Plastic may be with us a lot longer than we thought. In addition to clogging up landfills and becoming trapped in Arctic ice, some of it is turning into stone. Scientists say a new type of rock cobbled together from plastic, volcanic rock, beach sand, seashells, and corals has begun forming on the shores of Hawaii. 
 
 “The article is intriguing and fascinating,” says geophysicist Douglas Jerolmack of the University of Pennsylvania, who was not involved in the work. “If these things can be preserved, then they might be a nice marker around the world of when humans came to dominate the globe and leave behind their refuse in mass quantities.” 
 
 Geologist Patricia Corcoran of the University of Western Ontario in London, Canada, and Charles Moore, captain of the oceanographic research vessel Alguita, stumbled upon the new rocks on a beach on the Big Island of Hawaii. These stones, which they’ve dubbed “plastiglomerates,” most likely formed from melting plastic in fires lit by humans who were camping or fishing, the team reports this month in GSA Today. Although anywhere there is a heat source, such as forest fires or lava flows, and “abundant plastic debris,” Corcoran says, “there is the potential for the formation of plastiglomerate.” When the plastic melts, it cements rock fragments, sand, and shell debris together, or the plastic can flow into larger rocks and fill in cracks and bubbles to form a kind of junkyard Frankenstein. 
 
 Corcoran says some of the plastic is still recognizable as toothbrushes, forks, ropes, and just “anything you can think of.” Once the plastic has fused to denser materials, like rock and coral, it sinks to the sea floor, and the chances it will become buried and preserved in the geologic record increase. 
 
 Corcoran and her team canvassed Kamilo Beach on the Big Island for more of the rocks and found plastiglomerate in all 21 sites they surveyed. She says people have already found plastiglomerate on another Hawaiian island, and she expects there to be much more on coastlines across the world. Plastiglomerate is likely well distributed, it’s just never been noticed before now, she says. 
 
 Jerolmack agrees. “All around the world where there’s trash being openly burned in mass quantities, you can imagine there are even larger melted plastic deposits” where plastiglomerate could form. 
 
 The discovery adds to the debate about whether humanity’s heavy hand in natural processes warrants the formal declaration of a new epoch of Earth history, the Anthropocene, says paleontologist Jan Zalasiewicz of the University of Leicester in the United Kingdom, who was not involved in the study. Plastics in general are so pervasive that they’ve been documented in a number of surprising places, including ingested in wildlife and on the sea floor. The mass of plastic produced since 1950 is close to 6 billion metric tons, enough to bundle the entire planet in plastic wrap. Combine plastic’s abundance with its persistence in the environment, and there’s a good chance it’ll get into the fossil record, Zalasiewicz says. “Plastics, including plastiglomerates, would be one of the key markers by which people could recognize the beginning of the Anthropocene.” 
 
 How long the plastic will endure remains a matter of debate, however. Jerolmack says he doubts the material will stick around in the fossil record. After all, plastic melts, and rocks often pass through hellish depths and temperatures through tectonic processes and burial. Geologist Philip Gibbard of the University of Cambridge in the United Kingdom says he imagines that plastics might “revert back to a source of oil from whence they came, given the right conditions of burial.” But Zalasiewicz and Corcoran say that isn’t true for all the plastic. Some of the material can be preserved as a thin carbon film, much like the way fossil leaves are preserved. Zalasiewicz says that in some rare cases, in that etch of carbon “you may well be left the shape for a flattened plastic bottle.” ||||| Full Text View 
 
 Volume 24 Issue 6 (June 2014) 
 
 GSA Today 
 
 Article, pp. 4-8 | Abstract | PDF (3.8MB) 
 
 An anthropogenic marker horizon in the future rock record 
 
 Patricia L. Corcoran1*, Charles J. Moore2, Kelly Jazvac3 1 Dept. of Earth Sciences, University of Western Ontario, London, Ontario, Canada, N6A 5B7 
 
