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Pliocene–Pleistocene sedimentary and geomorphologic development of the Vasilikos river catchment, S Cyprus, in relation to uplift of the Troodos ophiolite and climate-related changes

Published online by Cambridge University Press:  25 October 2019

Hannah Murray Open the ORCID record for Hannah Murray [Opens in a new window]  and
Alastair HF Robertson
Hannah Murray*
Affiliation:
School of GeoSciences, Grant Institute, University of Edinburgh, James Hutton Road, Edinburgh EH9 3FE, UK
Alastair HF Robertson
Affiliation:
School of GeoSciences, Grant Institute, University of Edinburgh, James Hutton Road, Edinburgh EH9 3FE, UK
*
Author for correspondence: Hannah Murray, Email: [email protected]
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Abstract

The Pleistocene development of the Vasilikos River exemplifies the interaction of focused, tectonically induced surface uplift and climate-influenced changes. The resulting sediments are well exposed in Vasilikos Quarry and in the main river catchment further east. An important erosional surface incises the highest-level (oldest) fluvial conglomerates, down into Late Pliocene – Early Pleistocene open-marine mudrocks (Nicosia Formation), allowing integration with the circum-Cyprus sedimentary–geomorphic development (F1–F4 stages). To determine where the quarry deposits lie in relation to the Vasilikos river catchment, the fluvial deposits were mapped and valley profiles were constructed, revealing four main episodes, each associated with incision and distinctive fluvial deposition. Source lithology strongly influenced channel morphology, infill and adjacent slope-sediment (colluvium) composition. Palaeosols, particularly red-brown terra rossa, developed on abandoned fluvial terraces and adjacent hillslopes, especially overlying F3 surfaces. The combined evidence allows close correlation of the Vasilikos river and quarry deposits. Relatively coarse (chalky conglomerate/breccia) and fine-grained colluvium (calcareous silt – Cyprus harvara) developed especially on lower hillslopes following incision (mainly above F2 and F3 surfaces). Based on regional comparisons, overall sediment aggregation ended during the Early Pleistocene. The F1–F2 surfaces and deposits are inferred to be Middle Pleistocene, the F3 ones later Middle Pleistocene and the F4 ones near the Middle–Late Pleistocene boundary. Geomorphology and deposition were tectonically forced during strong, focused Early–Middle Pleistocene surface uplift. Coarse clastic ruff-off and palaeosol development (terra rossa) and related sediment aggradation are inferred to have increased during warm, humid periods. Late Pleistocene geomorphology and deposition were more influenced by climatic change, with semi-perennial streamflow, rapid sediment aggradation and palaeosol (terra rossa) development during warm, humid periods (interglacials). Cooler (glacial) periods enhanced fluvial-incision, sediment-bypassing and hillslope colluvial processes (e.g. frost shattering, downslope creep and mass flow) when sediment transport (bypassing) exceeded sediment supply. Neotectonic faulting affected the catchment but did not greatly affect geomorphology or sediment supply. Although climate / climate change (and eustatic sea-level change) had an important influence, tectonics is interpreted as the fundamental driver of geomorphological development and fluvial sedimentation, with implications for other areas, regionally to globally.

