Abstract
The environmental system is complex and dynamic. It involves many different processes, with characteristic time scales ranging from seconds to billions of years, which often interact in a non-linear manner. There is abundant evidence that the present-day environment is markedly different from those prevailing 500, 5,000, and 50,000 years ago, for example. It is clearly pointless to study the present-day environment in isolation; we need to understand the longer-term processes that influenced our world in the past, and will do so in the near future.
Access this chapter
Tax calculation will be finalised at checkout
Purchases are for personal use only
References
Chambers FA, Charman DJ (2004) Holocene environmental change: contributions from the peatland archive. Holocene 14(1):1–6
Christl M, Strobl C, Mangini A (2003) Beryllium-10 in deep-sea sediments: a tracer for the Earth’s magnetic field intensity during the last 200,000 years. Quat Sci Rev 22(5–7):725–739
Clymo RS (1984) The limits to peat bog growth. Philos Trans R Soc Lond B Biol Sci 303(1117):605–654
Cook ER, Buckley BM, Palmer JG, Fenwick P, Peterson MJ, Boswijk G, Fowler A (2006) Millennia-long tree-ring records from Tasmania and New Zealand: a basis for modelling climate variability and forcing, past, present and future. J Quat Sci 21(7):689–699
Druffel ERM, Robinson LF, Griffin S, Halley RB, Southon JR, Adkins JF (2008) Low reservoir ages for the surface ocean from mid-Holocene Florida corals. Paleoceanography 23(2)
Frank N et al (2009) The Holocene occurrence of cold water corals in the NE Atlantic: implications for coral carbonate mound evolution. Mar Geol 266(1–4):129–142
Hammer CU, Clausen HB, Dansgaard W (1980) Greenland ice sheet evidence of post-glacial volcanism and its climatic impact. Nature 288(5788):230–235
Hoffmann DL, Beck JW, Richards DA, Smart PL, Singarayer JS, Ketchmark T, Hawkesworth CJ (2010) Towards radiocarbon calibration beyond 28†ka using speleothems from the Bahamas. Earth Planet Sci Lett 289(1–2):1–10
Langdon PG, Barber KE, Hughes PDM (2003) A 7500-year peat-based palaeoclimatic reconstruction and evidence for an 1100-year cyclicity in bog surface wetness from Temple Hill Moss, Pentland Hills, southeast Scotland. Quat Sci Rev 22(2–4):259–274
McCracken KG, McDonald FB, Beer J, Raisbeck G, Yiou F (2004) A phenomenological study of the long-term cosmic ray modulation, 850–1958 AD. J Geophys Res-Space Phys 109:12103
Mollenhauer G, Schneider RR, Muller PJ, Spiess V, Wefer G (2002) Glacial/interglacial variablity in the Benguela upwelling system: spatial distribution and budgets of organic carbon accumulation. Global Biogeochem Cycles 16(4):1134
Reimer PJ et al (2004) IntCal04 terrestrial radiocarbon age calibration, 0–26 cal kyr BP. Radiocarbon 46(3):1029–1058
Reimer P et al (2009) IntCal09 and Marine09 radiocarbon age calibration curves, 0–50,000 years cal BP. Radiocarbon 51(4):1111–1150
Rutsch HJ, Mangini A, Bonani G, Dittrichhannen B, Kubik PW, Suter M, Segl M (1995) Be-10 And Ba concentrations in West-African sediments trace productivity in the past. Earth Planet Sci Lett 133(1–2):129–143
Segl M, Mangini A, Beer J, Bonani G, Suter M, Wölfli W (1989) Growth rate variations of manganese nodules and crusts induced by paleoceanographic events. Paleoceanography 4(5):511–530
Sturm M, Lotter AF (1995) Lake sediments as environmental archives. Eawag News, Eawag, p 44
Author information
Authors and Affiliations
Corresponding author
Rights and permissions
Copyright information
© 2012 Springer-Verlag Berlin Heidelberg
About this chapter
Cite this chapter
Beer, J., McCracken, K., von Steiger, R. (2012). Archives. In: Cosmogenic Radionuclides. Physics of Earth and Space Environments. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-642-14651-0_14
Download citation
DOI: https://doi.org/10.1007/978-3-642-14651-0_14
Published:
Publisher Name: Springer, Berlin, Heidelberg
Print ISBN: 978-3-642-14650-3
Online ISBN: 978-3-642-14651-0
eBook Packages: Earth and Environmental ScienceEarth and Environmental Science (R0)