 2 Algalita Marine Research Institute, Long Beach, California, 90803-4601, USA 
 
 3 Dept. of Visual Arts, University of Western Ontario, London, Ontario, Canada, N6A 5B7 
 
 ABSTRACT Recognition of increasing plastic debris pollution over the last several decades has led to investigations of the imminent dangers posed to marine organisms and their ecosystems, but very little is known about the preservation potential of plastics in the rock record. As anthropogenically derived materials, plastics are astonishingly abundant in oceans, seas, and lakes, where they accumulate at or near the water surface, on lake and ocean bottoms, and along shorelines. The burial potential of plastic debris is chiefly dependent on the material’s density and abundance, in addition to the depositional environment. Here, we report the appearance of a new “stone” formed through intermingling of melted plastic, beach sediment, basaltic lava fragments, and organic debris from Kamilo Beach on the island of Hawaii. The material, herein referred to as “plastiglomerate,” is divided into in situ and clastic types that were distributed over all areas of the beach. Agglutination of natural sediments to melted plastic during campfire burning has increased the overall density of plastiglomerate, which inhibits transport by wind or water, thereby increasing the potential for burial and subsequent preservation. Our results indicate that this anthropogenically influenced material has great potential to form a marker horizon of human pollution, signaling the occurrence of the informal Anthropocene epoch. *Email: DOI: 10.1130/GSAT-G198A.1 Manuscript received 3 Sept. 2013; accepted 8 Nov. 2013. 
 
 Introduction 
 
 Plastics, or synthetic organic polymers, are lightweight, durable products that are used for a number of consumer and non-consumer goods (Barnes et al., 2009). As anthropogenically derived materials, plastics only began to appear in the 1950s, with production and disposal rates increasing steadily over the past 60 years (Ryan and Moloney, 1993; Moore, 2008). Combined with abysmal rates of recovery, a massive amount of plastic debris has accumulated in Earth’s waterways and along shorelines (Derraik, 2002; Thompson et al., 2004; Corcoran et al., 2009; Law et al., 2010). These plastics have been proven dangerous to marine organisms and seabirds through ingestion, entanglement, and disruption of feeding patterns (Laist, 1997; Eriksson and Burton, 2003; Boren et al., 2006; Gregory, 2009; Aloy et al., 2011). In addition, adsorption of persistent organic pollutants (POPs) onto plastics (Mato et al., 2001; Endo et al., 2005; Rios et al., 2007, 2010) enhances the potential for bioaccumulation from ingested microplastics into fish. The unknown effect on apex predators, such as humans, is a major concern. These POPs, such as polychlorinated biphenyls (PCBs), can cause serious health effects, as they have been shown to be endocrine-disrupting chemicals and carcinogens (Bergman et al., 2013). 
 
 The degradation of plastic material is a slow process that can occur mechanically, chemically (thermo- or photo-oxidative), and to a lesser degree, biologically (Kulshreshtha, 1992; Shah et al., 2008; Cooper and Corcoran, 2010). The persistence of plastic in the environment has been estimated to be in the range of hundreds to thousands of years, although longevity can increase in cool climates and where material is buried on the ocean bottom or under sediment (Gregory and Andrady, 2003). A recent study examining the accumulation of marine ocean debris at depths of 25–3971 m over a 22-year period shows that 33% of all debris in Monterey Bay, California, USA, is composed of plastic litter (Schlining et al., 2013). Similar results from other localities reveal that much of plastic debris is below the water surface (Goldberg, 1997; Galgani et al., 2000; Keller et al., 2010). This debris may be composed of high-density plastics or low-density plastics with fouled surfaces (Ye and Andrady, 1991; Goldberg, 1997; Gregory, 2009; Lobelle and Cunliffe, 2011). Given the low water temperatures and decreased exposure to UV light at greater depths within and below the photic zone, sunken plastic debris has good potential to persist and eventually form part of the rock record. On beaches, plastic debris, such as resin pellets, fragments, and expanded polystyrene up to 11 mm in size, may be preserved within the upper 5 cm of beach sediment (Kusui and Noda, 2003). Claessens et al. (2011) identified microplastics in beach sediment cores at depths down to 32 cm. In addition, Fisner et al. (2013), in their study of polycyclic aromatic hydrocarbons in pellets, were able to locate plastic debris at sediment depths as great as 1 m. However, we found no visible loose plastic fragments at depths >10 cm in sand on Kamilo Beach, Hawaii. Given the beach’s constant exposure to the northeasterly trade winds, much of the small (<10 cm), lightweight plastic debris is blown to the backshore environment, where it becomes trapped in vegetation. On a beach as dynamic as Kamilo, preservation of plastics in the sediment column could occur where trapped sediment is covered with sand or where a polymer is combined with a much denser material. We observed the results of this density increase on Kamilo Beach, where great quantities of melted plastic have mixed with the substrate to create new fragments of much greater density, herein referred to as “plastiglomerate.” 
 
