| La Brea Tar Pits | |
|---|---|
Methane gas bubble emerging at La Brea Tar Pits (2004) | |
| Location | Hancock Park,Los Angeles, US |
| Coordinates | 34°03′46″N118°21′22″W / 34.0628°N 118.356°W /34.0628; -118.356 |
| Official website | |
| Official name | Hancock Park La Brea[1] |
| Reference no. | 170 |
| Designated | 1964 |

La Brea Tar Pits comprise an activepaleontological research site in urbanLos Angeles.Hancock Park was formed around a group oftar pits where naturalasphalt (also called asphaltum, bitumen, or pitch;brea in Spanish) has seeped up from the ground for tens of thousands of years. Over many centuries, the bones of trapped animals have been preserved. TheGeorge C. Page Museum is dedicated to researching the tar pits and displaying specimens from the animals that died there. "La Brea Tar Pits" is a registeredNational Natural Landmark.

Tar pits are composed ofheavy oil fractions, calledgilsonite, which seep from the earth as oil.Crude oil seeps up along the 6th Street Fault from theSalt Lake Oil Field, which underlies much of the Fairfax District north of Hancock Park.[2] The oil reaches the surface and forms pools, becoming asphalt as the lighter fractions of the petroleumbiodegrade or evaporate.[3] The asphalt then normally hardens into stubby mounds, which can be seen in several areas of the park.
This seepage has been happening for tens of thousands of years, during which the asphalt sometimes formed a deposit thick enough to trap animals. The deposit then became covered with water, dust, and leaves. Animals wandered in, became trapped, and died. Predators entered to eat the trapped animals and then also become stuck, a phenomenon called a "predator trap". As the bones of a dead animal sank, the asphalt would soak into them, turning them dark-brown or black in color. Lighterfractions of petroleum evaporated from the asphalt, leaving a more solid substance, which then encased the bones.
Dramatic fossils of large mammals have been extricated, and the asphalt also preservesmicrofossils: wood and plant remnants, rodent bones, insects, mollusks, dust, seeds, leaves, and pollen grains.[4] Examples of these are on display in the George C. Page Museum.Radiometric dating of preserved wood and bones has given an age of 38,000 years for the oldest known material from the La Brea seeps.

TheChumash andTongva people used tar from the pits to buildplank boats by sealing planks ofCalifornia redwood trunks and pieces of driftwood from theSanta Barbara Channel, which they used to navigate the California coastline andChannel Islands.[5]
ThePortolá expedition, a group of Spanish explorers led byGaspar de Portolá, made the first written record of the tar pits in 1769. FatherJuan Crespí wrote,
While crossing the basin, the scouts reported having seen some geysers of tar issuing from the ground like springs; it boils up molten, and the water runs to one side and the tar to the other. The scouts reported that they had come across many of these springs and had seen large swamps of them, enough, they said, to caulk many vessels. We were not so lucky ourselves as to see these tar geysers, much though we wished it; as it was some distance out of the way we were to take, the Governor [Portolá] did not want us to go past them. We christened themLos Volcanes de Brea [the Tar Volcanoes].[6]
Harrison Rogers, who accompaniedJedediah Smith on his 1826 expedition to California, was shown a piece of the solidified asphalt while atMission San Gabriel, and noted in his journal, "The Citizens of the Country make great use of it to pitch the roofs of their houses".[7]
The La Brea Tar Pits and Hancock Park were formerly part of theMexican land grant ofRancho La Brea. For some years, tar-covered bones were found on the property but were not initially recognized as fossils because the ranch had lost various animals—including horses, cattle, dogs, and even camels—whose bones closely resemble several of the fossil species. Initially, they mistook the bones in the pits for the remains ofpronghorn or cattle that had become mired. The original Rancho La Brea land grant stipulated that the tar pits be open to the public for the use of the localPueblo.[citation needed]
There were originally more than 100 separate pits of tar (or asphaltum) but most of those have been filled in with rock or dirt since settlement, leaving about a dozen accessible from ground level.[8]
In 1886, the first excavation for land pitch in the village of La Brea was undertaken byMessrs Turnbull, Stewart & co..[9]

Union Oil geologistW. W. Orcutt is credited, in 1901, with first recognizing that fossilized prehistoric animal bones were preserved in pools of asphalt on the Hancock ranch. In commemoration of Orcutt's initial discovery, paleontologists named theLa Brea coyote (Canis latrans orcutti) in his honor.[10]John C. Merriam of theUniversity of California, Berkeley led much of the original work in this area early in the 20th century.[3] Contemporary excavations of the bones started in 1913.
In the 1940s and 1950s, public excitement was generated by the preparation of previously recovered large mammal bones.[11] A subsequent study demonstrated the fossil vertebrate material was well preserved, with little evidence of bacterial degradation of bone protein.[12] They are believed to be some 10–20,000 years old, dating from theLast Glacial Period.[13]
On February 18, 2009, George C. Page Museum announced the 2006 discovery of 16 fossil deposits that had been removed from the ground during the construction of an underground parking garage for theLos Angeles County Museum of Art next to the tar pits.[14] Among the finds are remains of asaber-toothed cat,dire wolves, bison,horses, a giantground sloth, turtles, snails, clams, millipedes, fish, gophers, and anAmerican lion.[14][15] Also discovered is a nearly intact mammoth skeleton, nicknamed Zed; the only pieces missing are a rear leg, a vertebra, and the top of its skull, which was sheared off by construction equipment in preparation to build the parking structure.[15][16][17] These fossils were packaged in boxes at the construction site and moved to a compound behind Pit 91, on Page Museum property, so that construction could continue. Twenty-three large accumulations of tar and specimens were taken to the Page Museum. These deposits are worked on under the name "Project 23".
As work for the public transitD Line isextended, museum researchers know more tar pits will be uncovered, for example near the intersection of Wilshire and Curson.[14] In an exploratory subway dig in 2014 on theMiracle Mile, prehistoric objects unearthed includedgeoducks,sand dollars, and a 10-foot limb (3.0 m) from a pine tree, of a type now found inCentral California's woodlands.[18]

