[1] لاهیجانی، ع. ح (1384) کارگاه آموزشی تاثیر نوسان تراز آب دریای خزر بر اکوسیستمهای ساحلی، دانشکده منابع طبیعی و علوم دریایی دانشگاه تربیت مدرس، 47 ص.
[2] موسوی روحبخش، م (1380) زمینشناسی دریای خزر، سـازمان زمـینشناسی کشور، طـرح تـدوین کـتاب زمینشناسی ایران، شماره 80، 254 ص.
[3] Al-Sharhan, A. S., and Kendall, C. G. St. C (2003) Holocene coastal carbonates and evaporates of the southern Persian Gulf and their ancient analogues. Earth- Science Reviews, v. 61, 191-243.
[4] Arthur, M. A., and Sageman, B. B (2005) Sea-level control on source-rock development: perspectives from the Holocene Black Sea, the mid-Cretaceous Western Interior Basin of North America, and The late Devonian Appalachian Basin. In: Harris, N.B. (Eds.), The deposition of organic carbon rich sediments: models, mechanisms, and consequences. SP. Pub. No. 82 SEPM, Tulsa, pp. 35-59.
[5] Awosika, L. F., Al-Ghadban, A. N., Ahmad, M. H. & Adegbia, A. F (1993) Assesment of sediment foraminifera and current monitoring data collected during the 100 day ROPME, IOC/NOAA cruise; implications for transport dynamics in the ROPME sea area. – Final report of the scientific workshop on results of the RIV MT. Mitchell cruise in the ROPME sea area, 1: 241-252.
[6] Baudin, F., Disnar, J. R., Martine, P., and Dennielou, B (2010) Distribution of the organic matter in the channel-Levees systems of the Congo mud-rich deep sea fan (West Africa): implication fordeep offshore petroleum source rocks and global carbon cycle. Marine and Petroleum Geology, v. 27, 995-1010.
[7] Behbahani, R., Hosseinyar, G., Lak, R (2015) The controlling parameters on organic matter preservation within the bottom sediments of the northern part of the Persian Gulf. N. Jb. Geol. Palaont. Abh., v. 276, 267-283.
[8] Brunet, M. F.; Korotaev, O.; Ershov, A. V.; Nikishin, A. M (2003) The South Caspian Basin: a review of its evolution from subsidence modeling. Sedimentary geology, v. 156, 119-148.
[9] Creaney, S., and Passey, Q. R (1993) Recurring patterns of total organic carbon and source rock quality within a sequence stratigraphic framework. American Association of Petroleum Geologist Bulletin, v. 77, 386- 401.
[10] Demaison, G.J., Murris, R.J., and Huizinga, B.J (1984) Petroleum geochemistry and basin evaluation. AAPG Memori 35.
[11] Folk, R. L (1974) Petrology of sedimentary rocks. Texas (Hemphill publishing company) 182p.
[12] Gani, M. R (2003) Crisis for a general term referring to all types of sediment gravity flow deposits: gravite: Geological Society of America, Abstracts with programs, v. 34, No. 7, 171 p.
[13] Goddard, D. A., Mancini, E. A., Talukar, S. C. & Horn, M (1997) Bossier – Hanesvill shale, North Louisian Salt basin. – Lousiana State University, Baton Rouge, Louisiana, center for energy, PDF file, http:// www. Api. Ning. Com/ files, 46. Accessed 2 Jun 1997.
[14] Harris, N.B (2005) The deposition of organic carbon rich sediments: models, mechanisms and consequences- introduction. In: Harris, N.B. (Eds.), The deposition of organic carbon rich sediments: models, mechanisms, and consequences. SP. Pub. No. 82 SEPM, Tulsa, pp. 1-5.
[15] Harris, N.B., Freeman, K.H., Pancost, R.D., Mitchell, G.D., White, T.S., Bate, R.H (2005) Patterns of organic carbon enrichment in a lacustrine source rock in relation to paleo-lake level, Congo Basin, West Africa. In: Harris, N.B. (Eds.), The deposition of organic carbon rich sediments: models, mechanisms, and consequences. SP. Pub. No. 82 SEPM, Tulsa, pp. 103-123.
[16] Hunt, J. M (1995) Petroleum geochemistry and geology. Freeman, New York, 743 p.
[17] Ibach, L.E.J (1982)Relationship between sedimentation rate and total organic carbon content in ancient marine sediments. AAPG Bulletin, v. 66, 170- 188.
