Knowledge (XXG)

Tar pit

Source ๐Ÿ“

224:. These oil deposits were formed during the Miocene Epoch when marine plankton organisms accumulated in an ocean basin. Over time, sediments buried the organisms 300 to 1000 meters below Earth's surface, subjecting them to high pressures. This process turned the organic matter into oil. The 6th Street Fault that cuts through the Salt Lake Oil Field is the conduit that feeds the La Brea Tar Pits. Petroleum migrated to the surface over time, trapping and preserving animals and plants for the past 50,000 years. 494:. The La Brea Tar Pits emit about 500 kg of methane per day. The emissions are the highest along the 6th Street Fault, which is the conduit that feeds the tar pits with crude oil from the sediments underneath Earth's surface. It was also discovered that methane is evaporating out of the nearby soil, affecting the physiology of the native grasses. The La Brea Tar Pits have the highest natural gas flux measured for any onshore seepage zone in the United States. On a global scale, geologic CH 44: 33: 187:. At the surface, these light molecules may evaporate out of the crude oil, leaving behind the heavier, stickier molecules. Asphalt, or bitumen, usually contains hydrocarbon molecule chains with 50+ carbon atoms. The longer the hydrocarbon chain, the more viscous it becomes, and the boiling point increases.   354:
and other petroleum products. The origin of the bacteria in these natural asphalt pits is unknown, but it is believed that they evolved from preexisting soil microorganisms that survived an asphalt seepage event thousands of years ago. The soil microorganisms had to adapt and undergo genetic changes
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Tar pits are characteristic of their many fossils. This is the case because the thick, sticky asphalt traps animals.  Once animals step into the tar, they become immobilized and begin sinking immediately if the asphalt is warm and sticky enough. Predators that see these helpless animals usually
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A woman's body was recovered from the La Brea Tar Pits in 1914.  Only the skull and parts of the skeleton were preserved, and she was determined to have died about 9,000 years ago.  She was between the ages 18โ€“24 at death, and she was 4 feet and 8-10 inches tall. This is the only reported
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are located in Tar Pits Park in Carpinteria, California. These tar pits were predicted to have formed during the Pleistocene. During an excavation project, 25 plant species were recovered along with 55 species of birds and 26 species of mammals. Springs of tar still ooze to the surface through
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is subjected to pressure underground. If this crude oil seeps upward via fractures, conduits, or porous sedimentary rock layers, it may pool up at the surface. The lighter components of the crude oil evaporate into the atmosphere, leaving behind a black, sticky asphalt. Tar pits are often excavated
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Evaporation is an important process in the formation of tar pits. A reservoir of light crude oil on Earth's surface can be reduced by up to 75% of the initial volume just after a few days, forming asphalt as the resulting product. For medium crude oils, the volume may be reduced by 40%. Crude oils
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For thousands of years, Native Americans used tar from the La Brea Tar Pits as an adhesive and binding agent. They would use it as waterproof caulking to line their boats and baskets. When Europeans arrived at the tar pits, they began mining and extracting the tar for roofing material in nearby
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The bones and hard parts of the animals are well preserved because they are buried rapidly after the organism's death. Beneath the surface, the hard parts are engulfed with asphalt, and they are protected from climate variations like rain, wind, or snow that may accelerate weathering processes.
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is a large, bowl-like depression filled with bitumen. The lake has a maximum depth of 250 feet with an area of 100 acres, making it the largest deposit of solid bitumen on Earth. The lake is cold and dense near the shores, and it has a top layer that can be walked on. Underneath this skin, the
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Pitch Lake formed thousands of years ago in the presence of tectonic activity. Movement along a fault created a fracture that tapped into an oil and gas reservoir deep within the crust. The oil and gas seeped upward to Earth's surface through the fracture over time, creating Pitch
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An anticlinal trap is feeding the tar pit on the surface through the vertical fracture in the strata (indicated by the red arrow). Once the crude oil reaches the surface, evaporation takes place and lighter hydrocarbons are vaporized, leaving behind sticky
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environments. It is also hypothesized that the wetter climate during the Last Glacial Period may have increased the nitrogen availability to plants, which therefore increased the concentration of nitrogen in leaves. This change may have increased the
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In the La Brea Tar Pits, more than one million bones have been recovered since 1906. 231 vertebrate species, 234 invertebrate species, and 159 plant species have been identified. The most frequent large mammal found in the La Brea Tar Pits is the
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asphalt is continuously churning. The lake gets gradually softer and hotter near the center where the bitumen begins to bubble. The gas being released in the middle of the lake is largely methane and an ample amount of carbon dioxide.
