Daisy Cave, also known as CA-SMI-261, is an archeological site located on San Miguel Island in California. San Miguel Island is the westernmost island in the Channel Islands. [1] The island sits between the Santa Barbara Channel and the Pacific Ocean and is often notably battered by winds all year round, but the Daisy Cave itself provides solace from the weather and has served as an effective shelter time and time again. The cave appears to have multiple archaeological deposits, in which artifacts ranging from the "terminal Pleistocene to the present." [2] San Miguel was once part of a larger 'Superisland,' connected with Santa Rosa, Santa Cruz and Anacapa to make up Santarosae. [3] Santarosae existed as the 'superisland' until as recent as 10,000 years ago, with some estimation. [3]
The first excavations of the Daisy Cave are estimated to have occurred around the early 1900s. [4] These initial excavations are not well documented, nor well executed; therefore, the 1967 excavation led by Charles Rozaire is largely considered to be the first true scientific excavation. Rozaire (curator of archeology at the Los Angeles County Museum of Natural History) and his team excavated about 20% of the deposits within the Daisy Cave, but the technology at the time would hardly lend credence to the true age and significance of his findings. Within this first excavation, the remains of about 26 people were found, [2] as well as other various artifacts and remains.
The next excavation would occur in 1985, when Daniel A. Guthrie, Don P. Morris and Pandora E. Snethkamp conducted another, smaller excavation. They would discover "invaluable faunal and artifactal remains," [2] and this was the first time that evidence was dated to be from the Pleistocene, rather than being from the last 3000 years as Rozaire had suggested. The quality of the evidence was invaluable, but the quantity was lacking, these scholars also took the opportunity to correctly date the artifacts that Rozaire had recovered in his excavation back in 1967.
Most recently in 1989, Don P. Morris, S. Hammersmith, and Jon. M Erlandson completed a map of the Daisy Cave and scheduled further site studies and investigations. [4] Erlandson planned investigations for the summers of 1992, 1993, 1994 and 1996. [2] These efforts "completed the stratigraphically controlled excavation of three 50 cm x 100 cm wide test units in the deposits outside the rockshelter and an exploratory sounding extending Rozaire's test pit inside the cave deeper into stratified sediments beneath the cave floor." [2]
The Daisy Cave serves as a time capsule into the lives of Paleo-Indians, Paleo-Coastal peoples, and other maritime populations (ordered sequentially). [2] Each of the relics found in the Daisy Cave provides valuable insight into the lives of the Paleo-Indians and those who came after, as well as the land in which they existed. Artifacts that have been collected included pieces of basketry, various animal fossils, plant remains, shells and stone tools. [4]
Pieces of cordage and basketry from the Holocene (11,700 years ago to the present) have been found in deposits within the Daisy Cave. During Rozaire's 1967 excavation, "over 400 pieces of cordage, clumps of sea grass, and a 13.5 cm x 6 cm piece of a twined sea grass mat or robe" [5] were found deeper within the cave. The most ancient pieces of basketry (basketry is a general term used to describe "baskets, bags, matting, sandals, and other items made with similar techniques and materials,") [5] were discovered in the 1990s and compete in age with some of the oldest fauna remains that have been found so far.
Unlike the mainland of California, an extensive variation of animals is not prevalent. Evidence of dogs, foxes, skunks, birds and mice have been found during the many excavations that have taken place since the early 1900s. [6] Some of the most striking fossil discoveries within the Daisy Cave include those of various rodent species, evidence of the short-faced bear, and remains of two mammoth species.
Much of what has been revealed about the Paleocoastal peoples lies in the discovery of their diets. Exploration of the Daisy Cave has revealed fish bones and 'macrobotanical food remains' [7] that help scholars understand the structure of the Paleocoastal people's lives and adaptations. Because of their location, the early Channel Islanders boasted an impressive ingenuity when it came to harvesting food; they were perhaps the first peoples to utilize hook-and-line fishing, as well as boating. This evidence comes from the analysis of about "27,000 fish bones... dated between about 11,500 and 8500 cal B.P," [8] which suggests that fish and other marine creatures made up more than half of the Islander's diets. From the analysis of these remains, not only did fish make up much of the Islander's diet, but there was also a variety of species that the Islanders fished including: "clupeids, surfperch, rockfish, sheephead, flatfish, elasmobranchs, tunas, and other taxa that are essentially the same types of fish captured by late Holocene and ethnographic people in the area." [8] These various fish bones add to the already established evidence of netting and boat materials to conclude that the Channel Islanders were a population adept at fishing and making the most of their maritime habitat.