 Characteristics of Kamilo Beach 
 
 The location of the Hawaiian Islands within the North Pacific subtropical gyre makes them vulnerable to acting as sinks for plastic debris (Moore, 2008). The anticyclonic movement of surface ocean currents within the gyre results in preferential deposition of marine debris along the eastern and southeastern windward shorelines of the major Hawaiian Islands (Corcoran et al., 2009; McDermid and McMullen, 2004). Kamilo Beach, located on the southeastern tip of the island of Hawaii, is notable for its accumulation of vast amounts of marine debris (Moore, 2008) (Figs. 1A and 1B). Typical plastic debris include derelict fishing gear, including nets, oyster spacer tubes and buoys; food and drinking containers; resin pellets; and abundant multi-colored fragments or “plastic confetti” (Fig. 1C). The main stretch of Kamilo Beach is ~700 m long, and its northern termination is marked by a rocky headland jutting 300 m oceanward at low tide. The beach is accessible by four-wheel drive vehicle only, and it is an ~12 km drive from the nearest paved road. The remoteness of the beach plays an important role in the formation of a potential plastiglomerate marker horizon, as most visitors camp for extended periods of time and build fires for cooking and warmth. In addition, regular, organized beach clean-ups are difficult. 
 
 Formation of Plastiglomerate on Kamilo Beach 
 
 We use the term plastiglomerate to describe an indurated, multi-composite material made hard by agglutination of rock and molten plastic. This material is subdivided into an in situ type, in which plastic is adhered to rock outcrops, and a clastic type, in which combinations of basalt, coral, shells, and local woody debris are cemented with grains of sand in a plastic matrix (Figs. 2A and 2B). Of the 21 sample locations containing plastiglomerate on Kamilo Beach, in situ plastiglomerate was identified at nine. Partially melted polymers adhered to basalt outcrops included fishing nets, piping, bottle caps, and rubber tires. Locally, molten plastic had infilled vesicles in volcanic rock, thereby forming plastic amygdales (Fig. 2C). The largest surface exposure of in situ plastiglomerate was 176 × 82 cm, which was evident only following removal of 15 cm of beach sediment (Fig. 2D). Beach sand and woody debris were locally adhered to the plastic surfaces. Based on its location in more sheltered regions of the beach or within depressions of volcanic rock outcrops, in situ plastiglomerate is interpreted to represent campfire debris. 
 
 Clastic plastiglomerate fragments, >2 cm in size, were collected from 21 locations along Kamilo Beach. In addition, we measured the abundance and sizes of angular, clastic plastiglomerate fragments in a quadrat measuring 5 m × 5 m. Partially buried, fractured, in situ plastiglomerate at the center of the quadrat is interpreted as the source of the angular fragments. One hundred and sixty-seven fragments were identified, ranging in size from 2.0 to 22.5 cm, with 55% represented by fragments <4.5 cm. In contrast to the angular nature of the fragments within the quadrat, clastic plastiglomerate fragments found closer to the water and along the strandline were rounded (Fig. 2B) as a result of abrasion in the foreshore environment. A total of 205 fragments sampled from Kamilo Beach displayed different combinations of coral pebbles, plastic, basalt pebbles, woody debris (including charcoal, nuts, and seeds), and sand (including shell fragments) (Fig. 3A). Angular fragments <4 cm in size mainly comprised the sand-plastic group, whereas larger angular fragments were predominantly composed of sand, plastic, basalt pebbles, and woody debris. This discrepancy may be a result of the preferential weathering of organic woody debris and charcoal from the larger fragments, leaving smaller fragments devoid of organic material. 
 
 Although plastic debris in some plastiglomerate fragments was melted beyond recognition, we were able to identify distinct types of plastic in most samples. Plastic types included netting/ropes, pellets, partial containers/packaging, lids, tubes/pipes, and “confetti” (Figs. 4A–4D). The latter plastic type was most abundant, as it represents the embrittled remains of intact products, such as containers (Fig. 3B). Partial containers and lids were preserved and were identified in 22% of all fragments. Approximately 20% of the samples contained evidence of fishing-related debris, as indicated by netting, ropes, nylon fishing line, as well as remnants of oyster spacer tubes. We observed that some of the plastiglomerate had been buried by sand and organic debris, as well as having been trapped within vegetation, which demonstrates the potential for preservation in the future rock record. 
 