1515: 560:, only about a mile north of the La Brea Tar Pits. This methane pocket created an explosion that injured 21 people. This event increased awareness of the potential dangers of methane pockets and hydrocarbon seepage in the area. 543:
The natural geologic sources of methane and other hydrocarbons should be considered when modeling atmospheric greenhouse gases. Not all sources of hydrocarbons in the atmosphere are a result of anthropogenic emissions.
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Schulze-Makuch, Dirk; Haque, Shirin; de Sousa Antonio, Marina Resendes; Ali, Denzil; Hosein, Riad; Song, Young C.; Yang, Jinshu; Zaikova, Elena; Beckles, Denise M.; Guinan, Edward; Lehto, Harry J. (April 1, 2011).
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have been found living in microliter-sized droplets of water recovered from the lake. The biomass in Pitch Lake lake was reported up to 10 cells per gram of asphalt. Many of these microbes survive on sulfur, iron,
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will evaporate differently depending on their chemical composition. The average composition of a bitumen sample by weight is 80.2% carbon, 7.5% hydrogen, 7.6% oxygen, 1.7% nitrogen, and 3.0% sulfur.
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was similar between glacial and modern trees. Since the amount of carbon dioxide during the Last Glacial Period was between 180 and 200 ppm (409.8 ppm today), there was less carbon available for
269:. A well-preserved horse skull was also found in the Binagadi asphalt lake. It is estimated to be 96-120 thousand years old. It is on display at the Natural-Historical Museum of Azerbaijan in 297:
Lake. Due to this constant replenishment of the oil and gas, the lake has a slight current.  The current is largely unnoticed because the top layer of Pitch Lake is mostly solid.
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Weber, Derek; Marquez, Bertha A.; Taylor, Charnise; Raya, Paul; Contreras, Paul; Howard, David; Nwachuku, Ikenna; Fusco, Katie; Morales, Fernanda; Doezema, Lambert A. (September 1, 2017).
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concentrations in the atmosphere. This response to fluctuating carbon levels is seen in plants over time. For example, increased stomatal conductance is observed in modern
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data for trees that have fallen into the asphalt. Looking at carbon isotope data in prehistoric trees can reveal information about plant responses to different amounts of
483:), evaporate, leaving behind larger hydrocarbons that make up the chemical composition of asphalt. This is a concern because methane, ethane, and propane are either major 143:. Heteroatom compounds are organic molecules that contain elements that are not carbon or hydrogen, while hydrocarbons contain only carbon and hydrogen. Crude oil is less 506:
emissions estimates from gas seepage in sedimentary rock are in the order of 50-70 Tg/year and 2-4 Tg/year respectively. These values are roughly half of the global CH
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would advance into the tar pits with the hope of catching their next meal. As a result, prey are usually found beneath the predator during excavation projects.
99:, it is considered an anticlinal trap. The figure in this section is a cartoon cross-section diagram that shows oil stuck in an anticlinal trap. If there is a 552:
Hydrocarbon seepage in urban or industrialized areas present a geologic hazard due to the explosive nature of hydrocarbons. On March 24, 1985, a pocket of
435:. The discovery of extremophiles in Pitch Lake provides insight into the possibilities for microbial life in the hydrocarbon lakes that are found on Titan. 346:. Hundreds of new species of bacteria were discovered that have the ability to thrive in environments with little to no water or air. They contain special 123:
Tar pits are pools of asphalt. However, at the beginning of their formation, they were not always sticky and dense. The pools were composed of
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or in tectonic regions where the land is bending and folding. If the structure above the concave-down fold (arch) is a non-porous rock or
427:, or other hydrocarbons. Ongoing research is being conducted in Pitch Lake because it mimics the environment found on the surface of 758: 817: 519: 614:
was higher during this period to increase their carbon consumption. When moving into the following Interglacial Period, the
1269: 540:/year. These hydrocarbon emissions can be contributed to oil biodegradation and methanogenesis within the tar pits.   1089: 871: 147:
than asphalt because it contains a higher percentage of light hydrocarbons. Light hydrocarbons include the following
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passed through a small opening between the floor slab and foundation walls of a Ross clothing department store in
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family. These bacteria are known for being some of the most radiation-resistant organisms on the planet.  
