THE SAILING SEASON of the INDIAN OCEAN Mariners Of

Total Page:16

File Type:pdf, Size:1020Kb

THE SAILING SEASON of the INDIAN OCEAN Mariners Of chapter five THE SAILING SEASON OF THE INDIAN OCEAN Mariners of the Near East had been venturing on to the Erythraean Sea— the name by which Graeco-Roman writers referred to the more northerly reaches of the Indian Ocean and which include the Red Sea, the Arabian Sea, and the Gulfs of Aden and Arabia—throughout antiquity.1 However, it is only during the rst century ad that we are provided with detailed information regarding the nature of maritime trade in the northern waters of the Indian Ocean, through the sixth book of Pliny’s Naturalis Historia, and in the anonymously authored Periplus Maris Erythraei (to be referred to throughout the rest of this chapter as the Periplus). While the latter trans- lates as ‘A Sailing Round the Erythraean Sea’, it was noted by Casson that the title of the work is somewhat misleading for the text is primarily focused not on maritime conditions or navigational concerns but appears instead to be ‘ rst and foremost a guide for merchants,’ in which ‘the emphasis is overwhelmingly on trading information.’ It is this focus on trade which led Casson to conclude that the Periplus was probably written (in Greek) by a merchant out of Egypt and was based, at least in part, on personal obser- vation.2 There was certainly a demand for information regarding maritime trade across the Erythraean Sea during the early decades of the Roman Principate, with Strabo referring to the ‘large eets’ of commercial ships which, from at least the time of Augustus, were making voyages from Roman Egypt, sailing down the Red Sea and into the Gulf of Aden, from where they would venture out on to the Arabian Sea. Some of these merchant vessels would sail south and make for the trading ports along the African coast; other ships exiting the Gulf of Aden would instead have their prows turned to face eastwards and every year ‘as many as one hundred and 1 Prior to the Roman Imperial period, there are literary references to Egyptians, Phoeni- cians and Hellenistic Greeks trading with East Africa, while, as early as the third millen- nium bc, Babylon had trading links to both Africa and India (Casson 1995: 20f.; Oppenheim 1954). 2 Casson 1989: 7f.; 1991a. 214 chapter five twenty vessels were sailing from Myos Hormos [modern Quseir al Quadim, on the Egyptian Red Sea coast] to India.’3 Evidence for the ancient maritime trading links between the Mediter- ranean and India is also to be found in the archaeological record, most notably from the site of Arikamedu near Pondicherry on the Coromandel Coast of south-eastern India.4 Excavated remains of Mediterranean pottery assemblages recovered from the site indicate it was used as a port-of-trade by Graeco-Roman merchants from at least the second half of the second century bc, while the settlement appears to have reached its trading peak during the early years of the Principate, thus closely linking it to the upsurge in maritime trade between Egypt and India indicated by the literature from this time.5 While it seems that commercial contacts between the Mediter- ranean and India declined during the later Empire, the Peutinger Table still records the existence of a temple dedicated to the Imperial cult at the city of Muziris on the west coast of India. Recent nds of late antique and early medieval pottery from sites such as Pattnam on India’s Malabar Coast also provide an indication that contact across the Arabian Sea was maintained throughout late antiquity and even into the Middle Ages.6 The archaeologi- cal and textual evidence therefore indicate that ancient exchange between the Mediterranean and India involved ‘a seagoing commerce of signi cant scale and sustained duration.’7 Of principal interest to this study, however, is not so much the scale or longevity of the trade between the Mediterranean and India, but rather the 3 Geography, 2.5.12. See also 17.1.13. For the results of recent excavations conducted at the site of Myos Hormos, see Peacock & Blue 2006. 4 E.g. Begley et al 1996; Suresh 2007; Wheeler 1954: 145f. 5 For pottery analysis from Arikamedu, see Will 1991; 1996. It is also interesting to note that Tamil Sangam literature dating to the rst and second centuries ad also makes frequent reference to foreigners from the west acting not only as merchants but also mercenaries and craftsmen (see Rashe 1978: 645; Rajan 1988). While it cannot be assumed that all or indeed any of these were of Mediterranean origin since the Tamil term Yavana refers to any western foreigners, be they of Mediterranean, African or Arabian extraction, it is probably of no coincidence that, during the rst two centuries ad, pottery and glassware from this region of south-west India exhibit strong Mediterranean stylistic inuences (Rashke 1978: 671). Indeed, it has recently been pointed out that in the ancient Tamil poem, the Purananuru, composed c. 200bc–ad100, ‘the poet urges the local king to taste the sweet teral (wine), brought by the lovely ships of the Yavanas and served on trays of chiselled gold, by beautiful damsels with sparkling wrists. These pointed references to the Yavanas bringing gold and wine to south India indicate that the Yavanas were primarily Romans, because we know from other sources that gold and wine were among the chief commodities exported from the Mediterranean region to India’ (Suresh 2010: 29). 6 Raschke 1978: 673; Rauth 2003: 101; Shajan et al 2008. 7 Rauth 2003: 99..