 We measured the bulk density of 20 clastic plastiglomerate fragments sampled from Kamilo Beach. Bulk density of the clastic fragments ranged from 1.7 to 2.8 g/cm3, with the highest values determined from fragments rich in basalt pebbles. The measured bulk densities show that plastiglomerate has greater potential to become buried and preserved in the rock record than plastic-only particles, which typically have densities in the range of 0.8–1.8 g/cm3 (Kholodovych and Welsh, 2007). 
 
 Source of Molten Plastic 
 
 Although the island of Hawaii is volcanically active, the recorded locations of flowing lava over the past century are not coincident with the location of Kamilo Beach. Therefore, the plastiglomerate we sampled from Kamilo Beach cannot be the result of molten lava and polymer interaction. These plastiglomerate fragments were formed anthropogenically. Burning plastic debris in an open environment results in the release of chemical substances, such as carbon monoxide, polycyclic aromatic hydrocarbons, and dioxins (EPA, 2013). These pollutants can cause neurological symptoms, cancer, and hormonal disruptions in humans. In this regard, Kamilo Beach provides an example of an anthropogenic action (burning) reacting to an anthropogenic problem (plastics pollution), resulting in a distinct marker horizon of the informal Anthropocene epoch. Although campfire burning is responsible for the plastiglomerate on Kamilo Beach, it is conceivable that the global extent of plastic debris could lead to similar deposits where lava flows, forest fires, and extreme temperatures occur. 
 
 Informal Anthropocene Epoch 
 
 According to the geologic timescale, we are currently living in the Holocene epoch. However, Crutzen and Stoermer (2000) proposed the term “Anthropocene” to represent the period of time between the latter half of the 18th century and the present day. Although other workers have considered the onset of this informal epoch to have occurred at slightly different times (Ruddiman, 2003; Doughty et al., 2010), researchers agree that the Anthropocene is a time span marked by human interaction with Earth’s biophysical system (Zalasiewicz et al., 2011; Syvitsky, 2012). Geological evidence used in supporting this assertion comes from Holocene ice cores and soil profiles. For example, methane concentrations measured in ice cores display an increase at ca. 5000 yr B.P., which contrasts with the expected decline in CH 4 at that time, based on the orbital-monsoon cycle theory (Ruddiman and Thomson, 2001). Ruddiman and Thomson propose that this anomalous rise in CH 4 can be linked to early agricultural practices in Eurasia. In addition, an increase in atmospheric CO 2 at ca. 8000 yr B.P., as determined from ice cores, was explained by Ruddiman (2003) as a result of early forest clearance. 
 
 Soil profiles from peat bogs in Norway indicate an increase in lead concentrations in Europe over the past 300 years (Dunlap et al., 1999). Lead concentrations prior to ca. 1950 AD are attributed to mining activities, whereas a second Pb compositional signature in soil younger than 1950 AD is consistent with atmospheric lead derived mainly from combustion of leaded gasoline. Certini and Scalenghe (2011) suggested that anthropogenic soils are the “golden spikes” for the Anthropocene because they contain evidence of soil management practices for enhancing fertility. Examples include terracing, and formation of mixed charcoal, manure, plant debris, and animal bones. 
 
 Atmospheric compositions and soil management practices are only two indicators of anthropogenic activity, but relatively few examples of solid, human-made materials are preserved in the sediment record (Zalasiewicz et al., 2008). Even rarer are items that are correlatable on a global scale. Given the ubiquity of non-degradable plastic debris on our planet, the possibility of their global preservation is strong. Our study presents the first rock type composed partially of plastic material that has strong potential to act as a global marker horizon in the Anthropocene. 
 
 Acknowledgments 
 
 This project would not have been possible without the help of Noni and Ron Sanford of Volcano, Hawaii, beachcombers and steadfast volunteers of the Hawaii beach clean-up effort. Noni and Ron guided us to Kamilo Beach and provided us with a wealth of background information. Their wonderful hospitality is greatly appreciated! We also thank Megan Lamson of the Hawaii Wildlife Fund, who provided us with samples. 
 