In 1913,George Allan Hancock, the owner of Rancho La Brea, granted theNatural History Museum of Los Angeles County exclusive excavation rights at the Tar Pits for two years.[19] In those two years, the museum was able to extract 750,000 specimens at 96 sites, guaranteeing that a large collection of fossils would remain consolidated and available to the community.[20] Then in 1924, Hancock donated 23 acres (9.3 ha) to Los Angeles County with the stipulation that the county provide for the preservation of the park and the exhibition of fossils found there.[20]
The George C. Page Museum of La Brea Discoveries, part of the Natural History Museum of Los Angeles County, was built next to the tar pits in Hancock Park onWilshire Boulevard. It was named for the donor of the site. Construction began in 1975, and the museum opened to the public in 1977.[21] The area is part of urban Los Angeles in theMiracle Mile District.[22]
The museum tells the story of the tar pits and presents specimens excavated from them. Visitors can walk around the park and see the tar pits. On the grounds of the park are life-sized models of prehistoric animals in or near the tar pits. Of more than 100 pits, only Pit 91 is still regularly excavated by researchers and can be seen at the Pit 91 viewing station. In addition to Pit 91, the one other ongoing excavation is called "Project 23". Paleontologists supervise and direct the work of volunteers at both sites.[23]
As a result of a design competition in 2019, the Natural History Museum of Los Angeles County choseWeiss/Manfredi overDorte Mandrup andDiller Scofidio + Renfro to redesign the park, including by adding a pedestrian walkway framing Lake Pitt, which is 3,281 feet (1,000 metres) long.[24]
The museum is featured prominently in the 1992 cult classic filmEncino Man, where the title character recollects he was previously a caveman during his exploration of the museum's exhibits.[25][26][27]


In respect of it being the "richest paleontological site on Earth for terrestrial fossils of lateQuaternary age," theInternational Union of Geological Sciences (IUGS) included the "Late Quaternary asphalt seeps and paleontological site of La Brea Tar Pits" in its assemblage of 100 geological heritage sites around the world in a listing published in October 2022. The organization defines an IUGS Geological Heritage Site as "a key place with geological elements and/or processes of international scientific relevance, used as a reference, and/or with a substantial contribution to the development of geological sciences through history."[28]

Among the prehistoricPleistocene species associated with the La Brea Tar Pits areColumbian mammoths,dire wolves,short-faced bears,American lions,ground sloths (predominantlyParamylodon harlani, with much rarerMegalonyx jeffersonii andNothrotheriops shastensis) and thestate fossil of California, the saber-toothed cat (Smilodon fatalis). The tar pits don't contain non-birddinosaur remains, as these wereextinct before the pits formed.[29]
The park is known for producing myriad mammal fossils dating from theWisconsin glaciation. While mammal fossils generate significant interest, other fossils including fossilized insects and plants, and even pollen grains, are also valued. These fossils help define a picture of what is thought to have been a cooler, moister climate in the Los Angeles basin during the glacial age. Microfossils are retrieved from the matrix of asphalt and sandy clay by washing with a solvent to remove the petroleum, then picking through the remains under a high-powered lens.
Historically, the majority of the mammals excavated from the La Brea deposits had been large carnivores, supporting a hypothesized "carnivore trap" in which large herbivores entrapped in asphalt attracted predators and scavengers which then became entrapped while trying to steal a quick meal. However, new research with an eye towards microfossils has revealed a stunning diversity and abundance of many types of mammals. According to paleontologist Thomas Halliday, "Rancho La Brea Tar Pits... where big herbivores typically get stuck in tar which naturally seeps from the ground, and as a result, you get huge concentrations of just specifically herbivores. You get a herbivorous sample of the ecosystem and very few carnivores, except those that are trying to scavenge on the already dead carcasses that have just got stuck in the tar."[30][31][32][33][34]
Methane gas escapes from the tar pits, causing bubbles that make the asphalt appear to boil. Asphalt and methane appear under surrounding buildings and require special operations for removal to prevent the weakening of building foundations. In 2007, researchers fromUC Riverside discovered that the bubbles were caused by hardy forms of bacteria embedded in the natural asphalt. After consuming petroleum, the bacteria release methane. Around 200 to 300 species of bacteria were newly discovered here.[35]
Only one human has been found, a partial skeleton ofLa Brea Woman[36] dated to around 10,000calendar years (about 9,000radiocarbon years)BP,[37] who was 17 to 25 years old at death[38] and found associated with remains of a domestic dog, so was interpreted to have been ceremonially interred.[39] In 2016, however, the dog was determined to be much younger in date.[40]
Also, some even older fossils showed possible tool marks, indicating humans active in the area at the time. Bones of saber-toothed cats from La Brea showing signs of "artificial" cut marks at oblique angles to the long axis of each bone were radiocarbon dated to 15,200 ± 800 BP (uncalibrated).[41] If these cuts are in fact tool marks resultant from butchering activities, then this material would provide the earliest solid evidence for human association with the Los Angeles Basin. Yet it is also possible that there was some residual contamination of the material as a result of saturation by asphaltum, influencing the radiocarbon dates.[42]