Recommended publications
  • 000000548.Sbu.Pdf
    SSStttooonnnyyy BBBrrrooooookkk UUUnnniiivvveeerrrsssiiitttyyy The official electronic file of this thesis or dissertation is maintained by the University Libraries on behalf of The Graduate School at Stony Brook University. ©©© AAAllllll RRRiiiggghhhtttsss RRReeessseeerrrvvveeeddd bbbyyy AAAuuuttthhhooorrr... Archaeological Investigation of the Buri Peninsula and Gulf of Zula, Red Sea Coast of Eritrea A Dissertation Presented by Amanuel Yosief Beyin to The Graduate School in partial fulfillment of the requirements for the degree of Doctor of Philosophy in Anthropology (Archaeology) Stony Brook University May 2009 Stony Brook University The Graduate School Amanuel Yosief Beyin We, the dissertation committee for the above candidate for the Doctor of Philosophy degree, hereby recommend acceptance of this dissertation. John J. Shea Associate Professor, Anthropology David J. Bernstein Associate Professor, Anthropology John G. Fleagle Distinguished Professor, Anatomical Sciences Steven A. Brandt Associate Professor, Anthropology University of Florida, Gainesville This dissertation is accepted by the Graduate School Lawrence Martin Dean of the Graduate School ii Abstract of the Dissertation Archaeological Investigation of the Buri Peninsula and Gulf of Zula, Red Sea Coast of Eritrea by Amanuel Yosief Beyin Doctor of Philosophy in Anthropology (Archaeology) Stony Brook University 2009 This dissertation reports the results of archaeological survey and excavations on the Buri Peninsula and Gulf of Zula, Red Sea coast of Eritrea. Its primary goals were to seek evidence for prehistoric human settlement, and to define the geological, chronological and cultural contexts of the sites. The Red Sea Coast of Africa is thought to be an important refugium for humans dispersing from the interior of East Africa into Arabia and the Levant.
    [Show full text]
  • Historical Ties:  India’S Relations with Africa Date Back Several Centuries
    EDITORIAL 30TH JULY 2019 GREAT GAME IN AFRICA Context Defence Minister’s recent visit to Mozambique, which is a good moment to reflect on the growing significance of the East African coastal countries and the islands off it for the geopolitics of the Indo-Pacific. Introduction: During the visit to Mozambique, he is expected to sign a number of agreements, including on hydrographic survey, sharing of white shipping information and the monitoring of its exclusive zone. He is also expected to deliver two fast patrol naval craft to the country as part of India’s expanding security cooperation with Mozambique. India and Africa - Historical Ties: India’s relations with Africa date back several centuries. The presence of Indians in East Africa is documented in the 'Periplus of the Erythraean Sea' or Guidebook of the Red Sea by an ancient Greek author written in 60 AD. The geographical proximity and easy navigability in Indian Ocean resulted in well- established trade network between India and the Swahili Coast predating European exploration. More concrete relation between India and Africa begins to emerge during the Islamic age which is evident through the accounts of Venetian traveller Marco Polo. Political connection during the colonial era was linked through M.K Gandhi who began his political career in South Africa, became the leader of colonized and established Indian Natal Congress in 1894. After India got independent, it raised voice for African liberation taking their case to all the available international forums. End of racial struggle and decolonization became the rallying point of India–Africa relations. India was a forerunner as a champion of the interests of the developing countries from Africa, particularly through the Bandung Declaration of 1955, the Group of 77, and the Non-Aligned Movement (NAM).