Despite the Channel Islands being largely considered as lacking in diverse vegetation, evidence has slowly surfaced that suggests the Islander's also used plants to accompany their largely marine diet. The bulk of this knowledge comes from 16 samples extracted during the 1985-86 excavation conducted by Guthrie, Morris and Snethkamp. The 16 samples "yielded 11 carbonized seeds, 109 fragments of corms and related carbonized remains, and 43 small fragments of manroot." [7] These remains reveal the use of geophytes (geophytes: a perennial plant that bears its perennating buds below the surface of the soil) [9] as a food source, also supported by a high nutrient content that would be effective for Islanders, as well as the sheer amount of these plants that grew back as vegetative populations could recover after overgrazing. [7]
The Chumash are a Native American people of the central and southern coastal regions of California, in portions of what is now Kern, San Luis Obispo, Santa Barbara, Ventura and Los Angeles Counties, extending from Morro Bay in the north to Malibu in the south to Mt Pinos in the east. Their territory includes three of the Channel Islands: Santa Cruz, Santa Rosa, and San Miguel; the smaller island of Anacapa was likely inhabited seasonally due to the lack of a consistent water source. Historically, prior to the arrival of the Spanish, the names of the regions were called Obispeno, Purismeno, Cuyama, Emigdiano, Castaic, Ynezeno, Barbareno, Ventureno, San Miguel, Santa Rosa, Santa Cruz, and Anacapa.
The Channel Islands are an eight-island archipelago located within the Southern California Bight in the Pacific Ocean, off the coast of California. They define the Santa Barbara Channel between the islands and the California mainland. The four Northern Channel Islands are part of the Transverse Ranges geologic province, and the four Southern Channel Islands are part of the Peninsular Ranges province. Five of the islands are within the Channel Islands National Park. The waters surrounding these islands make up Channel Islands National Marine Sanctuary. The Nature Conservancy was instrumental in establishing the Channel Islands National Marine Sanctuary.
The island fox is a small fox species that is endemic to six of the eight Channel Islands of California. There are six subspecies, each unique to the island it lives on, reflecting its evolutionary history. They are generally docile, show little fear of humans, and are easily tamed. Island foxes played an important role in the spiritual lives of native Channel Islanders. They have been likely semi-domesticated as pets, used as pelts, or for other functions, like pest control.
San Miguel Island is the westernmost of California's Channel Islands, located across the Santa Barbara Channel in the Pacific Ocean, within Santa Barbara County, California. San Miguel is the sixth-largest of the eight Channel Islands at 9,325 acres (3,774 ha), including offshore islands and rocks. Prince Island, 700 m (2,300 ft) off the northeastern coast, measures 35 acres (14 ha) in area. The island, at its farthest extent, is 8 miles (13 km) long and 3.7 miles (6.0 km) wide.
Santa Rosae was, before the end of the last ice age, an ancient landmass off the coast of present-day southern California, near Santa Barbara County and Ventura County, of which the northern Channel Islands of California are remnants. At its largest, Santa Rosae was roughly 3-4 times bigger than the northern Channel Islands of today, nearly 125 km long from east to west. Between about 20,000 and 5,000 years ago, Santa Rosae lost about 70% of its land mass to post-glacial rising sea level, leaving behind a vast submerged landscape currently being explored by scientists. San Miguel, Santa Rosa, Santa Cruz, and Anacapa Island comprise the unsubmerged portions of Santa Rosae today. This island was about 5 miles offshore. It broke up between about 11,000 and 9,000 years ago, and the present northern Channel Islands took their shape after the continental ice sheets melted and sea levels rose by about 100 meters.
The island scrub jay, also known as the island jay or Santa Cruz jay, is a bird in the genus, Aphelocoma, which is endemic to Santa Cruz Island off the coast of Southern California. Of the over 500 breeding bird species in the continental U.S. and Canada, it is the only insular endemic landbird species.
Juana Maria, better known to history as the Lone Woman of San Nicolas Island, was a Native Californian woman who was the last surviving member of her tribe, the Nicoleño. She lived alone on San Nicolas Island off the coast of Alta California from 1835 until her removal from the island in 1853. Scott O'Dell's award-winning children's novel Island of the Blue Dolphins (1960) was inspired by her story. She was the last native speaker of the Nicoleño language.
The Nicoleño were the people who lived on San Nicolas Island in California at the time of European contact. They spoke a Uto-Aztecan language. The population of the island was "left devastated by a massacre in 1811 by sea otter hunters." Its last surviving member, who was given the name Juana Maria, was born before 1811 and died in 1853.
Gatecliff Rockshelter (26NY301) is a major archaeological site in the Great Basin area of the western United States that provides remarkable stratigraphy; it has been called the "deepest archaeological rock shelter in the Americas". Located in Mill Canyon of the Toquima Range in the Monitor Valley of central Nevada, Gatecliff Rockshelter has an elevation of 7,750 feet (2,360 m). David Hurst Thomas discovered Gatecliff Rockshelter in 1970 and began excavations in 1971. Full scale excavations occurred at Gatecliff Rockshelter for about seven field seasons in which nearly 33 feet (10 m) of sediments were exposed for a well-defined stratigraphic sequence. The well-preserved artifacts and undisturbed sediments at Gatecliff Rockshelter provides data and information have been applied to a range of research topics. Based on the analysis of the artifacts at Gatecliff Rockshelter, it can be determined that it was most likely a short-term field camp throughout prehistory. The latest evidence for human usage at Gatecliff occurs between ca. 5500 B.P. to 1250 B.P.
