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Late Holocene environmental reconstruction using cave sediments from Belize

Published online by Cambridge University Press:  20 January 2017

Jason S. Polk ,
Philip E. van Beynen  and
Philip P. Reeder
Jason S. Polk*
Affiliation:
Department of Geography, Environmental Science and Policy Program, University of South Florida, 4202 E. Fowler Ave., Tampa, FL 33620, USA
Philip E. van Beynen
Affiliation:
Department of Geography, Environmental Science and Policy Program, University of South Florida, 4202 E. Fowler Ave., Tampa, FL 33620, USA
Philip P. Reeder
Affiliation:
Department of Geography, Environmental Science and Policy Program, University of South Florida, 4202 E. Fowler Ave., Tampa, FL 33620, USA
*
*Corresponding author. Fax: +1 813 974 2184.E-mail address:jspolk@mail.usf.edu (J.S. Polk)
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Abstract

Cave sediments collected from Reflection Cave on the Vaca Plateau, Belize show variations in the δ13C values of their fulvic acids (FAs), which indicate periods of vegetation change caused by climatic and Maya influences during the late Holocene. The δ13C values range from − 27.11‰ to − 21.52‰, a shift of ∼ 5.59‰, which suggests fluctuating contributions of C3 and C4 plants throughout the last 2.5 ka, with C4 plant input reflecting periods of Maya agriculture. Maya activity in the study area occurred at different intensities from ∼ 2600 cal yr BP until ∼ 1500 cal yr BP, after which agricultural practices waned as the Maya depopulated the area. These changes in plant assemblages were in response to changes in available water resources, with increased aridity leading to the eventual abandonment of agricultural areas. The Ix Chel archaeological site, located in the study area, is a highland site that would have been among the first agricultural settlements to be affected during periods of aridity. During these periods, minimal water resources would have been available in this highly karstified, well-drained area, and supplemental groundwater extraction would have been difficult due to the extreme depth of the water table.

Keywords

Cave sedimentsCentral AmericaFulvic acidsMaya collapseClimate changeKarstPaleoclimateδ13C carbon isotopeITCZBelize
Type
Research Article
Information
Quaternary Research , Volume 68 , Issue 1 , July 2007 , pp. 53 - 63
Copyright
University of Washington