    [Show full text]
  • DEEP SEA LEBANON RESULTS of the 2016 EXPEDITION EXPLORING SUBMARINE CANYONS Towards Deep-Sea Conservation in Lebanon Project
    DEEP SEA LEBANON RESULTS OF THE 2016 EXPEDITION EXPLORING SUBMARINE CANYONS Towards Deep-Sea Conservation in Lebanon Project March 2018 DEEP SEA LEBANON RESULTS OF THE 2016 EXPEDITION EXPLORING SUBMARINE CANYONS Towards Deep-Sea Conservation in Lebanon Project Citation: Aguilar, R., García, S., Perry, A.L., Alvarez, H., Blanco, J., Bitar, G. 2018. 2016 Deep-sea Lebanon Expedition: Exploring Submarine Canyons. Oceana, Madrid. 94 p. DOI: 10.31230/osf.io/34cb9 Based on an official request from Lebanon’s Ministry of Environment back in 2013, Oceana has planned and carried out an expedition to survey Lebanese deep-sea canyons and escarpments. Cover: Cerianthus membranaceus © OCEANA All photos are © OCEANA Index 06 Introduction 11 Methods 16 Results 44 Areas 12 Rov surveys 16 Habitat types 44 Tarablus/Batroun 14 Infaunal surveys 16 Coralligenous habitat 44 Jounieh 14 Oceanographic and rhodolith/maërl 45 St. George beds measurements 46 Beirut 19 Sandy bottoms 15 Data analyses 46 Sayniq 15 Collaborations 20 Sandy-muddy bottoms 20 Rocky bottoms 22 Canyon heads 22 Bathyal muds 24 Species 27 Fishes 29 Crustaceans 30 Echinoderms 31 Cnidarians 36 Sponges 38 Molluscs 40 Bryozoans 40 Brachiopods 42 Tunicates 42 Annelids 42 Foraminifera 42 Algae | Deep sea Lebanon OCEANA 47 Human 50 Discussion and 68 Annex 1 85 Annex 2 impacts conclusions 68 Table A1. List of 85 Methodology for 47 Marine litter 51 Main expedition species identified assesing relative 49 Fisheries findings 84 Table A2. List conservation interest of 49 Other observations 52 Key community of threatened types and their species identified survey areas ecological importanc 84 Figure A1.
    [Show full text]
  • Geological Evolution of the Red Sea: Historical Background, Review and Synthesis
    See discussions, stats, and author profiles for this publication at: https://www.researchgate.net/publication/277310102 Geological Evolution of the Red Sea: Historical Background, Review and Synthesis Chapter · January 2015 DOI: 10.1007/978-3-662-45201-1_3 CITATIONS READS 6 911 1 author: William Bosworth Apache Egypt Companies 70 PUBLICATIONS 2,954 CITATIONS SEE PROFILE Some of the authors of this publication are also working on these related projects: Near and Middle East and Eastern Africa: Tectonics, geodynamics, satellite gravimetry, magnetic (airborne and satellite), paleomagnetic reconstructions, thermics, seismics, seismology, 3D gravity- magnetic field modeling, GPS, different transformations and filtering, advanced integrated examination. View project Neotectonics of the Red Sea rift system View project All content following this page was uploaded by William Bosworth on 28 May 2015. The user has requested enhancement of the downloaded file. All in-text references underlined in blue are added to the original document and are linked to publications on ResearchGate, letting you access and read them immediately. Geological Evolution of the Red Sea: Historical Background, Review, and Synthesis William Bosworth Abstract The Red Sea is part of an extensive rift system that includes from south to north the oceanic Sheba Ridge, the Gulf of Aden, the Afar region, the Red Sea, the Gulf of Aqaba, the Gulf of Suez, and the Cairo basalt province. Historical interest in this area has stemmed from many causes with diverse objectives, but it is best known as a potential model for how continental lithosphere first ruptures and then evolves to oceanic spreading, a key segment of the Wilson cycle and plate tectonics.
