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Single conduit Maze passages |
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(Plan view- Single conduit) Linear |
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(Plan view- Single conduit) Angulate |
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(Plan view- Single conduit) Sinuous |
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(Plan view- Maze passages) Network maze |
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a grid of intersecting passages; high, narrow cross sections |
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(Plan view- Maze passages) Anastomotic maze |
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curvilinear tubes of circular or elliptical cross section that intersect in a braided configuration |
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(Plan view- Maze passages) Spongework maze |
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interconnected non-tubular solution cavities of varied size and irregular geometry arranged in an apparently random 3D patterns |
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passages formed under hydraulic control |
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higher than wide, nearly vertical walls, little variation in passage width from top to bottom |
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(Cross section) Elliptical tube |
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groundwater flows under pipe - full conditions, wider than high Passage shapes controlled mainly by structure of surrounding bedrock Fissure Triangulate |
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(Cross section) Composite cross sections |
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cave passages preserve their earlier history in almost overwhelming detail |
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Speleothems Classification |
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Morphology - shapes - most frequent Origin - almost purposeless; origin can involve many mechanisms Crystal structure - probably most technically correct |
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Crystal growth controlled Shields Helictites Botryoidal Anthodites Oulopholites (gypsum flowers) Transistorites (spiders) |
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Explored the Lechuguilla cave in New Mexico - at 1,567 feet down, the deepest limestone cave in the US
Coined the term "phlegmball mats" to describe the living bacterial goo on the floors of acidic caves
Discovered the “buzzing passage” in Villa Luz |
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Co-lead, Cartographic Programmer Wakulla2 Expedition, 1998-1999. Created the first fully interactive 3D map of an underwater cave |
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an assistant professor of geology at Westminster College in Fulton, Missouri.
I never gave caves a thought until I explored one in King's Canyon National Park outside Fresno, California, with a college outing club |
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She and her colleagues on the SLIME (Subsurface Life In Mineral Environments) Team are investigating how microbes help form the colorful ferromanganese deposits that coat the walls
Lechuguilla Spider Cave Cueva de las Sardinas (Villa Luz) |
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what happens above ground happens below |
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adventure with a purpose fueled by passion for scientific intimacy getting closer, involved difference between ES and adventure: “when risking one’s life for science and exploration, danger is minimized in order to maximize the probability of achieving ones goals, not the other way around. ESs are not on the edge to see how high or far they can go but rather to document what they see along the way, and most important, to get extreme long enough, regularly enough, to draw some scientifically defensible conclusions in the process.” |
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know humans are capable of more than survival frontline advocates for what they study ammunition for proof “represent the informed voice of science to an often skeptical public.” |
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Flatworms, gastrotrichs, tardigrades, cladocerans, ostracods, mites, immature stages of various insects |
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Troglobionic carvernicoles |
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Gastropoda: ex. Snail, carychium exile Pseudoscorpion Ticks Acarina - mites: look like tiny spiders Harvestmen: daddy longlegs Arachnida: meta ovalis, meta menardi (europe); troglophile Amblypigidae: typically tropical; highly adapted; big and ugly; make noise when they move Insecta Diplura; small, long antenna, lack wings Thysanura (Bristletail): stay around entrances Collembola: Springtail; highly specialized troglobions Camel crickets (Ceuthophilus) Parthenogenesis: method of reproducing in which males are not needed Ovipositor: test soil for right makeup and injects eggs Coleoptera: beetle (neophanops, pseudoanophthalmus, leptodirus hohenwarti); some feed on cricket eggs Diptera: heleomyzidae, tipulidae (flies) |
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terrestrial “cave visitors” ex. bats, bears, raccoons, some snakes, crickets |
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aquatic “cave visitors” ex. crayfish, salamanders |
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few external cues; still evolving; ex. some salamanders |
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not supposed to be there; wander in by accident |
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Cavernicoles Life history characteristics |
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K strategies Longer duration of phases of life history Tendency to lose distinct reproductive cycles Longevity |
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Cavernicoles Development of reproductive strategies |
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Low fecundity Decrease in egg number Reproduce less often Increase in egg size |
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Troglobitic carvernicoles |
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Glow Worms: “fishing lines”; green/yellow glow, very bright; feed off adults Mycetophilidae: little worms that zip along mucous lines Millipedes Isopods: imported; adapt well; “rolly pollies” Urodela: plethodontidae; lizards/cave salamander, troglophiles Snakes: ectotherms Green frogs Phoebes (flycatcher); bird Ravens Turkey vulture (Carthartes aura): typically caves in cliffs; stay near entrance/in twilight area Chiroptera (bats): pipistrellus, myotis; make ceiling stains from oils on fur Cave rats (Neotoma): like packrats - steal something, but bring something back |
