Abstract
Neoproterozoic evolution of the Arabian-Nubian Shield (ANS) and East African Orogen (EAO), 870–541 Ma, spanned revolutionary changes in Earth Systems, including a supercontinent cycle (Rodinia break-up, opening/closing of the Mozambique Ocean, Gondwana assembly), extreme climate fluctuations between long-lived glacial episodes as postulated by the Snowball Earth Hypothesis (1992–2002), marked increases in oceanic and atmospheric oxygen levels, and expansion of the biosphere from simple microbial life to the inclusion of larger and more diverse multicellular organisms. Understanding of these Earth System transitions has advanced tremendously over the past two decades through the integration of global studies of Neoproterozoic sedimentary successions with refined geochronologic techniques. This approach applied to Neoproterozoic Snowball Earth (NSE) localities now indicates that Neoproterozoic glaciations included two global-scale (panglacial) episodes, the ~717–659 Ma Sturtian and ~650–640 to 635 Ma Marinoan glaciations—which together comprise the Cryogenian Period, and more regional episodes during the Ediacaran Period and possibly, albeit controversially, during the earlier Tonian Period. Recent geochronologic, geochemical, and sedimentologic studies of low metamorphic grade ANS successions substantially contribute to the global Neoproterozoic dataset and, along with recently revised age constraints for the Cryogenian Period, facilitate an updated assessment of how Neoproterozoic glaciations may have influenced the sedimentary record of the ANS during its development. Tonian and Sturtian glaciations would have occurred following Rodinian break-up and major phases of juvenile crust formation in arc/island arc settings of the Mozambique Ocean (870–690 Ma), while latent terrane accretion and magmatism were still active. Paleogeographic reconstructions for these intervals generally place the ANS at tropical latitudes, where chemical weathering rates of juvenile crust terranes would have been high. Evidence supporting Tonian glaciation in the ANS is unresolved, with banded iron formation (BIF) and possible glacial diamictite scattered over the Central Eastern Desert (CED) of Egypt, NW Arabia, and possible correlative units in NE Sudan, as strongest candidates based on available age control (~780–740 Ma) and lithologic compatibility with NSE episodes. New age constraints for some of these localities (i.e., Atud diamictite and Um Nar, El-Hadid, Um Ghamis, and Wadi Kareim BIF localities in the CED) now demonstrate that deposition coincided with the Sturtian panglacial interval. Strong evidence of Sturtian glaciation in the ANS also occurs at the top of the Tonian-early Cryogenian Tambien Group in Northern Ethiopia, where polymict diamictite (<719.7 ± 0.5 Ma) bearing clasts consistent with glacial transport transitionally overlies limestone with pre-Sturtian 87Sr/86Sr values of 0.7066. Diamictite clast compositions similar to lower Tambien Group units suggest derivation from Tambien Group source terranes within the ANS, such as may have developed during early structural emergence of the EAO and/or associated eustatic sea-level fall. Carbonate units preserving negative carbon isotope excursions correlated to the ~800 Ma Bitter Springs anomaly, ~737 Ma Islay anomaly, and ~720 Ma pre-Sturtian transition, demonstrate that the Tambien Group is an important archive for studying the Tonian transition to extreme climates of the Cryogenian. The Marinoan (~645–635 Ma) glaciation overlapped with incipient development of the EAO, resulting from convergence, uplift, and structural deformation of earlier formed arc and accreted arc terranes, as the Mozambique Ocean closed between cratonic fragments of West and East Gondwana. Because most of the ANS was likely elevated above sea level, the ANS/EAO had few depocenters capable of preserving Marinoan sedimentation. Some peripheral margin basins, such as Murdama and Furayh basins