    [Show full text]
  • IBF List of Designated Risk Areas October 2020
    IBF LIST of designated risk areas, with applicable benefits (as of 1st November 2020): 1) IBF Warlike Operations Area – 12 nm. off the mainland Yemeni Coast, excluding Maritime Security Transit Corridor (MSTC) in the Red Sea - Charts 1 and 2a bonus equal to basic wage, payable for 5 days minimum + per day if longer; doubled compensations for death and disability; right to refuse sailing, with repatriation at company’s cost and compensation equal to 2 month’s basic wage 1a) IBF Warlike Operations Area – all ports in Yemen – Chart 2a bonus equal to basic wage, payable for 5 days minimum + per day if longer; doubled compensations for death and disability; right to refuse sailing, with repatriation at company’s cost and compensation equal to 2 month’s basic wage 2) “IBF High Risk Area” – Gulf of Aden + 12 nm. off Somali East Coast (Shown in red shade on Chart 2 below, excluding the Internationally Recognized Transit Corridor (IRTC) as detailed in Chart 2a) bonus equal to basic wage, payable for the actual duration of stay / transit; doubled compensations for death and disability; right to refuse sailing, with repatriation at company’s cost increased BMP level 3) “IBF Extended Risk Zone” – West Indian Ocean and the Red Sea, up to the Yemen/Saudi Arabia border at 16⁰ 22’N (shown on chart 2a and 2b) and including the MSTC (shown on charts 1 and 3) but excluding the Warlike Operations Areas and the High Risk Area designated in 1, and 2a above. bonus equal to basic wage, payable only on the day the vessel is attacked; doubled compensations
    [Show full text]
  • Structure and Transport of the East African Coastal Current
    See discussions, stats, and author profiles for this publication at: https://www.researchgate.net/publication/248793481 Structure and transport of the East African Coastal Current Article in Journal of Geophysical Research Atmospheres · January 1991 DOI: 10.1029/91JC01942 CITATIONS READS 48 209 3 authors, including: Michele Fieux Pierre and Marie Curie University - Paris 6 56 PUBLICATIONS 1,894 CITATIONS SEE PROFILE Some of the authors of this publication are also working on these related projects: It is in a book: " L'océan à découvert " , 321 p. , sept 2017, CNRS Editions View project All content following this page was uploaded by Michele Fieux on 09 June 2018. The user has requested enhancement of the downloaded file. JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 96, NO. C12, PAGES 22,245-22,257, DECEMBER 15, 1991 Structure and Transport of the East African Coastal Current JOHN C. SWALLOW Drakewalls, Gunnislake, Cornwall, England FRIEDRICH SCHOTT lnstitut fiir Meereskunde an der Universitiit Kiel, Kiel, Germany MICH•,LE FIEUX Laboratoire d'Oc•anographie Dynamique et de Climatologie, Universit• Paris VI, Paris The East African Coastal Current (EACC) runs northward throughout the year between latitudes 11øSand 3øS, with surfacespeeds exceeding 1 m s-1 in northernsummer. Mean transport from five sectionsnear 4ø-5øS is 19.9Sv (1 Sv -- 106 m3 s-1) northwardin theupper 500 dbar, out to 120km offshore. Below that, between 500 and 1000 dbar, there appears to be a weak variable transport of the order of 1 Sv. Comparing transports in the EACC with those in the boundary current north of Madagascar, it seems that most of the water in the upper 300 dbar of the northern branch of the South Equatorial Current goes into the EACC.