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scientific study of caves From Greek spelaion (cave) and logos (study) |
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Ancient Greeks of Mycenae |
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Myths tell of a cave as the birthplace of Zeus Greek hell (Hades) lay below ground; ferryman Charon rowed souls across the river styx into a land of eternal suffering |
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more than 10,000 - 1,000,000 BP Cave paintings |
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in mountainous areas, steep slopes leading to flat valley, with an entrance at both ends underneath it; good for planting crops In rainy season, underground area floods and eventually floods the entire polje |
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1669 - captain of merchant ship; math teacher; explored Pen Park Hole on the north side of Bristol, England In cave for more than five hours, and “was troubled with an unusual and violent Head-ach, which I impute to my being in that Vault.” |
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Baron Johann Weichard Valvasor |
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Actively explored caves in Slovenia An austrian, 1678 - 1689, his observations fully justify his recognition as the earliest true speleologist First to study area systematically Studied 70 caves Thought that dragons inhabited caves because of the discovery of the “babies,” white salamanders they called “olms,” which were actually amphibians. |
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amphibians once thought to be baby dragons
Largest stygobion in the world
1768 - Joseph Nicolaus Laurenti formally described the salamander Proteus - after Greek god… |
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Nicholas Thomas Bremontier |
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(french civil engineer) 1765 - surveyed Grotte de Miremont at Rouffignac First really accurate plan map - 27 passage cross-sections |
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1781 - produced one of the earliest american plan cave maps - Madison’s Cave 1799 - A Memoir on the Discovery of Certain Bones of a Quadruped of the Clawed Kind - first American description of bones in a cave |
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1865, jan 27 - first photographs of caves Blue Johns Caverns in Derbyshire, England - used magnesium wire |
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Ozarks First specimen of a blind fish in America |
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“lady geologist” from St. Joseph, Missouri |
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1850-1853 Early reputation as father of modern speleology
In the US 1806 - plan map of Madison’s Cave (recall Jefferson’s map)
1849 - began systematic study of caves in slovenia
1854 published the monograph “die grotten und hohlen von adelsberg, lueg, planina und laas” |
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introduced classical classification of cave animals into three categories |
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Most famous of cave explorers of 19th century Published widely but actually did little original |
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FATHER OF SPELEOLOGY Work from 1888-1914+ Immense amount of original exploration - native france and most of europe Mediterranean islands, russia, america Techniques and equipment - folding canvas canoe Surface pollution - subterranean pollution in karst areas/eater supplies 1890 - used “la grottologie” for scientific study of caves
Founder of Systematic cave exploration Scientific exploration Use of telephones French Societe de Speleologie What set him apart Meticulous preparations Systematic recording of all aspects of caves Tremendous physical ability Incredible courage Died in 1938 at age 78 Explored nearly 1500 caves His technical innovations had become standard equipment for other cavers Gave samples to Franz von Hohenwarth who sent them to naturalist Ferdinand Schmidt |
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1822 - described the cave salamander Collected specimens near KY |
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Described first cave fish as Amblophysis speleus - first troglo/stygobite in US |
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an energetic association of european research |
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1907 - fauna of Mayfield’s cave, IN |
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1909 - book on cave vertebrates of america |
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Jan 30 - trapped in Sand Cave Stuck 16 days |
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Fluorescein Rhodamine Optical brighteners Bill Jones |
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emerging stream- cuts through |
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comes down through epikarst and flows out |
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Tectonic process Processes associated with Biblical Flood |
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Usually limestone or other carbonate rock Derived in Slovenia German name for Kras, region in NW Slovenia, partially extending into Italy |
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limited geographic distribution |
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ice/glacier caves, lava tubes |
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Aquatic Subterranean Habitats |
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Primary source: stream, mudbank - permanent |
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a change in the environment brought about by living organisms, particularly by plant life |
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water from outside source |
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reemerging water source (disappearing/reappearing stream) |
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permeable; spaces between particles |
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drove animals underground as they moved over the landscape |
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fed by organic matter coming in from outside |