 REFERENCES CITED 
 
 Aloy, A.B., Vallejo, B.M., Jr., and Juinio-Menez, M.A., 2011, Increased plastic litter cover affects the foraging activity of the sandy intertidal gastropod Nassarius pullus: Marine Pollution Bulletin, v. 62, p. 1772–1779, doi: 10.1016/j.marpolbul.2011.05.021. Barnes, D.K.A., Galgani, F., Thompson, R.C., and Barlaz, M., 2009, Accumulation and fragmentation of plastic debris in global environments: Philosophical Transactions of the Royal Society, v. 364, p. 1985–1998, doi: 10.1098/rstb.2008.0205. Bergman, A., Heindel, J.J., Jobling, S., Kidd, K.A., and Zoeller, T., 2013, State of the Science of Endocrine Disrupting Chemicals-2012: Geneva, United Nations Environment Programme and the World Health Organization, 260 p. Boren, L.J., Morrissey, M., Muller, C.G., and Gemmell, N.J., 2006, Entanglement of New Zealand fur seals in man-made debris at Kaikoura, New Zealand: Marine Pollution Bulletin, v. 52, p. 442–446, doi: 10.1016/j.marpolbul.2005.12.003. Certini, G., and Scalenghe, R., 2011, Anthropogenic soils are the golden spikes for the Anthropocene: The Holocene, v. 21, p. 1269–1274, doi: 10.1177/0959683611408454. Claessens, M., De Meester, S., Van Landuyt, L., De Clerck, K., and Janssen, C.R., 2011, Occurrence and distribution of microplastics in marine sediments along the Belgian coast: Marine Pollution Bulletin, v. 62, p. 2199–2204, doi: 10.1016/j.marpolbul.2011.06.030. Cooper, D.A., and Corcoran, P.L., 2010, Effects of mechanical and chemical processes on the degradation of plastic beach debris on the island of Kauai, Hawaii: Marine Pollution Bulletin, v. 60, p. 650–654, doi: 10.1016/j.marpolbul.2009.12.026. Corcoran, P.L., Biesinger, M.C., and Grifi, M., 2009, Plastics and beaches: A degrading relationship: Marine Pollution Bulletin, v. 58, p. 80–84, doi: 10.1016/j.marpolbul.2008.08.022. Crutzen, P.J., and Stoermer, E.F., 2000, The “Anthropocene”: Global Change Newsletter, v. 41, p. 17–18. Derraik, J.G.B., 2002, The pollution of the marine environment by plastic debris: A review: Marine Pollution Bulletin, v. 44, p. 842–852, doi: 10.1016/S0025-326X(02)00220-5. Doughty, C.E., Wolf, A., and Field, C.B., 2010, Biophysical feedbacks between the Pleistocene megafauna extinction and climate: The first human-induced global warming?: Geophysical Research Letters, doi: 10.1029/2010GL043985. Dunlap, C.E., Steinnes, E., and Flegal, A.R., 1999, A synthesis of lead isotopes in two millennia of European air: Earth and Planetary Science Letters, v. 167, p. 81–88, doi: 10.1016/S0012-821X(99)00020-5. Endo, S., Takizawa, R., Okuda, K., Chiba, K., Kanehiro, H., Ogi, H., Yamashita, R., and Date, T., 2005, Concentration of polychlorinated biphenyls (PCBs) in beached resin pellets: Variability in individual particles and regional differences: Marine Pollution Bulletin, v. 50, p. 1103–1114, doi: 10.1016/j.marpolbul.2005.04.030. Eriksson, C., and Burton, H., 2003, Origins and biological accumulation of small plastic particles in fur seals from Macquarie Island: Ambio, v. 32, p. 380–384. Fisner, M., Taniguchi, S., Moreira, F., Bicego, M.C., and Turra, A., 2013, Polycyclic aromatic hydrocarbons (PAHs) in plastic pellets: Variability in the concentration and composition at different sediment depths in a sandy beach: Marine Pollution Bulletin, v. 70, p. 219–226, doi: 10.1016/j.marpolbul.2013.03.008. Galgani, F., Leaute, J.P., Moguedet, P., Souplet, A., Verin, Y., Carpentier, A., Goraguer, H., Latrouite, D., Andral, B., Cadiou, Y., Mahe, J.C., Poulard, J.C., and Nerisson, P., 2000, Litter on the sea floor along European coasts: Marine Pollution Bulletin, v. 40, p. 516–527, doi: 10.1016/S0025-326X(99)00234-9. Goldberg, E.D., 1997, Plasticizing the seafloor: An overview: Environmental Technology, v. 18, p. 195–201, doi: 10.1080/09593331808616527. Gregory, M.R., 2009, Environmental implications of plastic debris in marine settings: Entanglement, ingestion, smothering, hanger-on, hitch-hiking and alien invasions: Philosophical Transactions of the Royal Society, v. 364, p. 2013–2025, doi: 10.1098/rstb.2008.0265. Gregory, M.R., and Andrady, A.L., 2003, Plastics in the marine environment, in Andrady, A.L., ed., Plastics and the Environment: New Jersey, Wiley & Sons, p. 379–401. Keller, A.A., Fruh, E.L., Johnson, M.M., Simon, V., and McGourty, C., 2010, Distribution and abundance of anthropogenic marine debris along the shelf and slope of the U.S. West Coast: Marine Pollution Bulletin, v. 60, p. 692–700, doi: 10.1016/j.marpolbul.2009.12.006. Kholodovych, V., and Welsh, W.J., 2007, Densities of amorphous and crystalline polymers, in