Keywords

Troodos Massifriver terracesalluviumcolluviumpalaeosolsfluvial processes
Type
Original Article
Information
Geological Magazine , Volume 157 , Issue 4 , April 2020 , pp. 573 - 602
Copyright
© Cambridge University Press 2019

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References

Allen, PA (2008) From landscape into geological history. Nature 451, 274–76.CrossRefGoogle Scholar
Anastasakis, G and Kelling, G (1991) Tectonic connection of the Hellenic and Cyprus arcs and related geotectonic elements. Marine Geology 97, 261–77.CrossRefGoogle Scholar
Arakel, AV (1982) Genesis of calcrete in Quaternary soil profiles, Hutt and Leeman Lagoons, Western Australia. Journal of Sedimentary Research 52, 109–25.CrossRefGoogle Scholar
Bagnall, PS (1960) The Geology and Mineral Resources of the Pano Lefkara-Larnaca Area. Memoirs of the Geological Survey, Cyprus, no. 5.Google Scholar
Balmer, E, Robertson, A, Raffi, I and Kroon, D (2018) Pliocene-Pleistocene sedimentary development of the syntectonic Polis graben, NW Cyprus: evidence from facies analysis, nannofossil biochronology and strontium isotope dating. Geological Magazine, 156, 889–917. doi: 10.1017/S0016756818000286.CrossRefGoogle Scholar
Bellamy, CV and Jukes-Browne, AJ (1905) The Geology of Cyprus. Plymouth: W. Brendon & Son, 72 pp.Google Scholar
Blum, MD and Törnqvist, TE (2000) Fluvial responses to climate and sea-level change: a review and look forward. Sedimentology 47, 2–48.CrossRefGoogle Scholar
Bridgland, D and Westaway, R (2008) Climatically controlled river terrace staircases: a worldwide Quaternary phenomenon. Geomorphology 98, 285–315.CrossRefGoogle Scholar
Calon, TJ, Aksu, AE and Hall, J (2005) The Oligocene-Recent evolution of the Mesaoria Basin (Cyprus) and its western marine extension, Eastern Mediterranean. Marine Geology 221, 95–120.CrossRefGoogle Scholar
Candy, I and Black, S (2009) The timing of Quaternary calcrete development in semi-arid southeast Spain: investigating the role of climate on calcrete genesis. Sedimentary Geology 220, 6–15.CrossRefGoogle Scholar
Candy, I, Rose, J and Lee, J (2006) A seasonally ‘dry’ interglacial climate in eastern England during the Early–Middle Pleistocene: palaeopedological and stable isotopic evidence from Pakefield, U.K. Boreas 35, 255–65.CrossRefGoogle Scholar
Caputo, R, Catalano, S, Monaco, C, Romagnoli, G, Tortorici, G and Tortorici, L (2010) Active faulting on the island of Crete (Greece). Geophysical Journal Internation 183, 111–26.CrossRefGoogle Scholar
Celma, DC, Pieruccini, P and Farabollini, P (2015) Major controls on architecture, sequence stratigraphy and paleosols of Middle Pleistocene continental sediments (“Qc Unit”), eastern central Italy. Quaternary Research 83, 565–81.CrossRefGoogle Scholar
Cohen, KM, Finney, SC, Gibbard, PL and Fan, JX (2013) The ICS international chronostratigraphic chart. Episodes, 36, 199–204.CrossRefGoogle Scholar
Collinson, JD (1996) Alluvial sediment sediments. In Sedimentary Environments: Processes, Facies and Stratigraphy (ed. Reading, H. G.), pp. 37–82. Oxford: Blackwell.Google Scholar
Constantinou, G (1995) Geological Map of Cyprus. Nicosia: Geological Survey Department, Cyprus.Google Scholar
Cosentino, D, Schildgen, TF, Cipollari, P, Faranda, C, Gliozzi, E, Hudáčková, N, Lucifora, S and Strecker, MR (2012) Late Miocene surface uplift of the southern margin of the Central Anatolian Plateau, Central Taurides, Turkey. Geological Society of America Bulletin 124, 133–45.CrossRefGoogle Scholar
D’Arcy, M and Whittaker, AC (2014) Geomorphic constraints on landscape sensitivity to climate in tectonically active areas. Geomorphology 204, 336–81.Google Scholar