in Arabia, overlapped with the Marinoan glaciation, but their sedimentary records have not been systematically studied for glacigenic characteristics. The onset of sedimentation in some post-amalgamation basins of the northern ANS (e.g., Jibalah Group of NW Arabia and possible equivalents in Jordan and Israel) may have overlapped with the Marinoan glaciation or Marinoan sediments could have been subsequently reworked in alluvial systems and redeposited during early basin formation. Following continental collision (~630–600 Ma), Ediacaran glaciations would have coincided with continued shortening and orogenic uplift (~600–540 Ma), when vast alluvial fan systems transported sediments away from EAO highlands. Ediacaran paleogeographic reconstructions generally place the ANS at higher tropical or temperate latitudes in the S. Hemisphere that may have supported regional scale glaciation. Within post-amalgamation basins of the northern Arabian Shield, the Jibalah Group sedimentary record includes polymict conglomerate, matrix-supported diamictite, and occasional dropstones that could be glacigenic. Regional deposition, constrained between underlying shield rocks (likely ≤605 ± 5 Ma) and the overlying Lower Cambrian basal unconformity (~540–520 Ma) and confirmed by U–Pb zircon dating of volcanic intervals within several basins, would have spanned the ~580 Ma Gaskiers glaciation, the ~575–567 Ma Shuram negative carbon isotope excursion, and younger Ediacaran glaciations. Although highly variable, sedimentary fill in many basins begins as polymict conglomerate with increasing limestone abundance in the higher succession, possibly consistent with a marine transgression. Carbonate δ13C values in combination with detrital zircon ages indicate that the basal conglomerate units pre-date the Shuram anomaly and could correlate with the ~580 Ma Gaskiers glaciation. Post-glacial supersequences may have been similarly deposited throughout northern Gondwana (Israel, Jordan, Saudi Arabia, Oman). Metazoan trace and probable body fossils are documented in Dhaiqa and Jifn basins above conglomeratic strata (Mataar Fm and Jifn Polymictic Conglomerate) that have been prospectively correlated with the Gaskiers glaciation. The lowest fossil horizons are no younger than 577 ± 5 Ma (Jifn) and 569 ± 3 Ma (Dhaiqa), similar to the Newfoundland record, where Ediacaran fauna appear ~9.5 myr after the ~580 Ma Gaskiers glaciation (Pu et al. in Geology 44:955–958, 2016). Follow-up studies are needed to assess the timing and glacigenic affinity of conglomerate and diamictite units, and to establish if and when marine deposition occurred within the Jibalah Group. A conspicuous stratigraphic feature of the northern Gondwanan margin is the widespread occurrence of an erosional unconformity throughout North Africa and Arabia separating Neoproterozoic basement from Cambro-Ordovician age sandstone that was principally sourced from erosion of the EAO. Although EAO erosion would have initiated as soon as regional uplift began, the exceptional power of Marinoan and Ediacaran ice sheets acting on a Himalaya-scale orogen may have contributed to ~650–540 Ma beveling of the Afro-Arabian Peneplain.
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References
Abd El-Rahman Y, Gutzmer J, Li X-H, Siefert T, Li C-F, Ling X-X, Li J (2020) Not all Neoproterozoic iron formations are glaciogenic: sturtian-aged non-Rapitan exhalative iron formations from the Arabian-Nubian Shield. Miner Deposita 55:577–596
Abdelsalam MG, Stern RJ (1993) Tectonic evolution of the Nakasib suture, Red Sea Hills, Sudan: evidence for a late Precambrian Wilson Cycle. J Geol Soc London 150:393–404
Abdelsalam MG, Stern RJ (1996) Sutures and shear zones in the Arabian-Nubian shield. J Afr Earth Sc 23:289–310
Abdelsalam MG, Stern RJ, Copeland P, El Faki EM, El Hur B, Ibrahim FM (1998) The Neoproterozoic Keraf Suture in NE Sudan: Sinistral transpression along the eastern margin of West Gondwana. J. Geology 106:133–147