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were recovered from the La Brea Tar Pits, and they revealed that the ratio of intercellular and atmospheric CO
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were also abundant. Additional fossils are constantly being discovered through continued excavation projects.
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uptake to survive under limiting carbon conditions. It is likely that the treesโ€™ stomatal conductance and
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in which each half of the fold dips away from the crest. Such structures are usually developed above
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to help tolerate the harsh, new environment, which ultimately gave rise to new bacterial species.
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Gerhart, Laci M.; Harris, John M.; Nippert, Jesse B.; Sandquist, Darren R.; Ward, Joy K. (2012).
1357: 1315: 1046: 932: 140: 104: 1590: 1582: 1545:"Preliminary Report on the Discovery of Human Remains in an Asphalt Deposit at Rancho la Brea" 1497: 1489: 1419: 1349: 1341: 1250: 1232: 1038: 924: 764: 754: 418: 327: 217: 1390:"Emission of Methane and Heavier Alkanes From the La Brea Tar Pits Seepage Area, Los Angeles" 1142: 1572: 1564: 1479: 1409: 1333: 1240: 1222: 1030: 916: 746: 396: 343: 262: 205: 168: 112: 79:. In fact, about 80 percent of petroleum found on Earth has been found in anticlinal traps. 577: 412: 100: 76: 846:"2.5: Hydrocarbon Types | PNG 301: Introduction to Petroleum and Natural Gas Engineering" 1560: 1405: 1329: 1218: 1026: 912: 43: 1303: 1245: 1202: 595: 573: 569: 484: 375: 221: 68: 750: 1633: 1484: 1467: 1050: 936: 488: 444: 1361: 568:
Tar pits are excellent preserving agents, and they also have the ability to provide
1468:"Glacial trees from the La Brea tar pits show physiological constraints of low CO2" 1167: 678: 432: 88: 897:"Macroseepage of methane and light alkanes at the La Brea tar pits in Los Angeles" 845: 32: 1114: 1034: 358:
In one study, the predominant bacteria found in the La Brea Tar Pits were of the
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Asphalt also lacks oxygen and water, so major decomposing organisms like aerobic
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as their reducing agent. Other bacteria discovered in the tar pits were of the
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above the oil reserve, the oil may migrate to the surface. This is possible by
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Proceedings of the Eighteenth Arctic Marine Oilspill Program Technical Seminar
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at the surface. The lighter hydrocarbons of the crude oil, which include
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Life was found in a ca. 28,000-year-old sample of natural asphalt in the
92: 37: 1203:"Microbial Diversity in Natural Asphalts of the Rancho La Brea Tar Pits" 261:. This tar pit is known for preserving the heads and bodies of multiple 75:
Tar pits form above oil reserves, and these deposits are often found in
472: 452: 424: 391: 160: 152: 60: 1090:"Pitch Lake, Trinidad - a geological wonder that is mined for asphalt" 322:, one of the most famous prehistoric carnivores that lived during the 460: 428: 387: 379: 347: 331: 164: 156: 148: 108: 171:. Crude oils may also contain some inorganic impurities, such as CO 1320: 788:"Chemical Constitution of Crude Oil | FSC 432: Petroleum Refining" 311: 237:
fractures in the underlying stratigraphic layers of marine shale.