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References

Aiken, G.R., McKnight, D.M., Wershaw, R.L., MacCarthy, P.(1985). Humic Substances in Soil, Sediment, and Water. John Wiley and Sons, New York.Google Scholar
Biggs, T.H., Quade, J., Webb, R.H.(2002). δ 13C values of soil organic matter in semiarid grassland with mesquite (Prosopis) encroachment in southeastern Arizona. Geoderma, 110, 109–130.Google Scholar
Botrell, S. (1996). Organic carbon concentration profiles in recent cave sediments: Records of agricultural pollution or diagensis?. Environmental Pollution, 91, 3 325–332.CrossRefGoogle Scholar
Brinkmann, R., Reeder, P.(1995). The relationship between surface soils and cave sediments: an example from west central Florida, USA. Cave and Karst Science, 22, 95–102.Google Scholar
Chase, A.F., Chase, D.Z.(1989). The investigation of Classic Period Maya warfare at Caracol, Belize. Mayab, 5, 5–18.Google Scholar
Chase, A.F., Chase, D.Z.(1998). Scale and intensity in Classic Period Maya Agriculture: Terracing and settlement at the “Garden City” of Caracol, Belize. Culture and Agriculture, 20, 2/3 60–77.CrossRefGoogle Scholar
Calderoni, G., Schnitzer, M.(1984). Effects of age on the chemical structure of paleosol humic acids and fulvic acids. Geochimica et Cosmochimica Acta, 48, 2045–2051.CrossRefGoogle Scholar
Clapp, C.E., Layese, M.F., Hayes, M.H.B., Huggins, D.R., Alimaras, R.R.(1997). Natural Abundances of 13C in Soils and Water. Hayes, M.H.B., Wilson, W.S. Humic Substances in Soils, Peats, and Waters: Health and Environmental Aspects The Royal Society of Chemistry, Cambridge.159–175.Google Scholar
Claret, F., Schafer, T., Rabung, T., Wolf, M., Bauer, A., Backau, G.(2005). Differences in properties and Cm(III) complexation behavior of isolated humic and fulvic acid derived from Opalinus clay and Callovo-Oxfordian argillite. Applied Geochemistry, 20, 1158–1168.Google Scholar
Colas, P.R., Stengert, K.C., Wolfel, U.(2006). The Mapping of Ix Chel: A Terminal Classic secondary Maya site on the Northern Vaca Plateau, Belize, Central America. Reeder, Philip P. Technical Report to Government of Belize Google Scholar
Coultas, C.L., Collins, M.E., Chase, A.F.(1993). The effect of Mayan agriculture on terraced soils of Caracol, Belize. Foss, J.E., Timpson, M.E., Morris, M.E. Proceedings of the First International Pedo-Archaeology Conference. Special Publication No. 93–4 Agricultural Experiment Station, University of Tennessee, Knoxville.Google Scholar
Courty, M.A., Vallverdu, J.(2001). The microstratigraphic record of abrupt climate changes in cave sediments of the Western Mediterranean. Geoarchaeology, 16, 5 467–500.Google Scholar
Cowgill, U.M. (1962). An agricultural study of the southern Maya Lowlands. American Anthropologist, 64, 2 273–286.Google Scholar
Curtis, J.H., Hodell, D.A., Brenner, M.(1996). Climate variability on the Yucatan Peninsula (Mexico) during the past 3500 years, and implication for Maya cultural evolution. Quaternary Research, 46, 37–47.Google Scholar
Curtis, J.H., Brenner, M., Hodell, D.A., Balser, R.A., Islebe, G.A., Hoogheimstra, H.(1998). a multi-proxy study of Holocene environmental change in the Maya Lowlands of Peten, Guatemala. Journal of Paleolimnology, 19, 139–159.Google Scholar
Demarest, A.A., Rice, P.M., Rice, D.S.(2004). The Terminal collapse in the Maya Lowlands: Assessing collapses, terminations, and transformations. Demarest, A.A., Rice, P.M., Rice, D.S. The Terminal Classic in the Maya Lowlands: Collapse, Transition, and Transformation University Press of Colorado, Boulder.545–572.Google Scholar
deMenocal, P.B. (2001). Cultural responses to climate change during the Late Holocene. Science, 292, 667–673.CrossRefGoogle ScholarPubMed
Desmarchelier, J.M., Goede, A., Ayliffe, L.K., McCulloch, M.T., Moriarty, K.(2000). Stable isotope record and its paleoenviornmental interpretation for a late Middle Pleistocene speleothem from Victoria Fossil Cave, Naracoorte, South Australia. Quaternary Science Reviews, 19, 763–774.CrossRefGoogle Scholar
Doane, T.A., Devevre, O.C., Horwath, W.R.(2003). Short-term carbon dynamics of humic fractions in low-input and organic cropping systems. Geoderma, 114, 319–331.Google Scholar
Dorale, J.A., Gonzalez, L.A., Reagan, M.K., Pickett, D.A., Murrell, M.T., Baker, R.G.(1992). A high-resolution record of Holocene climate change in speleothem calcite from Cold Water Cave, Northeast Iowa. Science, 258, 1626–1630.Google Scholar
Dorale, J.A., Edwards, R.L., Ito, E., Gonzalez, L.A.(1998). Climate and Vegetation History of the Midcontinent from 75 to 25 ka: A Speleothem Record from Crevice Cave, Missouri, USA. Science, 282, 1871–1874.Google Scholar
