2 General OverviewRiparian comes from the Latin word “ripa”, which means stream bank.A Riparian Ecosystem is a transitional system between aquatic and terrestrial ecosystems.These are either freshwater or marine and can lie near lakes, streams, pond, rivers, oceans or any body of water.
3 Zonation:Riparian systems are zoned just as many other types of ecosystems.Sedges and rush live on the banks at or above water level. These can frequently become submerged depending on what aquatic system is present.Shrubs live above the sedges and rush.Deciduous trees live above the bank and provide shade during the midday sun and a home for various species.The trees are the last plant species characterized in a Riparian system. The Upland system follows.
5 Soil types:There are a variety of soil types found in a Riparian system. Common soils are those which are found in wetlands (silts and clays).Sands and gravels are also common. These are highly porous which allow for water movement.Porosity allows for variability in the types of plants in the system.Zonation occurs in a small distance laterally. There is no general width to the system. It depends on the hydrology of the aquatic system.
6 Habitat: This is a very diverse ecosystem. These areas are very rich in life. They are home to various animals and plant.Small mammals are able to nest on the banks underneath the vegetation while birds are able to nest in the vegetation.The various plant species create a food source as well as shelter for insects, birds, mammals, and even fish in the water.
7 Vegetation:Vegetation provides cover and a natural habitat for species.
8 Uses: The plants that live in these systems help to clean the water. Stem densities near the shore can slow the water movement enough for suspended solids to settle out.The roots also bring in nutrients and metals from the water which help to improve the water quality.
9 Benefits:Natural undeveloped vegetated flood plain allow excess water to spread out and easily re-enter the channel or to be soaked up by the wetland soil.The vegetation provides various barriers against the flowing water.The natural ecosystem is beneficial for wildlife and they are aesthetically pleasing.
10 Human Influence:One problem is that humans tend to straighten and bend waterways at angles. This disrupts currents and creates areas of high erosion.Irrigation ditches are easily flooded because they are not able to handle excess water. High rains can cause them to flood creating more problems.Straight channels reduces surface area of banks and therefore reduces the amount of habitat available for animals. This in turn creates competition for space and food.
11 Human Influence:When buildings and unnatural structures are placed in a floodplain and near waterways reduce the ability of the soil to absorb the water.Buildings also impede the movement of the water and will be damaged by the excess water.
12 ProblemsStraightening or Channelizing waterways has turned them into a mechanical waterway instead of a healthy stream environment.When streams are straightened and direction is changed from its natural state inundation becomes a problem.
13 Problems cont:Acequias are found throughout the west because droughts are common in the area. Water divergence is a common practice which allows farmers to maintain crops through the dry season.This diverts water from its original source direction and into new areas.
15 Acequia cont: These are actually a man made irrigation ditches. These bring water to areas that are normally dry and allow for vegetation to grow that would not normally have been there.Erosion is a problem that frequently occurs
16 Restoration:There are many restoration efforts underway that will return Riparian Ecosystems to there natural state.One major problem with this effort is that diverting the water back to its original habitat will only create more problems just as the original divergence did.The effort must take place where the water is presently routed.
17 Restoration:Terraced and vegetated canal banks are now being used as a way to prevent inundation and erosion in events of high water.Proper plant species such as oaks, willows, and cottonwoods are being used to create shade and help smaller plant species grow.The trees will also out compete weeds to help create a healthy habitat for all life forms.
22 Geographical extentOnly found in freshwater environments not so much climate dependant as hydrology, generally found along rivers and streams in the Southeast Coastal Plain and along the Gulf Coastal Plain to southeastern Texas, and up the Mississippi River to southern Illinois.There a few areas with similar habitat and vegetation located in the northeast these are small in comparison.
23 Southern Deepwater Swamps General overview Sometimes referred to as southern freshwater forested swamp.Freshwater systems with standing water throughout all or most of the year.They can be nutrient-rich in alluvial river swamps or under nutrient-poor conditions such as in rainwater fed swamps.Primary production is closely related to hydrologic conditions.