Deckers, K (2005) Post-Roman history of river systems in Western Cyprus: causes and archaeological implications. Journal of Mediterranean Archaeology 18, 155–81.CrossRefGoogle Scholar
Ducloz, C (1964) Revision of the Pliocene and Quaternary stratigraphy of the central Mesaoria. In Annual Report of the Geological Survey Department, pp. 31–42.Nicosia: Geological Survey Department, Cyprus.Google Scholar
Duman, TY, Robertson, AHF, Elmacı, H and Kara, M (2017) Palaeozoic-Recent geological development and uplift of the Amanos Mountains (S Turkey) in the critically located northwesternmost corner of the Arabian continent, Geodinamica Acta 29, 103–38.CrossRefGoogle Scholar
Eaton, S and Robertson, AHF (1993) The Miocene Pakhna Formation, southern Cyprus and its relationship to the Neogene tectonic evolution of the Eastern Mediterranean. Sedimentary Geology 86, 273–96.CrossRefGoogle Scholar
Finné, M, Holmgren, K, Sundqvist, HS, Weiberg, E and Lindblom, M (2011) Climate in the eastern Mediterranean, and adjacent regions, during the past 6000 years – a review. Journal of Archaeological Science 38, 3153–73.CrossRefGoogle Scholar
Fountoulis, I, Mariolakos, I and Ladas, I (2014) Quaternary basin sedimentation and geodynamics in SW Peloponnese (Greece) and late stage uplift of Taygetos Mt. Bolletino di Geofisica Teorica e Applicata 55, 303–24.Google Scholar
Frechen, M, Neber, A, Tsatskin, A, Boenigk, W and Ronen, A (2004) Chronology of Pleistocene sedimentary cycles in the Carmel coastal plain of Israel. Quaternary International 121, 41–52.CrossRefGoogle Scholar
Gallen, S, Wegmann, K, Bohnenstiehl, D, Pazzaglia, F, Brandon, M and Fassoulas, C (2014) Active simultaneous uplift and margin-normal extension in a forearc high, Crete, Greece. Earth and Planetary Science Letters 398, 11–24.CrossRefGoogle Scholar
Garzanti, E, Andò, S and Scutellà, M (2000) Actualistic ophiolite provenance: the Cyprus case. Journal of Geology 108, 199–218.CrossRefGoogle ScholarPubMed
Glover, C and Robertson, AHF (1998) Role of regional extension and uplift in the Plio-Pleistocene evolution of the Aksu Basin, SW Turkey. Journal of the Geological Society 155, 365–88.CrossRefGoogle Scholar
Gomez, B (1982) Observations on the fluvial geomorphology of the Vasilikos Valley. In Vasilikos Valley Project: Fourth Preliminary Report, [1979–1980] (ed. Todd, IA), pp. 67–74. Field Archaeology, vol. 9.Google Scholar
Gomez, B (1987) The alluvial terraces and fills of the lower Vasilikos Valley, in the vicinity of Kalavasos Cyprus. Transactions of the Institute of British Geographers, n.s. 12, 345–59.CrossRefGoogle Scholar
Harrison, RW, Newell, WL, Batıhanlı, H, Panayides, I, McGeehin, JP, Mahan, SA, Ozhur, A, Tsiolakis, E and Necdet, M (2004) Tectonic framework and Late Cenozoic tectonic history of the northern part of Cyprus: implications for earthquake hazards and regional tectonics. Journal of Asian Earth Sciences 23, 191–210.CrossRefGoogle Scholar
Harrison, RW, Tsiolakis, E, Stone, BD, Lord, A, Mcgeehin, JP, Mahan, SA and Chirico, P (2013) Late Pleistocene and Holocene uplift history of Cyprus: implications for active tectonics along the southern margin of the Anatolian microplate. In Geological Development of Anatolia and the Easternmost Mediterranean Region (eds Robertson, AHK, Parlak, O and Ünlügenç, UC), pp. 561–84. Geological Society of London, Special Publication no. 372.Google Scholar
Harvey, AM (2002) The role of base-level change in the dissection of alluvial fans: case studies from southeast Spain and Nevada. Geomorphology 45, 67–87.CrossRefGoogle Scholar
Harvey, AM, Mather, AE and Stokes, M (2005) Alluvial fans: geomorphology, sedimentology, dynamics – introduction. A review of alluvial-fan research. In Alluvial Fans: Geomorphology, Sedimentology, Dynamics (eds Harvey, AM, Mather, AE and Stokes, M), pp. 1–7. Geological Society of London, Special Publication no. 251.Google Scholar