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that originated below Earth's surface. Crude oil is a mixture of
270: 212:. The petroleum that is seen on the surface is sourced from the 1516:"Climate Change: Atmospheric Carbon Dioxide | NOAA Climate.gov" 709:"Earth's physical resources: Petroleum: View as single page" 622:
decreased as a result of higher temperatures and higher CO
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treesโ€™ stomatal conductance and chloroplast demand for CO
960:"La Brea Tar Pits and Hancock Park | La Brea Tar Pits" 1009:
Gimranov, Dmitry; Kosintsev, Pavel (April 30, 2020).
1201:Kim, Jong-Shik; Crowley, David E. (July 15, 2007). 818:"Chemicals from Oil | S-cool, the revision website" 374:. Purple sulfur bacteria do not use water as their 648:instance of human remains found within tar pits. 1388:Etiope, G.; Doezema, L. A.; Pacheco, C. (2017). 1011:"Quaternary large mammals from the Imanay Cave" 683:University of California Museum of Paleontology 72:because they contain large fossil collections. 1442:"Concern for Methane Hangs Over Fairfax Area" 8: 1394:Journal of Geophysical Research: Atmospheres 1073:Azerbaijan Association of Medical Historians 1304:"Microbial Life in a Liquid Asphalt Desert" 1066:"Horses of Azerbaijan: A Historical Survey" 253:, or in the Caucasus, a region between the 115:and because oil is less dense than water. 1576: 1483: 1413: 1319: 1244: 1226: 733:Dusseault, Maurice B. (January 1, 2004). 1268:Madhusoodanan, Jyoti (August 8, 2014). 661: 528:, which are approximately 100-150 Tg CH 370:order, more simply referred to as  63:deposits. They form in the presence of 1538: 1536: 1461: 1459: 1457: 1455: 1435: 1433: 1383: 1381: 1379: 1377: 1375: 1373: 1371: 1296: 1294: 1292: 1207:Applied and Environmental Microbiology 1137: 1135: 1196: 1194: 1192: 1190: 1188: 1084: 1082: 982: 980: 954: 952: 950: 948: 946: 673: 671: 669: 667: 665: 7: 890: 888: 840: 838: 812: 810: 808: 782: 780: 778: 739:Elsevier Geo-Engineering Book Series 703: 701: 699: 216:reservoir and the oil sands in the 639:treesโ€™ photosynthetic capacities. 265:, a mammal that flourished in the 25: 1543:Merriam, J. C. (August 7, 1914). 439:Contributions to greenhouse gases 1485:10.1111/j.1469-8137.2011.04025.x 901:Journal of Atmospheric Chemistry 167:. These molecules have very low 67:, which is created when decayed 872:"The Evaporation of Oil Spills" 1143:"Fossils - Window to the past" 881:– via McGill University. 643:History of tar pits and humans 1: 1609:"La Brea Woman - Los Angeles" 751:10.1016/S1571-9960(04)80101-0 1119:UNESCO World Heritage Centre 1035:10.1016/j.quaint.2020.01.014 1569:10.1126/science.40.1023.198 443:Tar pits are formed by the 55:, sometimes referred to as 36:Tar pit at Tierra La Brea, 27:Asphalt pit or asphalt lake 1666: 1094:National Museums Liverpool 564:Key to paleoplant behavior 1064:Alakbarli, Farid (2016). 921:10.1007/s10874-016-9346-4 406:, another asphalt pit in 314:and bacteria are absent. 1015:Quaternary International 1440:Clayton, Janet (1985). 1400:(21): 12, 008โ€“12, 019. 1270:"Microbes in a Tar Pit" 850:www.e-education.psu.edu 792:www.e-education.psu.edu 602:trees had to enhance CO 382:is not produced during 987:Griggs, David (2014). 