24 GeomorphologyLocated in broad, flat floodplains or they can be in isolated basins.Deepwater swamps are located in floodplains where there are meandering river channels, adjacent to natural levees, oxbow lakes, and sloughs which represent areas of ponded water. (Leopold et al, 1964)Found in areas of very low relief, where slight changes in elevation (just a few cm) can produce quite different hydrologic conditions, soils, and plant communities. Brown 1972)Biogeochemical processes are strongly linked to hydrologic characteristics. The depth and duration of flooding, as well as whether the flood waters are flowing or stagnant, affect whether the wetlands serve as sinks, sources, or transformers of nutrients..(Brinson 1990)
25 Cypress swamps as sinks, possible transformers and sources Sinks: reports of 50% reduction in P as overflow waters passed through a swamp. (Day et al) In some locations it has been found that they were effective as sinks for over 50 years runoff of partially treated wastewater. More effective however, at P that at N collection.Transformers: total inputs and outputs of nutrients remain similar yet there are noted net increases in organic N and P and a decrease in inorganic N and P. Transformations from inorganic to organic forms can be important for secondary productivity downstream.(Mitsch 1993)Sources: in situations where there is periodic outflow from the system deepwater swamps can act as a mechanism of nutrient conservation during dormant seasons and transferred to the system during the growing season.
26 Hydrologic conditions Hydrology is the most important feature of deepwater swamp environments.Inflows are dominated by runoff from uplands and overflow from flooding rivers. (Mitsch and Gosselink 1993)Outflows are limited by controlled by substrate, and the swamps distance from adjacent streamsTopographic features may impound water and cause flooding from rainfall rather than from stream overflow.Water levels vary seasonally and annually, with high water levels coinciding with winter and spring rains and melting snow. In the summer low levels occur due to high evapotranspiration and low rainfall (Wharton and Brinson 1979)
27 pH and NutrientsWide range of acidity pH can vary from 3.5 in swamps fed by rainwater whereas the pH of many alluvial swamps can be 6 to 7.Cypress domes and dwarf cypress swamps are low in nutrients because of their hydrologic isolation. Sampling of (P) showed concentration of 50 to 160 µg/lAlluvial river swamps and lake edge swamps tend to have much greater input of nutrients. Sampling of (P) showed concentrations as high as 660µg/l(Mitsch et al.1977)
28 Sedimentation/ Primary Production Sediment deposition occurs during flooding conditionsThe rate of sedimentation can control the rate of succession.A high rate of sedimentation is associated with occurrence of cypress and tupelo stands which grow to be years of age (Hodges 1994).Primary productivity seems to be greater in the mixed hardwood swamp environment. These swamps tend to have seasonal flooding rather than constant flooding or constantly drained.
29 Productivity vs. Flooding The highest productivity occurs periodic/seasonal flooding situations, low productivity is characteristic in continuously flooded or drained.
30 Typical Vegetation Canopy vegetation: Well adapted to a wet environment. Includes bald cypress, pond cypress, tupelo, red bay and various hardwoods. Spanish moss typical in deep south.Understory vegetation: (difficult to generalize due to lots of other variables)Dependant on light penetration through canopy. Woody shrubs, small trees, herbaceous veg., variations from nutrient rich to nutrient poor. Nutrient rich areas grow a mat cover.
31 Typical hardwoods in canopy, understory mat of duckweed, virginia willow.
32 ButtressesSwollen Buttress, OkeefenokeeSwamp, GACypress with watermarks,Brunswick Co., NC.Good indicators of hydroperiod. Greatest swelling appears to be where there is continual wetting and soaking of the tree trunk. The actual function is unknown and thought to be a relic response.
33 Cypress KneesExtend from trunks to well above water level. Still unsure as to purpose. Thought to be anchors for the tree and/ or could be possible areas of gas exchange for the root system. (Ewel and Penfound)
34 Five subclassesEach have similar characteristics , however vary slightly(Wharton et al 1976)1.Still water cypress domes2.Dwarf cypress swamps3.Lake-edge swamps4.Slow-flowing cypress strands5.Alluvial river swamps
35 Cypress Domes Rainfall and surface inflow. Generally 1-10 hectares in size.Poorly drained to permanently wet, where they form dense cypress heads, composed almost entirely of cypress; within these heads, growth conditions are better towards the center. Sandy and clay soils, the cypress heads form a very distinctive dome shape and are called cypress domes, with progressively taller tress toward the center, attributed to greater peat accumulation.