Abdelsalam MG, Abdel-Rahman EM, El-Faki EM, Al-Hur B, El-Bashier FRM, Stern RJ, Thurmond AL (2003) Neoproterozoic deformation in the northeastern part of the Saharan Metacraton, northern Sudan. Precambr Res 123:203–221
Abdo A, Avigad D, Gerdes A, Morag N, Vainer S (2020) Cadomian (ca. 550 Ma) magmatic and thermal imprint on the North Arabian-Nubian Shield (south and central Israel): new age and isotopic constraints. Precambr Res 346:105804
Aftabi A (2001) Introduction of Bandar Abbas iron ore as the newest type of Rapitan banded iron formation. J Min Metall 60–70:53–66 (in Persian with English abstract)
Alene M, Jenkin GRT, Leng MJ, Darbyshire DP (2006) The Tambien Group, Ethiopia: an early Cryogenian (ca. 800–735 Ma) Neoproterozoic sequence in the Arabian-Nubian Shield. Precambr Res 149:79–89
Alessio B, Blades M, Murray G, Thorpe B, Collins AS, Kelsey D, Foden JD, Payne J, Al-Khirbash S, Jourdan F (2017) Origin and tectonic evolution of the NE basement of Oman: a window into the Neoproterozoic accretionary growth of India? Geol Mag 155:1150–1174
Al-Husseini MI (2000) Origin of the Arabian Plate structures: Amar collision and Najd rift. GeoArabia 5:527–542
Al-Husseini MI (2011) Ediacaran-Cambrian middle east geologic time scale 2014—late ediacaran to early Cambrian (Infracambrian) Jibalah Group of Saudi Arabia. GeoArabia 16:69–90
Al-Husseini MI (2014) Ediacaran-Cambrian middle east geologic time scale 2014—proposed correlation of Oman’s Abu Mahara Supergroup and Saudi Arabia’s Jibalah Group. GeoArabia 19:107–132
Al-Husseini MI (2015) Middle east geologic time scale 2015 Ediacaran and Cambrian Periods. J Middle East Petrol Geosci 20:511–528
Ali KA, Stern RJ, Manton WI, Kimura J-I, Khamees HA (2009) Geochemistry, Nd isotopes and U–Pb SHRIMP zircon dating of Neoproterozoic volcanic rocks from the Central Eastern Desert of Egypt: new insights into the ~750 Ma crust-forming event. Precambr Res 171:1–22
Ali KA, Stern RJ, Manton WI, Johnson PR, Mukherjee SK (2010a) Neoproterozoic diamictite in the Eastern Desert of Egypt and Northern Saudi Arabia: evidence of ~750 Ma glaciation in the Arabian-Nubian Shield. Int J Earth Sci 90:705–726
Ali KA, Stern RJ, Manton WI, Kimura J-I, Whitehouse M, Mukherjee SK, Johnson PR, Griffin WR (2010b) Geochemical, U–Pb zircon and Nd isotopic investigations of the Ghawjah Metavolcanic rocks, Northwestern Saudi Arabia. Lithos 120:379–392
Allen PA (2007) The Huqf Supergroup of Oman: basin development and context for Neoproterozoic glaciation. Earth-Sci Rev 84:139–185
Allen PA, Rieu R, Etienne JL, Matter A, Cozzi A (2011a) The Ayn formation of the Mirbat Group, Dhofar, Oman. In: Arnaud E et al. (eds) The geological record of Neoproterozoic glaciations. Geological Society of London Memoir 36, 239–249
Allen PA, Leather J, Brasier MD, Rieu R, Mccarron M, Le Guerroué E, Etienne JL, Cozzi A (2011b) The Abu Mahara Group (Ghubrah and Fiq formations), Jabal Akhdar, Oman. In: Arnaud E et al. (eds) The geological record of Neoproterozoic glaciations. Geological Society of London Memoir 36, 251–261
Antcliffe J (2013) Questioning the evidence of organic compounds called sponge biomarkers. Paleontology 56:917–925
Arkin Y, Beyth M, Dow DB, Levitte D, Haile T, Hailu T (1971) Geological map of Mekele Sheet area ND37-11 Tigre province. Imperial Ethiopian Government, Ministry of Mines. Geological Survey of Ethiopia. Scale 1:250,000
Asmerom Y, Jacobsen SB, Knoll AH, Butterfield NJ, Swett K (1991) Strontium isotopic variations of Neoproterozoic seawater: implications for crustal evolution. Geochim Cosmochim Acta 55:2883–2894
Asrat A, Barbey P, Ludden JN, Reisberg L, Gleizes G, Ayalew D (2004) Petrology and isotope geochemistry of the Pan-African Negash Pluton, northern Ethiopia: mafic-felsic magma interactions during the construction of shallow-level calc-alkaline plutons. J Petrol 45:1147–1179