Henson, FRS, Browne, RV and McGinty, J (1949) A synopsis of the stratigraphy and geological history of Cyprus. Quarterly Journal of the Geological Society 105, 1–41.CrossRefGoogle Scholar
Horton, BP, Kopp, RE, Garner, AJ, Hay, CC, Khan, NS, Roy, K and Shaw, TA (2018) Mapping sea-level change in time, space, and probability. Annual Review of Environment and Resources 43, 481–521. doi: 10.1146/annurev-environ-102017-025826.CrossRefGoogle Scholar
Hurst, MD, Mudd, SM, Walcott, R, Attal, M and Yoo, K (2012) Using hilltop curvature to derive the spatial distribution of erosion rates. Journal of Geophysical Research 117, 1–19.CrossRefGoogle Scholar
Jamieson, RA and Beaumont, C (2013) On the origin of orogens. Geological Society of America Bulletin 125, 1671–702.CrossRefGoogle Scholar
Jia, LY, Zhang, XJ, He, ZX, He, XL, Wu, FD, Zhou, YQ, Fu, LZ and Zhao, JX (2015) Late Quaternary climatic and tectonic mechanisms driving river terrace development in an area of mountain uplift: a case study in the Langshan area, Inner Mongolia, northern China. Geomorphology 234, 109–21.CrossRefGoogle Scholar
Jones, SJ, Frostick, LE and Astin, TR (2001) Braided stream and flood plain architecture: the Rio Vero Formation, Spanish Pyrenees. Sedimentary Geology 139, 229–60.CrossRefGoogle Scholar
Kinnaird, TC, Dixon, JE, Robertson, AHF, Peltenburg, E and Sanderson, DCW (2013) Insights on topography development in the Vasilikos and Dhiarizos Valleys, Cyprus, from integrated OSL and landscape studies, Mediterranean Archaeology and Archaeometry 13, 49–62.Google Scholar
Kinnaird, TC and Robertson, AHF (2013) Tectonic and sedimentary response to subduction and oblique collision in southern Cyprus, easternmost Mediterranean region. In Geological Development of the Anatolian Continent and Cyprus (eds Robertson, AHF, Parlak, O and Ünlügenç, U), pp. 585–615. Geological Society of London, Special Publication no. 372.Google Scholar
Kinnaird, TC, Robertson, AHF and Morris, A (2011) Timing of uplift of the Troodos Massif (Cyprus) constrained by sedimentary and magnetic polarity evidence. Journal of the Geological Society of London 168, 457–70.CrossRefGoogle Scholar
Kober, F, Zeilinger, G, Ivy-Ochs, S, Dolati, A, Smit, J and Kubik, PW (2013) Climatic and tectonic control on fluvial and alluvial fan sequence formation in the Central Makran Range, SE-Iran. Global Planetary Change 111, 133–49. doi: 10.1016/j.gloplacha.2013.09.003.CrossRefGoogle Scholar
Kourampas, A and Robertson, AHF (2000) Controls on Plio-Quaternary sedimentation within an active forearc region: Messenia Peninsula (SW Peloponnese), S. Greece. In Proceedings of the Third International Conference on the Geology of the Eastern Mediterranean (eds Panayides, I, Xenophonotos, C and Malpas, J), pp. 255–85. Nicosia: Geological Survey Department, Ministry of Agriculture and Natural Resources and Environment.Google Scholar
Kraus, MJ (1999) Paleosols in clastic sedimentary rocks: their geologic applications. Earth-Science Reviews 47, 41–70.CrossRefGoogle Scholar
Lambeck, K, Esat, TM and Potter, E (2002) Links between climate and sea levels for the past three million years. Nature 419, 199–206.CrossRefGoogle ScholarPubMed
Macklin, MG, Fuller, IC, Lewin, J, Maas, GS, Passmore, DG, Rose, J, Woodward, JC, Black, S, Hamlin, RHB and Rowan, JS (2002) Correlation of fluvial sequences in the Mediterranean basin over the last 200 ka and their relationship to climate change. Quaternary Science Reviews 21, 1633–41.CrossRefGoogle Scholar