36 Dwarf cypress swampsPond cypress is the dominant tree but grows stunted and scattered throughout the freshwater marshes. These trees rarely grow over 7 m high and average only 3 m in height. The poor growing conditions, which are defined here as lack of significant substrate above the limestone, prevent larger trees from establishing themselves in this environment. Fires often occur here but usually do not kill the cypress due to the lack of combustible organic material accumulation.
37 Slow-flowing Cypress Strands Diffuse freshwater stream flowing through a shallow forested depression on a gentle sloping plain (Wharton 1976). Substrate is primarily sand with a mixture of limestone and shell beds. Shallow peat layer. They have a seasonal hydroperiod(wet and dry cycle. Corkscrew Swamp, Fl
38 Lake edge swampsGenerally bald cypress swamps found along lake margins in the Southeast. Also have tupelo and other water tolerant hardwoods. Seasonal fluctuations in water level. Nutrient rich due to runoff from lake and uplands. Also can act as filters that receive overland flow from the uplands and allows sediments to settle and chemicals to absorb into the sediments before discharge into the open lake .
39 Alluvial River swampsFound in floodplains of river and creeks of the southeast. Dominated by bald cypress and/ or water tupelo. Confined to permanently flooded depressions. Abandoned river channels(oxbows) or elongated swamps that usually parallel the river(sloughs). Sometimes referred to as backswamps. Nutrient rich because of river flooding and upland runoff.
40 Economic resources and environmental impacts Cypress was a staple commodity during the ’s for new settlers of the south.These areas were logged extensively. Many deepwater swamps were lost due to clearcutting. Production increased from 495 million board feet 1899 to 1 billion board feet in1913. By 1925 stocks were running low, they had essentially cut all the old growth cypress and second generation cypress was not as well suited. It is still a valuable resource just not as widely marketed.
41 Hydrology modelsS.L. Brown developed a hydrology model depicting how drainage of the Green Swamp wetlands led to lower aquifers, drier streams, and greater flooding.Other models by Littlejohn and Weimoff have demonstrated storage capacities and groundwater protection capabilities of these areas.
42 Further research efforts Studies should be done to improve long term predictive capabilities and knowledge of the fine structure of these systems in order to incorporate proper planning and management practices.Particularly in the area of hydrological function and any factors contributing to loss.
44 Topics Defining pocosins Geographic extent Soils Hydrology Vegetation Low vs. high pocosin communitiesFaunaSuccessionResponse to fireDevelopmentManagement
45 Definitions Fresh water wetlands. Algonquin word poquosin, roughly = “swamp-on-a- hill”.Early European settlers used the term to describe a variety of swampy or marshy land consisting of poorly drained, peaty soils supporting pond pines and evergreen shrubs.The Oxford English Dictionary defines a pocosin as a track of low swampy ground usually wooded in the southern united states.
46 Defintions Cont’dIn 1875 W.C. kerr, the state geologist of NC in a geologic Survey of North Carolina, defined pocosins as “flatwoods with no natural drainage ways, different from swamps in that they are not alluvial, occurring on divides between rivers and sounds and frequently elevated above streams of which they are the source”.
47 Defintions Cont’dIn 1928 Wells provided a more broad definition. According to Wells the defining factors of a pocosin include soil type, hydrology, topography, occurrence of periodic burning, and vegetation.
48 Wells described pocosins as wetlands occurring in broad shallow stream basins, drainage basin heads or broad flat upland areas of the coastal plains that are characterized by long hydroperiods, temporary surface water, periodic burning, and soils of sandy humus, muck, and peat. The dominant vegetation being broad leaved evergreen shrubs or low trees.Later defining of the term by other authors, generally followed this concept pocosins.
49 According to the U.S. fish and Wildlife wetland classification system pocosins are classified as follows:System: PalustrineClass: Scrub-shrubSub-class: Broadleaved evergreen.Water regime: Saturated.Water chemistry: Fresh-acidSoil: Medisaprist
50 Geographic ExtentOccur on the southeastern coastal plain spanning from Virginia to southern Florida.North Carolina possesses seventy percent of all pocosins.In 1962 there were approximately 2,243,550 acres of pocosins in NC.