[18] Langford, F. F. & Blanc-Valleron, M. M (1990) Interpreting Rock-Eval pyrolysis data using graphs of pyrolizable hydrocarbons vs. total organic carbon. – American Association of Petroleum Geologists Bulletin, v. 74: 799-804.
[19] Lewis, C. F. M., Mayer, L. A., Mukhopadhyay, P. K., Kruge, M. A., and Coakley, J. P (2000) Multi beam sonar backscatter lineaments and anthropogenic organic components in lacustrine silty clay, evidence of shipping in western lake Ontario. International Journal of coal Geology, v. 43, 307-324.
[20] Leroy, S.A.G., Tudryn, A., Chalie, F., Merino, L.L., Gasse, F (2013) From the Allerd to the mid-Holocene: palynological evidence from the south basin of the Caspian Sea. Quaternary Science Reviews, v.78, 77-97.
[21] Leroy, S.A.G., Marretb, F., Gibertc, E., Chalie´d, F., Reysse, J.-L., Arpef, K (2007) River inflow and salinity changes in the Caspian Sea during the last 5500 years. Quaternary Science Reviews, v. 26, 3359–3383.
[22] Meyers, P. A (2003) Applications of organic geochemistry to paleolimnological reconstruction: a summary of examples from the Laurentian Great Lakes. – Organic Geochemistry, v. 34: 261- 289.
[23] Meyers, P. A (1997) Organic geochemical proxies of paleoceanographic, paleolimnologic, and paleoclimatic processes. Organic Geochemistry, v.27, 213-250.
[24] Morton, A. M., Allen, M., Simmons, F., Spathopoulos, J., Still, D., Hinds, H., Ismalzadeh, A., Kroonenberg, S (2003) Provenance patterns in a neotectonic basin: Pliocene and Quaternary sediment supply to the South Caspian. Basin research, v.15, 321-337.
[25] Nichols, G (2009) Sedimentology and stratigraphy, 2nd edition, Chichester, UK; Blackwell Science, 432 p.
[26] Paropkari, A., Prakash, C., and Mascarenhas, A (1993) New evidence for enhanced preservation of organic carbon in content with oxygen minimum zone on the Western continental slope of India. Marin geology, v. 111, 7-13.
[27] Patience, A. J., Lallier-Verges, E., Alberic, P., Desprairies, A. & Tribovillard, N (1996) Relationships between organo-mineral and early diagenesis in the Lacustrine environment: A study of surficial sediments from the Lac du Bouchet (France).- Quaternary Science Reviews, v.15: 213-221.
[28] Pratima, M., Kessarkar, L., and Purchandra, R (2007) Organic carbon in sediments of the southwestern margin of India: influence of productivity and Monsoon variability during the late Quaternary. Journal Geological Society of India, v. 69, 42-52.
[29] Reynolds, R. M (1993) Physical oceanography of the Gulf, Strait of Hormuz, and the Gulf of the Oman, Results from the Mt Mitchell expedition the 1991 Gulf war: coastal and marine environmental consequences. Marine Pollution Bulletin, v. 27: 35-59.
[30] Sifeddine, A., Gutierrez, L., Ortlieb, L., Boucher, H., Velazco, F., Field, D., Vargas, G., and Boussafir, M (2008) Laminated sediments from the central Peruvian continental slope: A 500 year record of upwelling system produvtivity, terrestrial run off and redox conditions. Progress in Oceanography, v. 79, 190- 197.
[31] Tsuchida, K., Okui, A., Yamade, Y., Yamazaki, N., and Iwahashi, R (2005) The application of alinked physical ocean circulation-ecosystem model to prediction of organic-carbon sedimentation in lake Tanganyika, East African Rift system. In: Harris, N.B. (Eds.), The deposition of organic carbon rich sediments: models, mechanisms, and consequences. SP. Pub. No. 82 SEPM, Tulsa, pp. 243-259.
[32] Tuzhilkin, V. S., Katunin, D. N., and Nalbandov, Y. R (2005) Natural chemistry of Caspian Sea waters. In: Hutzinger, O., (Eds.), the handbook of environmental chemistry, v.5, water pollution, part p, 83-108.
[33] Tuzhilkin, V. S., and Kosarev, A. N (2005) Thermohaline structure and general circulation of the Caspian Sea waters. In: Hutzinger, O., (Eds.), the handbook of environmental chemistry, v.5, water pollution, part p, 33-57.
[34] Tyson, R.V (2001) Sedimentation rate, dilution, preservation and total organic carbon, some results of a modeling study. Organic Geochemistry, v. 32, 333- 339.
)