Mark, J.E., ed., Physical Properties of Polymers Handbook: New York, Springer, p. 611–616. Kulshreshtha, A.K., 1992, Chemical degradation, in Hamid S.S., Amin, M.B., and Maadhah, A.G., eds., Handbook of Polymer Degradation: Boca Raton, Florida, CRC Press, p. 55–90. Laist, D.W., 1997, Impacts of marine debris: Entanglement of marine life in marine debris including a comprehensive list of species with entanglement and ingestion records, in Coe, J.M., and Rogers, D.B., eds., Marine Debris: Sources, Impacts and Solutions: Berlin, Springer, p. 99–141. Law, K.L., Moret-Ferguson, S., Maximenko, N.A., Proskurowski, G., Peacock, E.E., Hafner, J., and Reddy, C.M., 2010, Plastic accumulation in the North Atlantic subtropical gyre: Science, v. 329, p. 1185–1188, doi: 10.1126/science.1192321. Lobelle, D., and Cunliffe, M., 2011, Early microbial biofilm formation on marine plastic debris: Marine Pollution Bulletin, v. 62, p. 197–200, doi: 10.1016/j.marpolbul.2010.10.013. Kusui, T., and Noda, M., 2003, International survey on the distribution of stranded and buried litter on beaches along the Sea of Japan: Marine Pollution Bulletin, v. 47, p. 175–179. Mato, Y., Isobe, T., Hideshige, T., Kanehiro, H., Ohtake, C., and Kaminuma, T., 2001, Plastic resin pellets as transport medium for toxic chemicals in the marine environment: Environmental Science & Technology, v. 35, p. 318–324, doi: 10.1021/es0010498. McDermid, K.J., and McMullen, T.L., 2004, Quantitative analysis of small-plastic debris on beaches in the Hawaiian Archipelago: Marine Pollution Bulletin, v. 48, p. 790–794, doi: 10.1016/j.marpolbul.2003.10.017. Moore, C.J., 2008, Synthetic polymers in the marine environment: A rapidly increasing long-term threat: Environmental Research, v. 108, p. 131–139, doi: 10.1016/j.envres.2008.07.025. Rios, L.M., Moore, C., and Jones, P.R., 2007, Persistent organic pollutants carried by synthetic polymers in the ocean environment: Marine Pollution Bulletin, v. 54, p. 1230–1237, doi: 10.1016/j.marpolbul.2007.03.022. Rios, L.M., Jones, P.R., Moore, C., and Narayana, U.V., 2010, Quantitation of persistent organic pollutants adsorbed on plastic debris from the Northern Paciðc Gyre’s ‘‘eastern garbage patch’’: Journal of Environmental Monitoring, v. 12, p. 2226–2236, doi: 10.1039/c0em00239a. Ruddiman, W.F., 2003, The Anthropogenic greenhouse era began thousands of years ago: Climatic Change, v. 61, p. 261–293, doi: 10.1023/B:CLIM.0000004577.17928.fa. Ruddiman, W.F., and Thomson, J.S., 2001, The case for human causes of increased atmospheric CH4 over the last 5000 years: Quaternary Science Reviews, v. 20, p. 1769–1777, doi: 10.1016/S0277-3791(01)00067-1. Ryan, P.G., and Moloney, C.L., 1993, Marine litter keeps increasing: Nature, v. 361, p. 23, doi: 10.1038/361023a0. Schlining, K., von Thun, S., Kuhnz, L., Schinling, B., Lundsten, L., Jacobsen Stout, N., Chaney, L., and Connor, J., 2013, Debris in the deep: Using a 22-year video annotation database to survey marine litter in Monterey Canyon, central California, USA: Deep-Sea Research Part I: Ocean Research Paper 79, p. 96–105. Shah, A.A., Hasan, F., Hameed, A., and Ahmed, S., 2008, Biological degradation of plastics: A comprehensive review: Biotechnology Advances, v. 26, p. 246–265, doi: 10.1016/j.biotechadv.2007.12.005. Syvitsky, J., 2012, Anthropocene: An epoch of our making: Global Change Newsletter, v. 78, p. 12–15. Thompson, R.C., Olsen, Y., Mitchell, R.P., Davis, A., Rowland, S.J., John, A.W.G., McGonigle, D., and Russell, A.E., 2004, Lost at sea: Where is all the plastic?: Science, v. 304, p. 838, doi: 10.1126/science.1094559. U.S. Environmental Protection Agency, 2013, Wastes – Non-Hazardous Waste – Municipal Solid Waste: Human Health: http://www.epa.gov/osw/nonhaz/municipal/backyard/health.htm (last accessed 21 Feb. 2014). Ye, S., and Andrady, A.L., 1991, Fouling of floating plastic debris under Biscayne Bay exposure conditions: Marine Pollution Bulletin, v. 22, p. 608–613, doi: 10.1016/0025-326X(91)90249-R. Zalasiewicz, J., Williams, M., Haywood, A., and Ellis, M., 2011, The Anthropocene: A new epoch of geological time?: Philosophical Transactions of the Royal Society, v. 369, p. 835–841, doi: 10.1098/rsta.2010.0339. Zalasiewicz, J., Williams, M., Smith, A., Barry, T.L., Coe, A.L., Brown, P.R., Brenchley, P., Cantrill, D., Gale, A., Gibbard, P., Gregory, F.J., Hounslow, M.W., Kerr, A.C., Pearson, P., Knox, R., Powell, J., Waters, C., Marshall, J., Oates, M., Rawson, P., and Stone, P., 2008, Are we now living in the Anthropocene?: GSA Today, v. 18, p. 4–8, doi: 10.1130/GSAT01802A.1. 
 