51 In fact, according to Wilson, at this time pocosins accounted for the primary land area type in several of the counties in North Carolina.Dare: 55.7%Tyrell: 54.2%Hyde: 53.4%Jones: 42.7%Pender: 36.1%Carteret: 34.7%
52 Wilson's data was later compared to 1979 LANDSAT imagery, and aerial photographs to determine the total amount of the pocosin land that had been altered or drained in the seventeen year period.It was determined that 1,503,000 acres of pocosins remained in However only 695,000 of these were left completely in their natural state.
53 740,000 acres (33%) of the pocosins had been completely developed. Completely developed pocosins in this study were defined as those that have been drained and ditched, their natural vegetation removed, their soils prepared for agriculture, forestry, industry, etc, and that are clearly depicted on landsat imagery or other aerial photos.
54 The largest areas of Natural pocosins in North Carolina are located in Pasquotank and Dare counties in The northern coastal plain.
55 Pocosins are also still abundant in Carteret, Craven, and Jones counties, in the central part of the coastal plain.
56 Abundant still in Pender, Duplin, and, Brunswick counties in the southern portion of the coastal plain.
57 Pocosin soilsAt the end of the Wisconsin ice age (~ 10,000 years ago) sea level began to rise from a level approximately 122 m below it current elevation.As the large exposed continental shelf became submerged, stream flows on the eroding plain slowed, and water table rose.
58 Pocosin soilsDeposition in the stream channels increased as did that of the inter-stream areas.With the aid of a more mild climate aquatic vegetation began to grow in shallow areas which in turn led to the accumulation of peat.
59 Pocosin soilsOnce the peat had begun to form in the low drainage areas it built up and out ward laterally across the inter-stream divides.At this point there is the beginning of a transition from a mineral soil to a peat soil.
60 Pocosin soilsC-14 dating results have determined the age of the earliest deposited organic clay and over lying peat of the Chesapeake Bay and Dismal swamp to be approximately approximately 10,340 and 8,135 years before present, respectively.It is believed that the deposition of peat in the lower portions of the North Carolina coastal plain to have occurred around the same time.
61 Pocosin soilsMedisaprist soils: Well decomposed organic soils (histosols) with an organic depth of greater than 40cm.To be considered a histosol a soil must have 20 % organic matter if there is no clay present, or at least 30% if there is up 60% clay.The organic surface horizon of a pocosin soil can be greater than 130 cm.
62 Pocosin soils Anaerobic environment Preserves organics.Acidic, with pH ranging fromNutrient poor. Especially in P.Low cation exchange capacity.Water logged
63 Soils/hydrologyAccumulation of organic matter causes the surface of a pocosin to become regionally elevated.As a result the water table within the peat will rise to a degree that it becomes isolated from the chemical influence of the groundwater system below.Rainwater thereafter is the dominant source of nutrients and minerals, thus a pocosin is ombrotrophic.
64 Soils/hydrologyAt this point there is a change in head force of the water and the net movement is downward through the peat to the underlying sediments.Recharge will occur under these conditions, though it will be very limited.Low conductivity of the peat.Small difference between the two water levels.
65 Soils/HydrologyThe effects of the of the isolation of the water table within the peat and that of the ground water beneath the peat was observed by in study by C.C. Daniel III of the Pungo Wildlife refuge.The figure below shows the reduction of dissolved cations in the water of the shallow well that does not penetrate the peat/mineral soil contact vs. a deeper well that reaches to the groundwater within the mineral soil.
67 Soils/Hydrology Ca reacts with carbonic acid (H2CO3) Forms calcium bicarbonate (Ca[HCO3]2)(Ca[HCO3]2) dissociates in water leaving the bicarbonate ion (HCO3-).Responsible for most of the buffering for natural water systems.This reflects the low pH and poor buffering capabilities of these organic soils.
68 hydrologyThe water budget of pocosins results in fairly static water levels.
69 HydrologyThere are four input out put events that influence water budget.1. PrecipitationExclusive input of water.2. EvapotranspirationGreatest portion of output during summer and fallhigh temperatures and low precipitation.3. RunoffIn form of sheet flow following rain eventsGreatest during winter and springhigher precipitation and consequent higher water table4. Groundwater DischargeVery Low due to poor drainage of peaty soil
70 VegetationIn general structure and distribution of vegetation is controlled by interrelated environmental conditions.Thickness of peatLength of hydroperiodSeverity of fireNutrient availability
71 Vegetation Primary characteristic is presence of a dense shrub layer. Also the pond pine (Pinus Serotina)is indicative of pocosins.Also the zenobia (Zenobia pulverulenta) is native to pocosins.Sphagnum mossThough herbs are not major part of a pocosin community they do sprout vigorously after fire.