    [Show full text]
  • Djibouti: Z Z Z Z Summary Points Z Z Z Z Renewal Ofdomesticpoliticallegitimacy
    briefing paper page 1 Djibouti: Changing Influence in the Horn’s Strategic Hub David Styan Africa Programme | April 2013 | AFP BP 2013/01 Summary points zz Change in Djibouti’s economic and strategic options has been driven by four factors: the Ethiopian–Eritrean war of 1998–2000, the impact of Ethiopia’s economic transformation and growth upon trade; shifts in US strategy since 9/11, and the upsurge in piracy along the Gulf of Aden and Somali coasts. zz With the expansion of the US AFRICOM base, the reconfiguration of France’s military presence and the establishment of Japanese and other military facilities, Djibouti has become an international maritime and military laboratory where new forms of cooperation are being developed. zz Djibouti has accelerated plans for regional economic integration. Building on close ties with Ethiopia, existing port upgrades and electricity grid integration will be enhanced by the development of the northern port of Tadjourah. zz These strategic and economic shifts have yet to be matched by internal political reforms, and growth needs to be linked to strategies for job creation and a renewal of domestic political legitimacy. www.chathamhouse.org Djibouti: Changing Influence in the Horn’s Strategic Hub page 2 Djibouti 0 25 50 km 0 10 20 30 mi Red Sea National capital District capital Ras Doumeira Town, village B Airport, airstrip a b Wadis ERITREA a l- M International boundary a n d District boundary a b Main road Railway Moussa Ali ETHIOPIA OBOCK N11 N11 To Elidar Balho Obock N14 TADJOURA N11 N14 Gulf of Aden Tadjoura N9 Galafi Lac Assal Golfe de Tadjoura N1 N9 N9 Doraleh DJIBOUTI N1 Ghoubbet Arta N9 El Kharab DJIBOUTI N9 N1 DIKHIL N5 N1 N1 ALI SABIEH N5 N5 Abhe Bad N1 (Lac Abhe) Ali Sabieh DJIBOUTI Dikhil N5 To Dire Dawa SOMALIA/ ETHIOPIA SOMALILAND Source: United Nations Department of Field Support, Cartographic Section, Djibouti Map No.
    [Show full text]
  • General: Anonymous. Periplus Maris Erythraei (Or 'Voyage Around The
    General: Anonymous. Periplus Maris Erythraei (or ‘Voyage around the Erythraean Sea’). L. Casson. The Periplus Maris Erythraei: Text with Introduction, Translation, and Commentary. Princeton (1989). Cosmas Indicopleustes. Christian Topography. Boivin, N., Blench, R., & Fuller, D. (2009). Archaeological, linguistic and historical sources on ancient seafaring: A multidisciplinary approach to the study of early maritime contact and exchange in the Arabian Peninsula. In M. Petraglia & J. Rose (Eds.), The evolution of human populations in Arabia (pp. 251–278). New York: Springer. S. Faller. "The World According to Cosmas Indicopleustes—Concepts and Illustrations of an Alexandrian Merchant and Monk." M. P. Fitzpatrick. "Provincializing Rome: The Indian Ocean Trade Network and Roman Imperialism." Journal of World History 22 (2011): 27–54. S. Sidebotham. "The Red Sea and Indian Ocean in the Age of the Great Empires." In A Companion to the Archaeology of the Ancient Near East, ed. D. Potts, 1041-1059. (2012). Week One: Roman Egypt and Late Antique Egypt K. Damgaard, "A Palestinian Red Sea Port on the Egyptian Road to Arabia: Early Islamic Aqaba and its Many Hinterlands." In L. Blue – J. Cooper – R. Thomas – J. Whitewright (eds.), Connected Hinterlands: Proceedings of the Red Sea Project IV Held at the University of Southampton, September 2008, 85-98. Oxford (2009). S. Sidebotham. "Trade in Roman Berenike." In Berenike and the Ancient Maritime Spice Route. Berkeley and Los Angeles (2011), 221–258. S. Sidebotham. "Other Emporia." In Berenike and the Ancient Maritime Spice Route, 175-194. Berkeley and Los Angeles (2011). J. Whitewright. "The Ships and Shipping of Indo-Roman Trade: A View from Egyptian Red Sea Ports." Herom 6 (2017): 137-172.