Dorale, J.A., Edwards, R.L., Onac, B.P.(2002). Stable isotopes as environmental indicators in speleothems. Yuan, D.-X. Karst Processes and the Carbon Cycle Geological Publishing House, Beijing, China.107–120.Google Scholar
Fairbanks, R.G., Mortlock, R.A., Chiu, T., Cao, L., Kaplan, A., Guilderson, T., Fairbanks, T.W., Bloom, A.L., Grootes, P.M., Nadeau, M.(2005). Radiocarbon calibration curve spanning 0 to 50,000 years BP based on paried 230Th/234U/238U and 14C dates on pristine corals. Quaternary Science Reviews, 24, 1781–1796.Google Scholar
Fronza, G., Fuanti, C., Grasselli, P., Serra, S., Guillou, F.R.C.(2001). δ 13C and δ 18O-values of glycerol of food fats. Rapid Communication in Mass Spectrometry, 15, 763–766.Google Scholar
Furley, P.A. (1976). Soil-slope–plant relationships in the Northern Maya Mountains, Belize, Central America: III. Variations in the properties of soil profiles. Journal of Biogeography, 3, 3 303–319.Google Scholar
Furley, P.A., Newey, W.W.(1979). Variations in plant communities with topography over tropical limestone soils. Journal of Biogeography, 6, 1–15.Google Scholar
Gascoyne, M. (1992). Palaeoclimate determination from cave calcite deposits. Quaternary Sciences Reviews, 11, 609–663.Google Scholar
Gill, R.B. (2000). The Great Maya Droughts: Water, Life, and Death. University of New Mexico Press, Albuquerque.Google Scholar
Grunewald, G., Kaiser, K., Jahn, R., Guggenberger, G.(2006). Organic matter stabilization in young calcareous soils as revealed by density fractionation and analysis of lignin-derived constituents. Organic Geochemsitry, 37, 1573–1589.CrossRefGoogle Scholar
Gunn, J.D., Matheny, R.T., Folan, W.J.(2002). Climate-change studies in the Maya area: a diachronic analysis. Ancient Mesoamerica, 13, 79–84.CrossRefGoogle Scholar
Haug, G.H., Hughen, K.A., Sigman, D.M., Peterson, L.C., Rohl, U.(2001). Southward migration of the Intertropical Convergence Zone through the Holocene. Science, 293, 1304–1308.Google Scholar
Haug, G.H., Günther, D., Peterson, L.C., Sigman, D.M., Hughen, K.A., Aeschlimann, B.(2003). Climate and the collapse of the Maya Civilization. Science, 299, 1731–1735.Google Scholar
Hayes, M.H.B., Wilson, W.S.(1997). Humic Substances, Peats and Sludges: Health and Aspects. Royal Society of Chemistry, Cambridge.Google Scholar
Hodell, D.A., Curtis, J.H., Brenner, M.(1995). Possible role of climate in the collapse of Classic Maya civilization. Nature, 375, 391–394.Google Scholar
Hodell, D.A., Brenner, M., Curtis, J.H., Guilderson, T.(2001). Solar forcing of drought frequency in the Maya Lowlands. Science, 292, 1367–1370.Google Scholar
Hodell, D.A., Brenner, M., Curtis, J.H.(2005a). Terminal classic drought in the northern Maya lowlands inferred from multiple sediment cores in Lake Chichancanab (Mexico). Quaternary Science Reviews, 24, 1413–1427.CrossRefGoogle Scholar
Hodell, D.A., Brenner, M., Curtis, J.H., Medina-Gonzalez, R., Ildefonso-Chan Can, E., Albornaz-Pat, A., Guilderson, T.P.(2005b). Climate change on the Yucatan Peninsula during the Little Ice Age. Quaternary Research, 63, 109–121.Google Scholar
Huang, Y., Street-Perrott, F.A., Metcalfe, S.E., Brenner, M., Moreland, M., Freeman, K.H.(2001). Climate change as the dominant control on glacial–interglacial variations in C3 and C4 plant abundance. Science, 293, 1647–1651.Google Scholar
Hughen, K.A., Eglinton, T.I., Xu, L., Makou, M.(2004). Abrupt tropical vegetation response to rapid climate changes. Science, 304, 1955–1959.CrossRefGoogle ScholarPubMed
Leyden, B.W. (2002). Pollen evidence for climatic variability and cultural disturbance in the Maya Lowlands. Ancient Mesoamerica, 13, 85–101.CrossRefGoogle Scholar
Liao, J.D., Boutton, T.W., Jastrow, J.D.(2006). Organic matter turnover in soil physical fractions following woody plant invasion of grassland: Evidence from natural 13C and 15N. Soil Biology and Biochemistry, 38, 3197–3210.CrossRefGoogle Scholar
Lucero, L.J. (2002). The collapse of the Classic Maya: A case for the role of water control. American Anthropologist, 104, 3 814–826.Google Scholar
Miller, T. (1990). Caves and Caving in Belize: An Overview. Caves and Caving, 46, 2–4.Google Scholar
Neff, H., Pearsall, D.M., Jones, J.G., Arroyo de Pieters, B., Freidel, D.E.(2006). Climate change and population history in the Pacific Lowlands of Southern Mesoamerica. Quaternary Research, 65, 390–400.Google Scholar
Panno, S.V., Curry, B.B., Wang, H., Hackley, K.C., Liu, C.L., Lundstrom, C., Zhou, J.(2004). Climate change in southern Illinois, USA, based on the age and δ 13C of organic matter in cave sediments. Quaternary Research, 61, 301–313.Google Scholar