72 Two pocosin vegetation types Low vs. high pocosins
73 Low Pocosins Very nutrient poor. Occur in the center of the domed peatlands.Usually on peat deposits1-5m deep.Plant roots can never reach mineral soil.
74 Low Pocosins Identified by low stature of shrubs(<1.5m). Also by sparse distribution and low stature of trees.
75 Low Pocosins Completely ombrotpophic. Low dense shrub layer usually dominated by fetterbush (lyonia Lucida), swamp cyrilla, or titi (Cyrilla racemiflora), or Zenobia, and frequently greenbrier (Smilax spp.).Trees usually include stunted pond pine , as well as swamp red bays, loblolly-bay, and sweetbay (Magnolia virginiana).
76 High PocosinsHigh pocosin vegetation types usually occur from the intermediate portion to the center of the domed peatland.Usually on peat deposits 1.5m thick or less.Peat is shallow and saturated enough for for roots to sometimes reach underlying mineral soil.Shrubs range m tall.Sparse distribution and short stature of trees are also characteristic.
77 High PocosinsReceive very little surface or ground water so are largely ombrotrophic.Vegetation species is similar to low pocosin.Taller shrub layer and trees.More nutrients.
78 Successional Patterns Two contrasting theories.1. Controls of pocosin succession are fire intensity and frequency.Low pocosin considered a pioneer stage succeeding to high pocosin and then bay forest.Climax within a few hundred years (without disturbance).
79 Successional Patterns 2. Succession is controlled by nutrient levels.Succession goes from marsh to swamp forest to bay forest to tall pocosin to short pocosin.Supported by pollen analysis.
80 Development As early as the 1700s swamp land in NC has been developed. The early 1800s successful agriculture at lake Phelps and Mattamuskeet lead to the state draining swamp lands extensively.J. Paul Lilly sates in A History of swamp land development. “that essentially all swamp lands in North Carolina have been logged at least once, and have had some drainage imposed, either for agricultural development, or to aid in logging and reforestation”.
81 DevelopmentDrainage of pocosins and their use as agricultural land can lead to over 20x the phosphorus output of natural pocosins.Those converted to cattle operations have been shown to out put up to 70x the amount of P of a natural pocosin.
82 DevelopmentFor example, the conversion of pocosins to agricultural land in the Albemarle Sound region was shown to output 3X as much N and 28X as much P s before its conversion.Increased nutrient outputs such as these are likely to facilitate the eutrophication process of near by water bodies.And in this case was linked to subsequent algal blooms in The Chowan River.
83 DevelopmentNegative consequences of pocosin drainage and development include but are not limited to.Habitat lossLoss of natural flood bufferDiminished water quality
84 Management/preservation Preservation and smart management of pocosins is imperative for the maintenance of natural diversity in North Carolina.These areas have often been considered wastelands by managers.The continued existence of pocosins relies on these managers to realize their ecological importance, and mandate formal protective safeguards for these communities(Richardson, 1982).
86 DefinitionIsolated, elliptical, shallow depressions (~50’ deep) oriented in a NW-SE direction with a sand ring pronounced in SE: “Neptune’s Racetracks”. Ellipse generally narrows to SE.Often vegetated by bay treesMost depend on rainwater for moisture, nutrients, though some have stream flow.Vary from 50m – 8km in lengthFrom 6,000-60,000 years in age or more
88 DistributionWere possibly ~ 500,000 total, but inventory difficult due to human alteration. Now possibly 10-20,000 remainingLargest given area of occurrence includes southern NJ to northern Fla. ~80% in N. and S. Carolina
89 Wetland LossEstimated 97% of Carolina Bay wetlands in South Carolina have been lost due to :Draining for agriculture- 71%Logging – 34%Highways / developmentthreaten many
90 Named for presence of bay trees: Loblolly bay, red bay, and sweet bay VegetationDepends on size, depth, hydrology, and soil characteristicsFrom open water with pond cypressTo thick, shrubby pocosin type areas on peat matsNamed for presence of bay trees: Loblolly bay, red bay, and sweet bay
91 Some common soil types Ponzer Dominant in large bays RutledgeFound along inside boundary of large bays, but is most of small onesHigher / dryer than PozerHigh organic matter, but sandyRiminiFound on some rims, not extensiveThin “A” horizon over wide sandy layer“B” horizon full of organic acidsPonzerDominant in large baysAnoxic, mostly organic matterThick Black, organic rich “A” horizon over loamy material
92 Carolina Bay Orientations Notable orientation was not realized until 1930’s and the advent of aerial photography. Smaller bays deviate more from preferred orientation.