372:purple sulfur bacteria 49: 40: 1338:10.1089/ast.2010.0488 870:Fingas, Merv (1995). 247:Binagadi Asphalt Lake 241:Binagadi Asphalt Lake 46: 35: 1415:10.1002/2017JD027675 1228:10.1128/AEM.01372-06 1115:"La Brea Pitch Lake" 386:. Instead, they use 350:that can break down 234:Carpinteria Tar Pits 228:Carpinteria Tar Pits 85:stratigraphic layers 1578:2027/uc1.c045791729 1561:1914Sci....40..198M 1406:2017JGRD..12212008E 1330:2011AsBio..11..241S 1219:2007ApEnM..73.4579K 1027:2020QuInt.546..125G 913:2017JAtC...74..339W 588:Last Glacial Period 548:Dangers of tar pits 408:Trinidad and Tobago 361:Gammaproteobacteria 290:Trinidad and Tobago 214:Salt Lake Oil Field 141:inorganic compounds 679:"La Brea Tar Pits" 532:/year and 6-8 Tg C 328:saber-toothed cats 50: 41: 1645:Petroleum geology 1613:www.laalmanac.com 1555:(1023): 198โ€“203. 1446:Los Angeles Times 1213:(14): 4579โ€“4591. 1147:ucmp.berkeley.edu 431:โ€™s largest moon, 419:Enterobacteriales 169:molecular weights 107:in the overlying 16:(Redirected from 1657: 1624: 1623: 1621: 1619: 1605: 1599: 1598: 1580: 1540: 1531: 1530: 1528: 1526: 1512: 1506: 1505: 1487: 1463: 1450: 1449: 1437: 1428: 1427: 1417: 1385: 1366: 1365: 1323: 1298: 1287: 1286: 1284: 1282: 1265: 1259: 1258: 1248: 1230: 1198: 1183: 1182: 1180: 1178: 1172:igws.indiana.edu 1164: 1158: 1157: 1155: 1153: 1139: 1130: 1129: 1127: 1125: 1111: 1105: 1104: 1102: 1100: 1086: 1077: 1076: 1070: 1061: 1055: 1054: 1006: 1000: 999: 993: 984: 975: 974: 972: 970: 956: 941: 940: 892: 883: 882: 876: 867: 861: 860: 858: 856: 842: 833: 832: 830: 828: 822:www.s-cool.co.uk 814: 803: 802: 800: 798: 784: 773: 772: 730: 724: 723: 721: 719: 705: 694: 693: 691: 689: 675: 485:greenhouse gases 397:Rubrobacteraceae 344:La Brea Tar Pits 338:Living organisms 206:La Brea Tar Pits 200:La Brea Tar Pits 195:Notable tar pits 113:capillary fringe 77:anticlinal traps 21: 1665: 1664: 1660: 1659: 1658: 1656: 1655: 1654: 1630: 1629: 1628: 1627: 1617: 1615: 1607: 1606: 1602: 1542: 1541: 1534: 1524: 1522: 1520:www.climate.gov 1514: 1513: 1509: 1472:New Phytologist 1465: 1464: 1453: 1439: 1438: 1431: 1387: 1386: 1369: 1300: 1299: 1290: 1280: 1278: 1267: 1266: 1262: 1200: 1199: 1186: 1176: 1174: 1166: 1165: 1161: 1151: 1149: 1141: 1140: 1133: 1123: 1121: 1113: 1112: 1108: 1098: 1096: 1088: 1087: 1080: 1068: 1063: 1062: 1058: 1008: 1007: 1003: 991: 986: 985: 978: 968: 966: 958: 957: 944: 894: 893: 886: 874: 869: 868: 864: 854: 852: 844: 843: 836: 826: 824: 816: 815: 806: 796: 794: 786: 785: 776: 761: 732: 731: 727: 717: 715: 707: 706: 697: 687: 685: 677: 676: 663: 658: 645: 633: 630:grown in low CO 625: 621: 613: 605: 593: 586:trees from the 578:paleoatmosphere 566: 550: 539: 535: 531: 518:emissions from 517: 513: 509: 505: 501: 497: 482: 478: 470: 466: 458: 441: 413:Burkholderiales 390:in the form of 340: 326:. 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Index

Asphalt seeps

Trinidad

asphalt
petroleum
organic matter
anticlinal traps
Anticlines
stratigraphic layers
thrust faults
aquitard
shale
fault
fracture
strata
capillary fringe
crude oil
heteroatom
hydrocarbons
metals
inorganic compounds
viscous
alkanes
methane
ethane
propane
butane
molecular weights
La Brea Tar Pits

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