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Increasing production of economically valuable limestone through paleontological interpretation of the fossil Record.
(1996). Ralph Cavallo, Anthony Cinelli – Florida Atlantic University (FAU)
The researchers hypothesize that the subject quarry may be able to increase it’s output of economically valuable limestone by mining to a slightly greater depth. The data will indicate topographic relief which is not visible at the surface but readily apparent in the sedimentary environment in which the strata were deposited. The researchers believe a biological reef deposit lies below what is now the base of the quarry. This would provide a large amount of quality aggregate.
Key Words: Bermont, Caloosahatchee, Gastropod, Lake Okeelanta, Molluscan, Nifo, Okeechobeean.
The GKK quarry is located in central Palm Beach county. GKK produces sand, concrete aggregate, roadfill, and clean fill for a variety of uses and consumers. There are twenty distinct layers from the top to the bottom of the Quarry. To distinquish the Units found in the quarry, the term Palm Beach Unit will be used for the purpose of this paper. The Units are abbreviated as ‘ PB Unit’ or ‘PBU’. The .1m of top soil (PB Unit 1) is scraped from the surface exposing 2-3 m of white sand. This sand is approximately 70% silica (PB Unit 2). Beneath the sand is a layer of clay sized particles that appears to have been weathered from the limestone immediately below it ( PB Unit 3). This .1m thick layer has produced the few large mammalian fossils that have been recovered. The bones have been leached and are atypical of the density one would exspect from bones that have been replaced by mineral processes. The lower portion of the bones were encased in the .6m thick, underlying, massive, and sandy micritic limestone (PB Unit 4). This micritic limestone grades rapidly into a Fort Thompson molluscan faunal assemblege which is loosely consolidated. Palm Beach Unit Five (PB Unit 5) is similar to Unit 4, beginning with a consolidated layer and grading into less consolidated shells. The Unit is 5m thick, beginning with a solid layer of bivalves which are comprised mostly of the Genus Chione. Then, the Unit grades into a .9m thick loosely consolidatedand more diverse Bermont molluscan fauna (PB Unit 6). Unit seven (PB Unit 7) is a massive micritic limestone .1m thick. Unit eight (PB Unit is a .3m thick lime mud with shell fragments. Unit nine (PB Unit 9) is .2m thick and resembles Unit 6. Rose coral and back reef fauna typify Unit 10 (PB Unit 10). Molluscan shell material make up the loosely consolidated bioclasts of the .4m thick Unit Eleven (PB Unit 11). The next strata is .4m thick massive lime mud (PB Unit 12). Palm Beach Unit Thirteen (PB Unit 13) is a layer 1.8m thick consisting primarily of bivalves and gastropods. Unit Fourteen (PB Unit 14) is a layer .2m deep that is nearly solid and consisting of Chione clams. The Lake Okeelanta (Petuch,1988) Unit (PB Unit 15) is a layer which varies from .1m thick in the western wall to nearly pinching out and becoming impoverished on the eastern wall. Brian Schnirel in the early to mid 1990’s researched and mapped out the stratigraphy of the Palm Beach Rock Quarry which is now closed. This quarry was only 1 mile to the east of the GKK quarry. Absolutely no evidence of Lucustrine marls or associated fossils were ever found giving credence to the eastern shore of Lake Okeelanta existing at the eastern portion of GKK. Additional evidence of land fauna at higher levels of the Palm Beach rock quarry material gives evidence of infilling. A chain of islands (Petuch,1992) existed along the east coast of Florida bordering either the Okeechobean Sea (Petuch, 1986) or Lake Okeelanta depending on glacial eustatics. The infilling to the east of GKK gave rise to the island named Loxahatchee Island (Cavallo, Cinelli 1996) in honor of the township it lies near. The freshwater Lucustrine and terrestrial fauna of Unit Fifteen is comprised of species of the Genus: Pomacidae and Seminolina. Occasionally, a mangrove root is found. The Seminolina assemblage consists almost exclusively of planorbid forms and no sclariform species. Brian Schnirel, following research by Dr. Ed Petuch, has researched this species and material from deep water formations many miles to the west along Route 27 near South Bay, Florida. In his research of deeper lucustrine layers, the reverse is true. Sclariform species not only predominate, but quite elongated. Planorbids can be found but usually comprise of a single species: Seminolina zyggorat (Petuch, Schnirel 1995) which seems to occupy a niche in deeper water that other planorbids find difficult to adapt to. In the deeper areas of Lake Okeelanta, the calcarious marls vary from a tan to dark chocolate brown. Fossils within these marls can be extremely numerous and generally comprise about 70% of the matrix. In the eastern shoreline environment near Loxahatchee Island, the GKK lucustrine material is nearly a 100% fossil conglomerate. This is due to the combination of the prolific nature of the planorbids, wave action carrying dead individuals for depositon along the shore, and little deposition of sedimentation being a near shore environment. The wave action of this enormous lake does not seem to be overly strong however. This is based on the lack of a Thanatocoenosis of the GKK fossil material. Below the base of BPU 15, the last of the gastropod genus Pyrazisinus to creep in the mud are found. This previously undescribed species of Pyrazisinus is an indicator of brackish water and shallow muddy bottom environment that ended as PBU 16 gave way to PBU 15. This environment changed to a freshwater environment as a result of a drop in sea level due to a glacial episode. Below PBU 15 is a .3m deep layer cocsisting of typical loosely consolidated Bermont bioclasts (PB Unit 16). Below this layer (PB Unit 17) contains .3m of consolidated bioclasts primarily of Chione clams. In the quarry, the employees of GKK call the material out of next unit (PB Unit 1 "shit rock". It consists of semiconsolidated mudstone. The color ranges from black to brown, the rock is hard and fractures when struck. However, when it is crushed and washed, it disintegrates. The fabric of the rock is an organically rich mud with a few marine gastropods within the layer. Below this, is a layer of Chione clams .2m thick (PB Unit 19). Lower still (PB Unit 20) is .3m of the infamous "s–t rock". At the bottom of PBU 20 is a layer (PB Unit 21) of marine bioclasts including fossils indicative