93 Meteorites! Prouty (1952), Melton and Schriever(1933), etc. Meteorites coming in at a low trajectory from the northwest or one broke apart and debris fanned out over Carolinas.Impact direction pushed up sand into southeast rimsProblems: No meteoric material found, no shatter cones or SiO2 polymorphs, what about “ghost bays”? different ages of bays?
94 Comet: Eyton & Parkhurst, 1975 Refute marine ideas because Carolina Bay types were found in Va. Piedmont ’ above SL = no known marine terraces above 350’.Refute meteor or asteroid ideas after studying impact mechanics of Baldwin (1965) and determining that the crater would be roughly1000 feet deeprim heights of 150 feetrim width of 1000 feet
95 Carolina Comet Eyton & Parkhurst, 1975 Approached from NW, fragmentedCohesiveness of clay rich surficial sediments lessened crater depthVolatile content in nucleus of fragments caused them to explodeLed to shock waves which created depressions
96 “Tunguska event” did it happen again? June 30th, Near the Tunguska River, Siberia.Explosion leveled 2000 sq km of tundra and left felled trees radiating 9 miles from one area. Others left branchless.No meteorites found: Proposed that a small comet vaporized before impact, but the heat/energy caused by shockwave affected surfaceMany shallow, funnel shaped depressions left. By 1928 these were filled with swampy vegetationWeeks afterward sky was bright: comet tailKnocked guy off his porch 29 miles away
97 Modern Oriented Lakes Kacrowski, 1977 Found similar features in: East Texas, Chile and the North Slope of AlaskaWas able to recreate oriented bays with a wind machine and a sand boxBut: -Why do we need to go to the ends of the earth to find similar if it’s just winds?Why are winds in Carolinas able to do this?Soils anchored by roots are too stable for windsWhy has this process stopped?What about bays within bays and overlapping bays? (Savage, H., Mysterious Carolina Bays)
98 Artesian Spring Hypothesis Johnson, D.A. 1942 Vast amount of artesian springs eroded sediments or dissolved karst leaving a pool of surface water that appeared elongated as the artesian spring migrated along regional dip. Northwesterlies furthered the elliptical shape.
99 Carolina Bays and the Shapes of Eddies Cooke, C.W. 1954 Carolina Bays are of marine originOriginally hollows in marine terraceSand rims are bars / spits / dunes built by tidal eddies in former estuaries or tidal flats on Pleistocene age marine terraces.
100 Cooke Refutes:Artesian spring hypothesis: too many bays, bays are above artesian flow, too hard to maintain artesian head in surficial sedimentsRounding effects of waves: bays are too perfect, orientation is too perfectRotation of earth must be involved!
101 Tidal currents often create stationary eddies b/c they often flow into wide, quiet water bodies. Stationary eddies should leave impression on surface.Incoming tide scours sand and drops it in bars. Wave activity pushes it up into crescent beach ridge around the eddy, which may become vegetated.The eddy slows/stops with growth of beach ridge and the bay begins to silt and become marsh-like.A fall in sea level will result in transition into a freshwater bog, a Carolina Bay.
102 cot(bearing) = cos(lat) Gyroscopic EddiesFixedPrecessingb:a=sin(lat)b is oriented N450Wb:a=cos(lat)cot(bearing) = cos(lat)The rotation of the earth has a gyroscopic effect on already rotating bodies of water, or eddies, causing them to change shape from a circle to an ellipse.
103 Halfmoon Island, Chesapeake Bay,Va. Based on Cooke’s equations for a precessing eddy,at latitude 37049’ the ratio of long and short diameters should be 0.79, and direction of long axis should be N 51041’ W.