    [Show full text]
  • Searching for the Ancient Harbours of the Erythraean Sea Wertyuiopasdfghjklzxcvbnmqwertyui an Analytical Investigation
    qwertyuiopasdfghjklzxcvbnmqwerty uiopasdfghjklzxcvbnmqwertyuiopasd fghjklzxcv bnmqwertyuiopasdfghjklzx cvbnmqwertyuiopasdfghjklzxcvbnmq Searching for the Ancient Harbours of the Erythraean Sea wertyuiopasdfghjklzxcvbnmqwertyui An Analytical Investigation 30/9/2010 opasdfghjklzxcvbnmqwertyuiopasdfg Carmen Tânia Macleroy Obied hjklzxcvbnmqwertyuiopasdfghjklzxc vbnmqwertyuiopasdfghjklzxcvbnmq wertyuiopasdfghjklzxcvbnmqwertyui opasdfghjklzxcvbnmqwertyuiopasdfg hjklzxcvbnmqwertyuiopasdfghjklzxc vbnmqwertyuiopasdfghjklzxcvbnmq wertyuiopasdfghjklzxcvbnmqwertyui opasdfghjklzxcvbnmqwertyuiopasdfg Contents ACKNOWLEDGEMENTS ................................................................................................................................................................ 5 ABSTRACT .......................................................................................................................................................................... 10 CHAPTER 1 ........................................................................................................................................................................... 11 ͞,ĂƌďŽƵƌƐĂŶĚ/ŶĚŽ-ZŽŵĂŶdƌĂĚĞ͟ 1.1. Aims and Research Questions......................................................................................................................................... 11 1.1.1. PROPOSED RESEARCH ................................................................................................................................................. 11 1.1.2. AIMS .........................................................................................................................................................................
    [Show full text]
  • Mesoscale Eddies in the Gulf of Aden and Their Impact on the Spreading of Red Sea Outflow Water ⇑ Amy S
    Progress in Oceanography 96 (2012) 14–39 Contents lists available at SciVerse ScienceDirect Progress in Oceanography journal homepage: www.elsevier.com/locate/pocean Mesoscale eddies in the Gulf of Aden and their impact on the spreading of Red Sea Outflow Water ⇑ Amy S. Bower , Heather H. Furey Department of Physical Oceanography, Woods Hole Oceanographic Institution, Woods Hole, MA 02543, USA article info abstract Article history: The Gulf of Aden (GOA) in the northwestern Indian Ocean is the receiving basin for Red Sea Outflow Received 29 November 2010 Water (RSOW), one of the World’s few high-salinity dense overflows, but relatively little is known about Received in revised form 6 September 2011 spreading pathways and transformation of RSOW through the gulf. Here we combine historical data, Accepted 18 September 2011 satellite altimetry, new synoptic hydrographic surveys and the first in situ direct observations of subsur- Available online 10 October 2011 face currents in the GOA to identify the most important processes in the spreading of RSOW. The new in situ data sets were collected in 2001–2003 as part of the Red Sea Outflow Experiment (REDSOX) and consist of two CTD/LADCP Surveys and 49 one-year trajectories from acoustically tracked floats released at the depth of RSOW. The results indicate that the prominent positive and negative sea level anomalies frequently observed in the GOA with satellite altimetry are associated with anticyclonic and cyclonic eddies that often reach to at least 1000 m depth, i.e., through the depth range of equilibrated RSOW. The eddies dominate RSOW spreading pathways and help to rapidly mix the outflow water with the background.