Penn, M.G., Sutton, D.A., Monro, A.(2004). Vegetation of the Greater Maya Mountains, Belize. Systematics and Biodiversity, 2, 1 21–44.Google Scholar
Quade, J., Cerling, T.E., Bowman, J.R.(1989). Development of Asian monsoon revealed by marked ecological shift during the latest Miocene in northern Pakistan. Letters to Nature, 342, 163–166.Google Scholar
Qualls, R.G. (2004). Biodegradability of humic substances and other fractions of decomposing leaf litter. Soil Science Society of America Journal, 68, 1705–1712.CrossRefGoogle Scholar
Qualls, R.G., Takiyama, A., Wershaw, R.L.(2003). Formation and loss of humic substances during decomposition in a pine forest floor. Soil Science Society of America Journal, 67, 899–909.CrossRefGoogle Scholar
Pessenda, L.C.R., Boulet, R., Aravena, R., Rosolen, V., Gouveia, S.E.M., Ribeiro, A.S., L amotte, M.(2001). Origin and dynamics of soil organic matter and vegetation changes during the Holocene in a forest-savanna transition zone, Brazilian Amazon region. The Holocene, 11, 2 250–254.CrossRefGoogle Scholar
Pessenda, L.C.R., Ledru, M.P., Gouveia, S.E.M., Aravena, R., Ribeiro, J.A., Bendassolli, J.A., Boulet, R.(2005). Holocene paleoenvironmental reconstruction in northeastern Brazil inferred from pollen, charcoal, and carbon isotope records. The Holocene, 15, 6 812–820.Google Scholar
Reeder, P. (2003). Physical and cultural landscapes on the Northern Vaca Plateau, Belize. Journal of Belizean Affairs, 5, 1 5–30.Google Scholar
Reeder, P., Brinkmann, R., Alt, E.(1996). Karstification on the Northern Vaca Plateau, Belize. Journal of Cave and Karst Studies, 58, 2 121–130.Google Scholar
Rosenmeier, M.F., Hodell, D.A., Brenner, M., Curtis, J.A., Martin, J.B., Anselmetti, F.S., Ariztegui, D., Guilderson, T.P.(2002). Influence of vegetation change on watershed hydrology: implications of paleoclimatic interpretation of lacustrine δ 18C records. Journal of Paleolimnology, 27, 117–131.CrossRefGoogle Scholar
Schwartz, D., Mariotti, R., Lanfranchi, R., Guillet, B.(1986). 13C/12C ratios in soil organic matter as indicators of vegetation changes in the Congo. Geoderma, 39, 97–103.Google Scholar
Shaw, J.M. (2003). Climate change and deforestation: Implications for the Maya Collapse. Ancient Mesoamerica, 14, 157–167.Google Scholar
Spaccini, R., Piccolo, A., Haberhauer, G., Gerzabek, M.(2000). Transformation of organic matter from maize residues into labile and humic fractions of three European soils as revealed by 13C distribution and CPMAS-NMR spectra. European Journal of Soil Science, 51, 583–594.Google Scholar
Spaccini, R., Mbagwu, J.S.C., Conte, P., Piccolo, A.(2006). Changes of humic substances characteristics from forested to cultivated soils in Ethiopia. Geoderma, 132, 9–19.Google Scholar
Soto, L.R (2005). Reconstruction of Late Holocene Precipitation for Central Florida as Derived from Isotopes in Speleothems Unpublished Masters Thesis, Department of Geology. University of South Florida, Tampa, Florida.Google Scholar
Stevenson, F.J. (1994). Humus Chemistry—Genesis, Composition, Reactions. 2nd ed.Wiley, New York.Google Scholar
Turney, C.S.M., Bird, M.I., Roberts, R.G.(2001). Elemental δ 13C at Allen's Cave, Nullarbor Plain, Australia: assessing post-depositional disturbance and reconstructing past environments. Quaternary Science, 16, 779–784.Google Scholar
van Beynen, P.E., Ford, D., Schwarcz, H.(2000). Seasonal variability in organic substance in surface cave waters at Marengo Cave, Indiana. Hydrological Processes, 14, 1177–1197.3.0.CO;2-Q>CrossRefGoogle Scholar
van Noordwijk, M., Cerri, C., Woomer, P.L., Nugroho, K., Bernoux, M.(1997). Soil carbon dynamics in the humid tropical forest zone. Geoderma, 79, 187–25 Google Scholar
Webb, E.A., Schwarcz, H.P., Healy, P.F.(2004). Detection of ancient maize in lowland Maya soils using stable carbon isotopes: evidence from Caracol, Belize. Journal of Archaeological Science, 31, 1039–1052.Google Scholar
Webster, J (2000). Speleothem Evidence of Late Holocene Climate Variation in the Maya Lowlands of Belize, Central America and Archaeological Implications. Unpublished Doctoral Dissertation. Department of Geography. University of Georgia, Athens, GA.233pp.Google Scholar
Weninger, B., Joris, O., Danzeglocke, U.(2005). CalPal Radiocarbon Calibration Package. University of Cologne, Germany.Google Scholar
Xu, S., Zheng, G.(2003). Variations in radiocarbon ages of various organic fractions in core sediments from Erhai Lake, SW China. Geocemical Journal, 37, 135–144.Google Scholar
Yamskikh, A. (1998). Late Holocene soil formation in the valley of the River Yenisei, Central Siberia. Catena, 34, 47–60.Google Scholar