey, no warranty, expressed or implied, is made by the USGS as to the accuracy and functioning of the program and related program material, nor shall the fact of distribution constitute any such warranty, and no responsibility is assumed by the USGS in connection therewith. * U.S. Geological Survey Menlo Park, CA 94025 Comments encouraged tralpha @ omega? .wr.usgs .gov [email protected] [email protected] (gobackward) <j (goforward) Description of Report This report illustrates, through computer animations and paper models, why sand dunes can develop different forms. By studying the animations and the paper models, students will better understand the evolution of sand dunes, Included in the paper and diskette versions of this report are templates for making a paper models, instructions for there assembly, and a discussion of development of different forms of sand dunes. In addition, the diskette version includes animations of how different sand dunes develop. Many people provided help and encouragement in the development of this HyperCard stack, particularly David M. Rubin, Maura Hogan and Sue Priest. -
Widespread Paleopolyploidy, Gene Tree Conflict, and Recalcitrant Relationships Among the 3 Carnivorous Caryophyllales1 4 5 Joseph F
bioRxiv preprint doi: https://doi.org/10.1101/115741; this version posted March 10, 2017. The copyright holder for this preprint (which was not certified by peer review) is the author/funder, who has granted bioRxiv a license to display the preprint in perpetuity. It is made available under aCC-BY-NC 4.0 International license. 1 2 Widespread paleopolyploidy, gene tree conflict, and recalcitrant relationships among the 3 carnivorous Caryophyllales1 4 5 Joseph F. Walker*,2, Ya Yang2,5, Michael J. Moore3, Jessica Mikenas3, Alfonso Timoneda4, Samuel F. 6 Brockington4 and Stephen A. Smith*,2 7 8 2Department of Ecology & Evolutionary Biology, University of Michigan, 830 North University Avenue, 9 Ann Arbor, MI 48109-1048, USA 10 3Department of Biology, Oberlin College, Science Center K111, 119 Woodland St., Oberlin, Ohio 44074- 11 1097 USA 12 4Department of Plant Sciences, University of Cambridge, Cambridge CB2 3EA, United Kingdom 13 5 Department of Plant Biology, University of Minnesota-Twin Cities. 1445 Gortner Avenue, St. Paul, MN 14 55108 15 CORRESPONDING AUTHORS: Joseph F. Walker; [email protected] and Stephen A. Smith; 16 [email protected] 17 18 1Manuscript received ____; revision accepted ______. bioRxiv preprint doi: https://doi.org/10.1101/115741; this version posted March 10, 2017. The copyright holder for this preprint (which was not certified by peer review) is the author/funder, who has granted bioRxiv a license to display the preprint in perpetuity. It is made available under aCC-BY-NC 4.0 International license. 19 ABSTRACT 20 • The carnivorous members of the large, hyperdiverse Caryophyllales (e.g. -
South of Hanko Peninsula
2013 5 CT JE RO SEA P C I T BAL Oceana proposal for a Marine Protected Area South of Hanko Peninsula INTRODUCTION Hanko Peninsula, located at the entrance to the Gulf of Finland, is the southern-most part of the Finnish mainland and boasts an archipelago and long sandy beaches. Salinity is relatively low, ranging from 5.5 to 7.5 psu, and the waters in the shallower coastal areas are limnic1. Upwellings, a common occurrence in the area wherein nutrient-rich sediments are brought up to the surface, cause a rapid increase in the salinity in areas at 35 meters, and a small increase in salinity in the surface water2. The inner waters of the archipelago freeze every year, while the more open waters freeze regularly, but not every winter3. Parts of the coastal area are protected under EU Natura 2000 network, and the area is classified as a sea area requiring specific protection measures. Wetland areas are also included in the Ramsar network. Because of the special characteristics of the area (changing salinity, archipelagos, wetlands), there are a lot of different zones that are able to host a wide variety of different species and communities4. Oceana conducted in the spring of 2011 and 2012 information from the area with ROV (Remotely Operated Vehicle), bottom samples and scuba dives. 1 5 South of Hanko Peninsula DesCRipTION OF The AREA Low salinity limits the amount of marine species in the area. Species composition changes completely from the open waters to the coast; with marine species being more common further from the coast and limnic species getting more common closer to the shore. -
Fluvial Sedimentary Patterns
ANRV400-FL42-03 ARI 13 November 2009 11:49 Fluvial Sedimentary Patterns G. Seminara Department of Civil, Environmental, and Architectural Engineering, University of Genova, 16145 Genova, Italy; email: [email protected] Annu. Rev. Fluid Mech. 2010. 42:43–66 Key Words First published online as a Review in Advance on sediment transport, morphodynamics, stability, meander, dunes, bars August 17, 2009 The Annual Review of Fluid Mechanics is online at Abstract fluid.annualreviews.org Geomorphology is concerned with the shaping of Earth’s surface. A major by University of California - Berkeley on 02/08/12. For personal use only. This article’s doi: contributing mechanism is the interaction of natural fluids with the erodible 10.1146/annurev-fluid-121108-145612 Annu. Rev. Fluid Mech. 2010.42:43-66. Downloaded from www.annualreviews.org surface of Earth, which is ultimately responsible for the variety of sedi- Copyright c 2010 by Annual Reviews. mentary patterns observed in rivers, estuaries, coasts, deserts, and the deep All rights reserved submarine environment. This review focuses on fluvial patterns, both free 0066-4189/10/0115-0043$20.00 and forced. Free patterns arise spontaneously from instabilities of the liquid- solid interface in the form of interfacial waves affecting either bed elevation or channel alignment: Their peculiar feature is that they express instabilities of the boundary itself rather than flow instabilities capable of destabilizing the boundary. Forced patterns arise from external hydrologic forcing affect- ing the boundary conditions of the system. After reviewing the formulation of the problem of morphodynamics, which turns out to have the nature of a free boundary problem, I discuss systematically the hierarchy of patterns observed in river basins at different scales.