Macleod, C and Murton, BJ (1993) Structure and tectonic evolution of the Southern Troodos Transform Fault Zone, Cyprus, In Magmatic Processes and Plate Tectonics (eds Prichard, HM, Alabaster, T, Harris, NBW and Neary), CR, pp. 41–176.Geological Society of London, Special Publication no. 76.Google Scholar
Maddy, D, Demir, T, Bridgland, DR, Veldkamp, A, Stemerdink, C, Van der Schriek, T and Westaway, R (2008) The Early Pleistocene development of the Gediz River, western Turkey: an uplift-driven, climate-controlled system? Quaternary International 189, 115–28.CrossRefGoogle Scholar
Main, CE, Roberston, AHF and Palamakumbura, RN (2016) Pleistocene geomorphological and sedimentary development of the Akaki River catchment (northeastern Troodos Massif) in relation to tectonic uplift versus climatic change. International Journal of Earth Science 105, 463–85.CrossRefGoogle Scholar
Massari, F, Capraro, L and Rio, CD (2007) Climatic modulation of timing of systems-tract development with respect to sea-level changes (Middle Pleistocene of Crotone, Calabria, southern Italy). Journal of Sedimentary Research 77, 461–8.CrossRefGoogle Scholar
McCallum, JE and Robertson, AHF (1990) Pulsed uplift of the Troodos Massif: evidence from the Plio-Pleistocene Mesaoria Basin. In Ophiolites Oceanic Crustal Analogues: Proceedings of the Symposium; “Troodos 1987” (eds Malpas, J, Moores, EM, Panayiotou, A and Xenophontos, C), pp. 217–30. Nicosia: Geological Survey Department, Cyprus.Google Scholar
McCallum, JE and Robertson, AHF (1995) Sedimentology of two fan delta systems in the Pliocene Pleistocene of the Mesaoria Basin, Cyprus. Sedimentary Geology 98, 215–44CrossRefGoogle Scholar
McCallum, JE, Scrutton, RA, Robertson, AHF and Ferrari, W (1993) Seismostratigraphy and Neo gene-Recent depositional history of the south central continental margin of Cyprus. Marine and Petroleum Geology 10, 426–38.CrossRefGoogle Scholar
Miall, AD (1996) The Geology of Fluvial Deposits. Berlin: Springer.Google Scholar
Morel, SW (1960) The Geology and Mineral Resources of the Apsiou-Akrotiri Area. Memoirs of the Geological Survey, Cyprus, no. 7, Part ll, pp. 51–83. Nicosia: Geological Survey Department, Cyprus.Google Scholar
Muhs, DR, Budahn, J, Avila, A, Skipp, G, Freeman, J and Patterson, DA (2010) The role of African dust in the formation of Quaternary soils on Mallorca, Spain and implications for the genesis of Red Mediterranean soils. Quaternary Science Reviews 29, 2518–43CrossRefGoogle Scholar
Nemec, W and Kazanci, N (1999) Quaternary colluvium in west-central Anatolia: sedimentary facies and palaeoclimatic significance. Sedimentology 46, 139–70.CrossRefGoogle Scholar
Nichols, GJ and Fisher, JA (2007) Processes, facies and architecture of fluvial distributary system deposits. Sedimentary Geology 195, 75–90.CrossRefGoogle Scholar
Palamakumbura, RN and Robertson, AHF (2016a) Pleistocene terrace formation related to surface tectonic uplift: example of the Kyrenia Range lineament in the northern part of Cyprus. Sedimentary Geology 339, 46–67.CrossRefGoogle Scholar
Palamakumbura, RN and Robertson, AHF (2016b) Pliocene–Pleistocene sedimentary-tectonic development of the Mesaoria (Mesarya) Basin in an incipient, diachronous collisional setting: facies evidence from the north of Cyprus. Geological Magazine 155, 997–1022. doi: 10.1017/S0016756816001072.CrossRefGoogle Scholar
Palamakumbura, RN, Robertson, AHF, Kinnaird, TC and Sanderson, DCW (2016a) Sedimentary development and correlation of Late Quaternary terraces in the Kyrenia Range, northern Cyprus, using a combination of sedimentology and optical luminescence data. International Journal of Earth Sciences (Geologische Rundschau) 105, 439–62.CrossRefGoogle Scholar