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CaCO3 stratified layers of organic matter |
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species that share specific traits (i.e. no eyes, lack of pigment, etc.) |
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retreats into caves when dry; has pigment and eyes; leave caves by November |
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orange, stripes (long-tail salamander) or speckles; has eyes; stays near cave entrance to feed on crickets |
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rarely seen in caves because they are ectothermic (cold-blooded) |
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use caves as nurseries; insectivorous - control pests; guano serves as base for food web |
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endangered species; found in only eight caves in the world; hibernate in caves - are sensitive to disturbance |
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inland body of water connected to the ocean |
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study of cave-dwelling life - cavernicoles |
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Population growth curve J-shaped, S-shaped Population growth = dN/dT = rN(K-N/K) D=delta=change; r=biotic potential; K=carrying capacity; N=number of individuals; T=time Late maturity Low reproductive rate - to reproduce may be too expensive Large size at hatching Increased longevity |
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Strong reduction in or total absence of pigmentation Reduced eyes Attenuated appendages Increase in tactile and chemical senses Increase in metabolic economy Increased number of adaptations to reduce desiccation Development of paedomorphic forms Reduction in various behavioral traits |
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Selected species Rapid population growth - unstable |
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Descent with modification Species arise from preexisting species Gradual change in from and function |
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exchanging genes over space and time |
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Differential reproduction |
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evolution proceeds gradually with progressive change Slow rate of speciation Darwin |
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evolution occurs in spurts |
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1795 Geological gradualism |
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profound change on earth is the cumulative product of slow but continuous processes |
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1809 Inheritance of acquired characteristics: use and disuse Assumed acquired characters were inherited |
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1769-1832 Catastrophism Boundaries between fossil strata correspond in time to catastrophic events- floods, drought Destroy many species Repopulate by immigration or by Special Creation |
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species immutable - did not support concept of evolution |
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the theory that changes in the earth's crust during geological history have resulted from the action of continuous and uniform processes. |
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top layer of limestone (subcutaneous zone) |
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4th century BC – recognized cave but did not know how to explain them |
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erosive power of surface water |
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strong believer in speleogenesis by stream action (vadose) |
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elliptical – grows outwards longways |
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downcutting “keyhole” shape |
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maintained erosion alone sufficient to form caves |
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believed a combo of both vadose and dissolution and erosion |
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considered phreatic dissolution the principal factor |
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caves are formed by the action of flowing water either at or above the water table infiltrating surface water is a vert aggressive and the aggressiveness is quickly lost as the water passes into the saturated zone solution thus takes place most actively at the top of the saturated zone water dissolves sinkhole drains, vertical shafts, and solution chimneys until it reaches the top of the saturated zone turn and flow horizontally along fractures |
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solution takes place in the phreatic zone upon reaching the water table, groundwater continues toward its outlet along flow lines that curve deeply into the phreatic zone when regional uplift occurs, water table is lowered and gradually the upper levels of the cave become air-filled at this stage dripstone deposits (speleothems) form |
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shallow as opposed to deep |
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(1932): impressed by the observation that most cave passages are nearly horizontal and some seem to be stacked in levels hypothesized that caves form in the interval between the high and low stands of the water table as it fluctuates between wet and dry seasons |
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Mixing Zone and Halocline caves |
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solution can occur by mixing waters saturated at different carbon dioxide partial pressures this mixing corrosion provides another mechanism for bedrock dissolution deep within a limestone mass mixture of carbonate saturated fresh water with arbonate saturated salt water prodices an undersaturated solution capable of further dissolution cave development also takes place in the active mixing zone along the halocline in coastal karst called mixing-zone, halocline, or flank-margin caves |
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upwelling of deep source of thermal waters- quite different from caves formed from cold groundwater- often associated with ore deposits – large maze caves in the Black Hills of South Dakota |
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one source o sulfuric acid is the oxidation of sulfide minerals, mainly pyrite, that occur dispersed in many carbonate rocks |
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