 top
– Since the mid-1950s, humans have produced more than 6 billion tons of plastic—and at least in Hawaii, geologists are finding that some of it is now fusing to volcanic rocks, seashells, sand, and coral to form an entirely new type of rock. Calling them plastiglomerates, the geologists say they found the stones at all 21 sites they surveyed on the Big Island—the New York Times reports the rocks ranged from as small as a peach pit to as large as a large pizza—and that they've been identified on another Hawaiian island as well. The prevailing theory is that the plastiglomerates form when people burn plastic in beach bonfires or campfires; the heat helps fuse the organic and inorganic materials, according to Science. Some of the plastic is still close enough to its original shape to resemble the toothbrushes, forks, and ropes they once were. Some of the rocks are likely making their way down to the bottoms of sea beds, where they are more likely to be preserved in the geological record. As one marine biologist tells the Times, "Most conventional plastic is relatively thin and fragments quickly, but what’s being described here is something that’s going to be even more resistant to the aging process." That has one geophysicist not involved in the study suggesting there's a sort of silver lining to this: The rocks "might be a nice marker around the world of when humans came to dominate the globe and leave behind their refuse in mass quantities," he says. As such, one paleontologist argues the plastiglomerates could "be one of the key markers by which people could recognize the beginning of the Anthropocene"—a new geologic era on Earth marked by human's heavy impact on the planet. (On the other end of the temperature scale, plastics have even found their way into Arctic ice.)