Palamakumbura, RN, Robertson, AHF, Kinnaird, TC, Van Calstern, P, Kroon, D and Tait, J (2016b) Quantitative dating of Pleistocene deposits of the Kyrenia Range, northern Cyprus: implications for timings, rates of uplift and driving mechanisms. Journal of the Geological Society 105, 1–41. doi.org/10.6084/m9.figshare.c.3260977.v1.Google Scholar
Pantazis, TM (1967) The Geology and Mineral Resources of the Pharmakas-Kalavasos Area. Memoirs of the Geological Survey, Cyprus no. 8.Google Scholar
Pantazis, TM (1973) A study of the secondary limestones (Havara and Kafkalla) of Cyprus. Geographical Chronicles II 4, 12–39.Google Scholar
Payne, AS and Robertson, AHF (1995) Neogene suprasubduction zone extension in the Polis graben system, west Cyprus. Journal of the Geological Society 152, 613–28.CrossRefGoogle Scholar
Poole, AJ and Robertson, AHF (1991) Quaternary uplift and sea-level change at an active plate boundary, Cyprus. Journal of the Geological Society 148, 909–21.CrossRefGoogle Scholar
Poole, A and Robertson, AHF (1998) Pleistocene Fanglomerate deposition related to uplift of the Troodos Ophiolite, Cyprus. In Proceedings of the Ocean Drilling Program, Scientific Results, vol. 160 (eds Robertson, AHF, Emeis, K-C, KRichter, C and Camerlenghi, A), pp. 544–69. College Station, Texas.Google Scholar
Poole, AJ and Robertson, AHF (2000) Quaternary marine terraces and aeolinites in coastal south and west Cyprus: implications for regional uplift and sea-level change. In Proceedings of the Third Internal Conference on the Geology of the Eastern Mediterranean (eds Panayides, I, Xenophontos, C and Malpas, J), pp. 105–23.Google Scholar
Poole, AJ, Shimmield, GB and Robertson, AHF (1990) Late Quaternary uplift of the Troodos ophiolite, Cyprus: uranium-series dating of Pleistocene coral. Geology 18, 894–7.2.3.CO;2>CrossRefGoogle Scholar
Pope, RJJ and Wilkinson, KN (2005) Reconciling the roles of climate and tectonics in Late Quaternary fan development on the Spartan piedmont, Creece. In Alluvial Fans: Geomorphology, Sedimentology, Dynamics (eds Harvey, AM, Mather, AE and Stokes, M), pp. 131–52. Geological Society of London, Special Publication no. 251.Google Scholar
Quigley, MC, Sandiford, M and Cupper, ML (2007) Distinguishing tectonic from climatic controls on range-front sedimentation. Basin Research 19, 491–505.CrossRefGoogle Scholar
Retallack, GJ (2001) Soils of the Past. An Introduction to Palaeopedology. Oxford: Blackwell Science, 404 pp.Google Scholar
Robertson, AHF (1976) Pelagic chalks and calciturbidites from the Lower Tertiary of the Troodos Massif. Journal of Sedimentary Petrology 46, 1007–16.Google Scholar
Robertson, AHF (1977a) Tertiary uplift history of the Troodos massif, Cyprus. Geological Society of America Bulletin 12, 1763–72.2.0.CO;2>CrossRefGoogle Scholar
Robertson, AHF (1977b) The origin and diagensis of cherts from Cyprus. Sedimentology 24, 11–30.CrossRefGoogle Scholar
Robertson, AHF (1990) Tectonic evolution of Cyprus. In Ophiolites Oceanic Crustal Analogues: Proceedings of the Symposium ‘Troodos 1987’ (eds Malpas, J, Moores, EM, Panayiotou, A and Xenophontos, C), pp. 235–52. Nicosia: Geological Survey Department of Cyprus.Google Scholar
Robertson, AHF, Eaton, S, Follows, EJ and McCallum, JE (1991) The role of local tectonics versus global sea-level change in the Neogene evolution of the Cyprus active margina. Special Publication of the International Association of Sedimentologists 12, 331–69.Google Scholar
Rose, J, Meng, X and Watson, C (1999) Palaeoclimate and palaeoenvironmental responses in the western Mediterranean over the last 140 ka: evidence from Mallorca, Spain. Journal of the Geological Society 156, 435–48.CrossRefGoogle Scholar
Sage, L and Letouzey, J (1990) Convergence of the African and Eurasian plates in the Eastern Mediterranean. In Petroleum and Tectonics in Mobile Belts (ed. Letouzey, J), pp. 49–68. Paris: Éditions Technip.Google Scholar