Avigad D, Gvirtzman Z (2009) Late Neoproterozoic Arabian—rise and fall of the northern Nubian Shield: the role of lithospheric mantle delamination and subsequent thermal subsidence. Tectonophysics 477:217–228
Avigad D, Kolodner K, McWilliams M, Persing H, Weissbrod T (2003) Origin of northern Gondwana Cambrian sandstone revealed by detrital zircon SHRIMP dating. Geology 31:227–230
Avigad D, Sandler A, Kolodner K, Stern RJ, McWilliams M, Miller N, Beyth M (2005) Mass Cambro production of Ordovician quartz-rich sandstone as a consequence of chemical weathering of Pan-African terranes: environmental implications. Earth Planet Sci Lett 240:818–826
Avigad D, Stern RJ, Beyth M, Miller N, McWilliams M (2007) Detrital zircon U–Pb geochronology of Cryogenian diamictites and lower Palaeozoic sandstone in Ethiopia (Tigrai): age constraints on Neoproterozoic glaciation and crustal evolution of the southern Arabian-Nubian Shield. Precambr Res 154:88–106
Bailo E, Schandelmeier H, Franz G, Sun C-H, Stern RJ (2003) Plutonic and metamorphic rocks from the Keraf Suture (NE Sudan): a glimpse of the tectonic evolution of the NE margin of W. Gondwana during Neoproterozoic time. Precambr Res 123:67–80
Bartley JK, Semikhatov MA, Kaufman AJ, Knoll AH, Pope MC, Jacobsen SB, (2001) Global events across the Mesoproterozoic-Neoproterozoic boundary: C and Sr isotopic evidence from Siberia. Precambr Res 111:165–202
Be’eri-Shlevin Y (2008) The origin and evolution of neoproterzoic magmatism in the northern Arabian-Nubian-Shield (Sinai Peninsula, Egypt, and southern Israel): evidence from the stable and radiogenic isotope record. Thesis (Ph. D.)-Ben-Gurion University of the Negev, Department of Geological and Environmental Sciences, 2008, Beer-Sheva
Bentor YK (1985) The crustal evolution of the Arabo-Nubian massif with special reference to the Sinai peninsula. Precambr Res 28:1–74
Bertrand-Sarfati J, Moussine-Pouchkine A, Amard B, Ait Kaci Ahmed A (1995) First Ediacaran fauna found in Western Africa and evidence for an early Cambrian glaciation. Geology 23:133–136
Beyth M (1972) The geology of central western Tigre, Ethiopia. PhD thesis, Bonn, University of Bonn
Beyth M, Stern RJ, Matthews A (1997) Significance of highgrade metasediments from the Neoproterozoic basement of Eritrea. Precambr Res 86:45–58
Beyth M, Avigad D, Wetzel HU, Matthews A, Berhe SM (2003) Crustal exhumation and indications for snowball Earth in the East African Orogen: North Ethiopia and East Eritrea. Precambr Res 123:187–201
Bibolini A (1920) Risultali preliminary delle osservazioni faite nel Nord-est della Colona Eritrea. Asmara
Bibolini A (1921) Sui conglomerati di Rore Babla e dei Monti Haggar in Colonia Eritrea. Bollettino della Società Geologica Italiana 40:169–176
Bibolini A (1922) Contributions a l’étude de la géologi de l’Afrique orientale Italienne. 13th International Geological Congress (1922, Brussels, Belgium). Title Comptes rendus de la XIIIe session, en Belgique, parts 1–3:797–814
Blasband B, White S, Brooijmans P, de Brooder H, Viser W (2000) Late Proterozoic extensional collapse in Arabian-Nubian Shield. J Geol Soc London 157:615–628
Boger SD, Miller JM (2004) Terminal suturing of Gondwana and the onset of the Ross-Delamerian Orogeny: the cause and effect of an Early Cambrian reconfiguration of plate motions. Earth Planet Sci Lett 219:35–48
Bold U, Smith EF, Rooney AD, Bowring SA, Buchwaldt R, Dudás FÖ, Ramezani J, Crowley JL, Schrag DP, Macdonald FA (2016) Neoproterozoic stratigraphy of the Zavkhan terrane of Mongolia: the backbone for Cryogenian and early Ediacaran chemostratigraphic records. Am J Sci 316:1–63
Bonavia FF, Chorowicz J (1992) Northward expulsion of the Pan-African of northeast Africa guided by a reentrant zone of the Tanzania Craton. Geology 20:1023–1026
Bowring SA, Myrow PM, Landing E, Ramezani J (2003) Geochronological constraints on terminal Neoproterozoic events and the rise of metazoans. Geophys Res Abstr 5(13219):219