Los Osos Back Bay is a prehistoric Chumash archaeological site in the Los Osos Valley, near the coast in San Luis Obispo County, California.
Franktown Cave is located 25 miles (40 km) south of Denver, Colorado on the north edge of the Palmer Divide. It is the largest rock shelter documented on the Palmer Divide, which contains artifacts from many prehistoric cultures. Prehistoric hunter-gatherers occupied Franktown Cave intermittently for 8,000 years beginning about 6400 BC The site held remarkable lithic and ceramic artifacts, but it is better known for its perishable artifacts, including animal hides, wood, fiber and corn. Material goods were produced for their comfort, task-simplification and religious celebration. There is evidence of the site being a campsite or dwelling as recently as AD 1725.
Jon M. Erlandson is an archaeologist, professor emeritus in the Department of Anthropology at the University of Oregon, and the former director of the University of Oregon Museum of Natural and Cultural History. Erlandson’s research interests include coastal adaptations, the peopling of North America, maritime archaeology and historical ecology and human impacts in coastal ecosystems.
Dewil Valley, located in the northernmost part of Palawan, an island province of the Philippines that is located in the Mimaropa region, is an archaeological site composed of thousands of artifacts and features. According to the University of the Philippines Archaeological Studies Program, or UP-ASP, the closest settlement can be found in New Ibajay, which is covered by the town capital of El Nido, which is located around 9 km (5.6 mi) south-east of Dewil Valley. Physically it measures around 7 km (4.3 mi) long, and 4 km (2.5 mi) wide. It is in this place which the Ille Cave, one of the main archaeological sites, can be found. It is actually a network of 3 cave mouths located at its base. It has been discovered that this site in particular has been used and occupied by humans over multiple time periods.
Elands Bay Cave is located near the mouth of the Verlorenvlei estuary on the Atlantic coast of South Africa's Western Cape Province. The climate has continuously become drier since the habitation of hunter-gatherers in the Later Pleistocene. The archaeological remains recovered from previous excavations at Elands Bay Cave have been studied to help answer questions regarding the relationship of people and their landscape, the role of climate change that could have determined or influenced subsistence changes, and the impact of pastoralism and agriculture on hunter-gatherer communities.
Matupi Cave is a cave in the Mount Hoyo massif of the Ituri Rainforest, Democratic Republic of the Congo, where archaeologists have found evidence for Late Stone Age human occupation spanning over 40,000 years. The cave has some of the earliest evidence in the world for microlithic tool technologies.
The Cerutti Mastodon site is a paleontological and possible archeological site located in San Diego County, California. In 2017, researchers announced that broken mastodon bones at the site had been dated to around 130,700 years ago.
Chipped stone crescents are a class of artifact found mainly associated with surface components of archaeological sites located in the Great Basin, the Columbia Plateau, and throughout California. Although their distribution covers a large portion of the western United States, crescents are often found in similar contexts in close proximity to water sources including playas, lakes, rivers, and mainland and island coast lines. Crescents are generally thought to be diagnostic to the terminal Pleistocene and early Holocene and are representative of assemblages that include fluted and stemmed projectile points.
The coastal migration hypothesis is one of two leading hypotheses about the settlement of the Americas at the time of the Last Glacial Maximum. It proposes one or more migration routes involving watercraft, via the Kurile island chain, along the coast of Beringia and the archipelagos off the Alaskan-British Columbian coast, continuing down the coast to Central and South America. The alternative is the hypothesis solely by interior routes, which assumes migration along an ice-free corridor between the Laurentide and Cordilleran ice sheets during the Last Glacial Maximum.
The Tuqan Man consists of human remains found on San Miguel Island off the coast of California in 2005. The skull and bones of a man buried between 9,800 and 10,200 years ago were exposed by beach erosion on this westernmost of the Channel Islands. The remains were encountered and preserved in 2005 by University of Oregon archaeologists. The remains were dated by way of radiocarbon dating and evaluation of artifacts which had been intentionally buried with him. Analysis of the bones indicated that he was in his forties when he died, and had spent time some distance east of what is now the Santa Barbara coastal region. It was not possible to extract the Tuqan Man's DNA, though increasingly better testing techniques and methods became available and were utilized over the 12 years that passed after his original discovery. The remains return to the island was delayed by resolution of tribal identification and ownership issues contingent on resolution of the precedent-setting Kennewick Man case from Washington State. Under procedures in accordance with the Native American Graves Protection and Repatriation Act (NAGPRA), in May, 2018, they were restored to the claiming Chumash tribe, for reburial on the island. The Chumash people had long occupied the island before the arrival of the first European explorers, and the find was given the place name of the island in the Chumash language.
The Scotts Valley Site (CA-SCAR-177), also known as the Lake Carbonera Site, is an archaeological site which has been documented as one of the oldest human settlement sites in Central California. Dated at 12,000-9,000 years before present, it is located in Scotts Valley, California, in the United States, at what was once a large pluvial lake.