Schaetzl, RJ and Anderson, S (2005) Terra rossa soils of the Mediterranean. In Soils: Genesis and Geomorphology, p. 201. Cambridge: Cambridge University Press.CrossRefGoogle Scholar
Schanz, SA, Montgomery, DR, Collins, BD and Duvall, AR (2018) Multiple paths to straths: a review and reassessment of terrace genesis. Geomorphology 312, 12–23.CrossRefGoogle Scholar
Schildgen, TF, Cosentino, D, Bookhagen, B, Niedermann, S, Yildirim, C, Echtler, H, Wittmann, H and Strecker, MR (2012) Multiphased uplift of the southern margin of the Central Anatolian plateau, Turkey: a record of tectonic and upper mantle processes. Earth and Planetary Science Letters 317–318, 85–95.CrossRefGoogle Scholar
Schildgen, TF, Yıldırım, C, Cosentino, D and Strecker, MR (2014) Linking slab break-off, Hellenic trench retreat, and uplift of the Central and Eastern Anatolian plateaus. Earth Science Reviews 128, 147–68.CrossRefGoogle Scholar
Schirmer, W (1998) Havara on Cyprus – a surficial calcareous deposit. Eiszeitalter und Gegenwart 48, 110–17.Google Scholar
Schirmer, W, Weber, J, Bachtadse, V, BouDagher-Fadel, M, Heller, F, Lehmkuhl, F, Panayides, I and Schirmer, U (2010) Fluvial stacking due to plate collision and uplift during the Early Pleistocene in Cyprus. Central European Journal of Geosciences 12, 514–23.Google Scholar
Seyrek, A, Demir, T, Pringle, M, Yurtmen, S, Westaway, R, Bridgland, D, Beck, A and Rowbotham, G (2008) Late Cenozoic uplift of the Amanos Mountains and incision of the Middle Ceyhan river gorge, southern Turkey; Ar–Ar dating of the Duüzici basalt. Geomorphology 97, 321–55.CrossRefGoogle Scholar
Siddall, M, Chappell, J and Potter, E (2006) Eustatic sea level during past interglacials. Developments in Quaternary Science 7, 75–92.CrossRefGoogle Scholar
Soulas, JP (2002) Active tectonics in southern Cyprus: fundamentals of seismic risk analysis. In Proceedings: Earthquake Risk Minimization; International Conference (eds Petrides, G, Chrysostomou, C, Kyrou, K and Hadjigeorgiou, C), pp. 38–62. Nicosia: Geological Survey Department, Ministry of Agriculture, Natural Resources and Environment in Cooperation with the Ministry of the Interiors and the Technical Chamber of Cyprus.Google Scholar
Starkel, L (2003) Climatically controlled terraces in uplifting mountain areas. Quaternary Science Reviews 22, 2189–98.CrossRefGoogle Scholar
Waters, J, Jones, SJ and Armstrong, HA (2010) Climatic controls on late Pleistocene alluvial fans, Cyprus. Geomorphology 115, 228–51.CrossRefGoogle Scholar
Weber, J, Schirmer, W, Heller, F and Bachtadse, V (2011) Magnetostratigraphy of the Apalós Formation (early Pleistocene): evidence for pulsed uplift of Cyprus. Geochemistry, Geophysics, Geosystems 12, 1–13.CrossRefGoogle Scholar
Wegmann, KW and Pazzaglia, FJ (2009) Late Quaternary fluvial terraces of the Romagna and Marche Apennines, Italy: climatic, lithologic, and tectonic controls on terrace genesis in an active orogen. Quaternary Science Reviews 28, 137–65. doi: 10.1016/j.quascirev.2008.10.006.CrossRefGoogle Scholar
Westaway, R, Bridgland, DR, Sinha, R and Demir, T (2009) Fluvial sequences as evidence for landscape and climatic evolution in the Late Cenozoic: a synthesis of data from IGCP 518. Global Planetary Change 68, 237–53. doi: 10.1016/j.gloplacha.2009.02.009.CrossRefGoogle Scholar
Whittaker, CA (2012) How do landscapes record tectonics and climate? Lithosphere 4, 160–4.CrossRefGoogle Scholar
Zitter, T, Huguen, C and Woodside, J (2005) Geology of mud volcanoes in the eastern Mediterranean from combined sidescan sonar and submersible surveys. Deep-Sea Research Part I 52, 457–75.CrossRefGoogle Scholar
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