104 Halfmoon Island Chesapeake Bay, Va. Formed on “Silver Bluff” a late Pleistocene marine terrace named for oolite cliff in Biscayne Bay, Miami (called the Kapapa strand in Hawaii). SL was 6’ above 1954 level.Beach ridge 5’ above high tide, continues subaqueously. Narrow, 10’ deep channel in Thorofare, but you can wade out to it. Weak, clockwise drift observed on either side of channel.Bar was probably built when the eddy was stronger due to greater tidal range in Chesapeake which speeded currents (and eddies) in Pokomoke Sound.
105 New Constraints on the Evolution of Carolina Bays from GPR – Grant, J New Constraints on the Evolution of Carolina Bays from GPR – Grant, J.A. et al. 1998Savannah River Site: ~190 Carolina Bays preserved in 803 sq km. Bays are located along terraces and interfluves of the Savannah River.Most bays are small w/ a long axis of ~ m. Some have ponds of ha which may dry seasonally.Used GPR, Cores, and archeological data to track evolution of 4 Carolina Bays: Flamingo, Mona and Woodward, and Thunder Bays
106 Varying HyrdrologiesFlamingo Bay: innundated up to 164 cm in spring. Shallows through summer, fall.Thunder Bay: holds water for 6-9 mo., wettest in spring and summer.Mona / Woodward Bays: hold water for 3-6 mo., wettest in spring and summer.
107 VegetationInteriors dominated by aquatic or herbaceous wetland species: smartweed, American lotus, panic grasses, blackgum, etc.Basin-Rim transition zone has facultative hardwoods: sweetgum, red maple, blackgumRims are dominated by slash pine and loblolly pine plantations
108 Stratigraphy Bay interior Regional quartz sand sheet: Grades from sandy sediment with little organics interbedded with silt / clay near the edge to organic rich, silty clays of a Rembert sandy loam soil towards the centerBay fill is mostly mid to late Holocene in age.Regional quartz sand sheet:Thin (1-3m), moderate sortingAbsent from within bay, but thickens to SE side likely present before bay formation
109 Stratigraphy ~cont. Upland Unit underlies sand sheet. Poorly sorted, but finer than sand sheet.Surface lies above that of basin interiors (likely there before basin formation)Flat lying under east and south rims but outcrops on northern rim of Flamingo Bay excavation of sand sheet depression in upland unit and sand reworked into SE rims?
110 Grant’s ModelGPR indicates multiple reactivation surfaces on base of rim sedimentsEvolution didn’t involve much modification of the underlying Upland unitDuring fluctuating water conditions (though still open) sediments were exposed for deflation and rim accretionRim sediments were deposited into standing vegetation ESE facing parabolic dune w/ no stratification and moderate sorting
111 Grants Model ~cont.Slow erosion of shoreline from WNW side provided sediment for basin infillInfill led to colonization of emergent vegetation less open water time/year less wave E to modify shoreline rims stop accretingSome sediments transferred back into basin through alluvial activity (sand wedges found grading down to basin)
112 Grant’s ModelProblems: scouring of bay margins needs southwesterlies and parabolic rim on ESE needs northwesterliesAnswers:Southwesterlies dominate bay orientation b/c they are most common during spring and summer when water level is highest minimum exposure of sediments to wind.Northwesterlies are dominant during fall and winter when water levels are low more deflation and downwind rim accretion
113 Not to be confused with… GRANT, C A biological explanation of the CarolinaBays. Sci. Monthly 61:
114 Lake Waccamaw, NC Stager and Cahoon (UNCW), 1987 Largest of Bay lakes,marine bluffs along north shore, location at major river indicate tectonic genesis.Wind / Waves caused orientationColder winters during Pleistocene moist phase Ice pushed sand ridges upMultiple ridges multiple shoreline positionsGenesis at end of pleistoceneUnique due to endemic speciesFound to be young ~15,000 yBP = young for endemics
115 ConclusionCarolina Bays remain another wonder of the world. General belief seems to be that existing wet depressions were further scoured by winds into preferred orientation.Theories abound: None fully acceptedModern technology could break the storyMust protect them for further study
116 “Given a confident belief that the answers are indeed out there in the sand, we come then to the true shame of the Carolina Bay story: the willingness of the current geophysical research community to tolerate and admit such a profound ‘mystery’ in their midst….The study of the Carolina Bay origin is the ‘crazy aunt in the attic’ of the CoastalPlain researcher”-George Howard