    [Show full text]
  • First Record of the Red Sea Immigrant Chrysallida Fischeri (Hornung and Mermod, 1925) (Gastropoda: Pyramidellidae) from Greek Waters
    Aquatic Invasions (2007) Volume 2, Issue 2: 95-98 Open Access doi: http://dx.doi.org/10.3391/ai.2007.2.2.2 © 2007 The Author(s). Journal compilation © 2007 REABIC Research Article First record of the Red Sea immigrant Chrysallida fischeri (Hornung and . Mermod, 1925) (Gastropoda: Pyramidellidae) from Greek waters Paraskevi Louizidou1, Maria Thessalou-Legaki1 and Argyro Zenetos2* 1Department of Zoology - Marine Biology, School of Biology, University of Athens Panepistimiopolis, GR 15784, Athens, Greece 2Hellenic Centre for Marine Research, Institute of Oceanography, Anavissos 19013, Attica, Greece *Corresponding author E-mail: [email protected] Received: 5 March 2007 / Accepted: 12 March 2007 Abstract The Red Sea mollusc Chrysallida fischeri (Hornung and Mermod, 1925) was collected in 2005 off Makri, Rhodes, Greece. This is the first record of the species in the Aegean Sea. The presence of both live specimens and shells suggest that C. fischeri is well established in the area. Key words: Chrysallida fischeri, Mollusca, alien species, Lessepsian immigrant, Rhodes, Aegean Sea, Greece . See Corrigendum, Aquatic Invasions 2(3): 278 95 Louizidou et al. Introduction The genus Chrysallida is represented by 48 species in European waters (CLEMAM website), seven of which, namely C. brusinai (Cossmann 1921), C. suturalis (Philippi 1844), C. terebellum (Philippi 1844), C. pirinthella (Melvill 1910), C. maiae (Hornung and Mermod 1924), C. micronana (Hornung and Mermod 1924) and C. fischeri (Hornung and Mermod 1925), occur in the Mediterreanean (Mienis and Zaslow 2004, Öztürk and van Aartsen 2006). The last four originated from the Red Sea and were introduced in the 20th century via the Suez Canal (Gofas and Zenetos 2003, Öztürk and van Aartsen 2006).
    [Show full text]
  • The Red Sea Basin Province: Sudr-Nubia(!) and Maqna(!) Petroleum Systems
    U. S. Department of the Interior U. S. Geological Survey The Red Sea Basin Province: Sudr-Nubia(!) and Maqna(!) Petroleum Systems by Sandra J. Lindquist1 Open-File Report 99-50-A This report is preliminary and has not been reviewed for conformity with the U.S. Geological Survey editorial standards or with the North American Stratigraphic Code. Any use of trade names is for descriptive purposes only and does not imply endorsement by the U.S. government. 1 Consultant to U. S. Geological Survey, Denver, Colorado Page 1 of 21 The Red Sea Basin Province: Sudr-Nubia(!) and Maqna(!) Petroleum Systems2 Sandra J. Lindquist, Consultant to U.S. Geological Survey, Denver, CO World Energy Project October, 1998 FOREWORD This report is a product of the World Energy Project of the U.S. Geological Survey, in which the world has been divided into 8 regions and 937 geologic provinces for purposes of assessment of global oil and gas resources (Klett and others, 1997). These provinces have been ranked according to the discovered petroleum volumes within each; high- ranking provinces (76 “priority” provinces exclusive of the U.S.) and others with varying types and degrees of intrigue (26 “boutique” provinces exclusive of the U.S.) were chosen for appraisal of oil and gas resources. The petroleum geology of these non-U.S. priority and boutique provinces are described in this series of reports. A detailed report containing the assessment results for all provinces will be available separately. The Total Petroleum System concept is the basis for this assessment. A total petroleum system includes the essential elements and processes, as well as all genetically related hydrocarbons that occur in petroleum shows, seeps and accumulations (discovered and undiscovered), whose provenance is a pod or related pods of mature source rock (concept modified from Magoon and Dow, 1994).
    [Show full text]