of the top of the Caloosahatchee fauna. Mining Operations: The land purchased for the intention of mining limestone was first surveyed by one of the owners, James A. Comyns (M.S. Civil Engineering). Based on his findings, equipment was brought in to take several hundred core samples from all over the property. Samples were sent to laboratories to determine the chemical content of the limestone and Los Angeles abrasion of the sand. To determine the continuity of the strata across the property, a radiation permit was secured and gamma log testing was performed. The testing indicated contiguous layers of rock. Subsequently, a crushing plant was built, drainage canals were dug, and the topsoil wa scraped away. The thick layer of quartz sand was mined for a variety of uses. Once the overburden is removed, a portable tracked drilling rig is used to drill to 6m depth using a compressed air slurry. The holes vary in number from 30 to nearly 300 depending on the need for rock. They are filled with a ‘Nifo’ (Nitrogen and Fuel Oil). (This mixture is similar to the compound used in the Oklahoma city federal building bombing.) In addition, the holes are filled with foam and detonator. The explosive filled holes are detonated simultaneously. This produces a large zone of rock that is fractured enough to allow the large earth moving equipment to remove it for processing. The rock is taken to the processing plant where the rock is crushed, washed, and sorted by size. The sorting of size is based on the ultimate use of the stone. Once the rock fractured by the blasting has been removed, what is now the floor of the quarry is blasted. Contained in this layer of fractured rock are the two layers of "shit rock". A washing process is not used on this rock as it maintains it’s hardness best when dry. This rock is used as base fill for roads primarily. The edges of the pit are dug to a slightly greater depth, creating a drainage canal. The water is removed from the bottom of the pit by several diesel/ hydraulic pumps with 12 inch discharge pipes into drainage canals that run the length of the property. Water for the processing plant is obtained exclusively from this drained water. The discharge from the plant flows into an abandoned pit where it is slowly being filled in with clay sized particles. This pit being filled with water is adjacent to a working pit. The hydrodynamic head forces water through the rock. The forced water separates the pits where it is filtered naturally and recycled as it flows into the catch canal at the bottom of the pit. Any excess water is released to the surrounding agricultural area or to the West Palm Beach canal. Occasionally, isolated pockets of connate water are struck, this saline water is circulated around the quarry until it is diluted to environmentally acceptable levels. Increasing output through Paleontology: The quarry is different from others in the area in that the sand is plentiful, and the quality of the aggregate is high. the owners were forced to build a test road bed by the florida department of transportation because they were incredulous even to laboratory reports. This begged the question: "why is this here?". The answer becomes apparent when we consider the data. (speaking of roads, since at least some of the owners were british, the main roads into GKK were driven in english fashion. that is, on the left side of the road. the east side of the roads always were in the worst shape with major ruts as the trucks leaving on the left side of the road were carrying heavy loads of fill.) The faunal types present are generally medium to shallow depth organisms. The flora most often found in the fossil record here are mangroves. The lakeokeelanta formation gradually pinches out fron west to east. That data, combined with the fairly abundant mammalian fossils has led the researchers to conclude that a paleoisland existed from the aftonian to sangamonian stage. The researchers theorize that the underlying rock on which the island grew consists of a biological reef of calabrian and piacenzian age. if this the case, the amount and quality of economically valuable limestone should meet or exceed that which has been mined from the bermont layers. The modern topography, especially of the canals which were dug to take advantage of the natural low relief, demonstrates that the areas of palm beach county that produce quality stone are found in conjunction with these areas. The natural pleistocene inlets which fed the okeechobean sea brought in nutrient, rich, warm, clean water that accelerated reef growth. at time of lower eustatic levels, the reefs became islands similar in faunal type to the florida keys. This being the case, an even more substantial layer of carbonates waits just below the floor of the quarry. Time however, for any quarry in south florida is limited. The great push by developers and politicians to develop any accessible land usually results to quick zoning changes to residential or commerical. More likely than not, instead of exploration of the deeper layers, the GKK site will most likely become a zero lot line housing community.
Cavallo, Ralph. Personal research.
Cinelli, Anthony. Personal research.
Petuch, Edward. Atlas of Florida fossil shells. (1994) Chicago spectrum press. Evanston, Illinois, U.S.A. 394 pp.
Edge of the fossil sea. (1992)
Bailey Matthews. Shell museum. 80 pp. Personal Communication.
Schnirel, Brian personal communication.
Addendum by Brian L Schnirel:
This was the culmination of many years of research by all parties. The Palm Palm Beach Rock quarry site mentioned in the report was investigated by myself alone. I had carte blanche in accessing that quarry by the property owners. I conducted a complete stratographic assessment of the area and collected many samples, including a hystravasum that was used as a holotype for a new species by Edward Petuch. All the stratographic records and boxes of sample material from the Palm Beach rock quarry section were placed in the "T" buildings (these buildings were part of a military base in WW2 along an airfield before converted to scientific research centers) at Florida Atlantic Unversity. Unfortunately, a facility member who had no knowledge of the value of the material, tossed it away to make room for an engineering center. As mentioned by the authors, no Lake Okeelanta material was found at that site which establishes the eastern shoreline of that paleolake.
Brian L. Schnirel
Source: POlYPHEMOS May 2004 Volume 1 Issue 2
Manuscript contributed by Brian – LCRC. Accepted on March 28, 2007.