Bowring SA, Grotzinger JP, Condon DJ, Ramezani J, Newall MJ, Allen PA (2007) Geochronologic constraints on the chronostratigraphic framework of the Neoproterozoic Huqf Supergroup, Sultanate of Oman. Am J Sci 307:1097–1145
Brasier MD, Shields G, Kuleshov VN, Zhegallo EA (1996) Integrated chemo-and biostratigraphic calibration of early animal evolution: Neoproterozoic-Early Cambrian of southwest Mongolia. Geol Mag 133:445–485
Brasier M, McCarron G, Tucker T, Leather J, Allen P, Shields G (2000) New U–Pb zircon dates for the Neoproterozoic Ghubrah glaciation and for the top of the Huqf Supergroup, Oman. Geology 28:175–178
Burke K, Kraus JU (2000) Deposition of immense Cambro-Ordovician sandstone bodies, now exposed mainly in N. Africa and Arabia, during the aftermath of the final assembly of Gondwana. Geol Soc Am Abstr Program 32:249
Burke K, Sengör C (1986) Tectonic escape in the evolution of continental crust. In: Reflection seismology—the continental crust. Am Geophys Union, Geodynamic series 14:41–53
Burns SJ, Matter A (1993) Carbon isotopic record of the latest Proterozoic from Oman. Eclogae Geol Helv 86:595–607
Bussert R (2010) Exhumed erosional landforms of the Late Palaeozoic glaciation in northern Ethiopia: indicators of ice-flow direction, palaeolandscape and regional ice dynamics. Gondwana Res 18:356–369
Butterfield NJ (2015) The neoproterozoic. Curr Biol 25:R859–R863
Caby R, Fabre J (1981) Late proterozoic to early palaeozoic diamictites, tillites and associated glacigenic sediments in the Série Pourprée of western Hoggar, Algeria. In: Harland WB, Hambrey MJ (eds) Earth’s pre-pleistocene glacial record, pp 140–145. Cambridge University Press
Calvez JY, Kemp J (1982) Geochronological investigations in the Mahd Adh Dhahab Quadrangle, Central Arabian Shield. Deputy Ministry for Mineral Resources: Jiddah, Saudi Arabia, BRGM-TR-02-5, pp 1–41
Canfield DE (2005) The early history of atmospheric oxygen: homage to Robert M. Garrels. Annu Rev Earth Planet Sci 33:1–36
Canfield DE, Poulton SW, Narbonne GM (2007) Late-neoproterozoic deep-ocean oxygenation and the rise of animal life. Science 315:92–95
Canfield DE, Poulton SW, Knoll AH, Narbonne GM, Ross G, Goldberg T, Strauss H (2008) Ferruginous Conditions dominated later neoproterozoic deep-water chemistry. Science 321:949–952
Canfield DE, Knoll AH, Poulton SW, Narbonne GM, Dunning GR (2020) Carbon isotopes in clastic rocks and the Neoproterozoic carbon cycle. Am J Sci 320:97–124
Cawood PA (2005) Terra Australis Orogen: rodinia breakup and development of the Pacific and Iapetus margins of Gondwana during the Neoproterozoic and Paleozoic. Earth Sci Rev 69:249–279
Cecioni G (1981) Precambrian pebbly mudstones in Eritrea, northeastern Ethiopia. In: Hambrey MJ, Harland WB (eds) Earth’s pre-pleistocene glacial record. Cambridge University Press, A24, 150
Cohen KM, Finney SC, Gibbard PL, Fan J-X (2013) updated 2015. The ICS international chronostratigraphic chart. Episodes 36:199–204
Cohen PA, Strauss JV, Rooney AD, Sharma M, Tosca N (2017) Controlled hydroxyapatite biomineralization in an ~810 million-year-old unicellular eukaryote. Sci Adv 3:
Cole JC (1988) Geology of the Aban Al Ahmar Quadrangle, Sheet 25F, Kingdom of Saudi Arabia (explanatory notes). Deputy Ministry for Mineral Resources Map GM-105A, C
Collins AS, Pisarevsky SA (2005) Amalgamating eastern Gondwana: the evolution of the circum-Indian Orogens. Earth-Sci Rev 71:229–270
Collins AS, Windley BF (2002) The tectonic evolution of central and northern Madagascar and its place in the final assembly of Gondwana. J Geol 110:325–339
Condon D, Zhu M, Bowring S, Wang W, Yang A, Jin Y (2005) U-Pb ages from the Neoproterozoic Doushantuo Formation, China. Science 308:95–98
Cosca MA, Shimron A, Caby R (1999) Late Precambrian metamorphism and cooling in the Arabian-Nubian Shield: petrology and 40Ar/39Ar geochronology of metamorphic rocks of the Elat area (southern Israel). Precambr Res 98:107–127
Cox GM, Lewis CJ, Collins AS, Halverson GP, Jourdan F, Foden J, Nettle D, Kattan F (2012) Ediacaran terrane accretion within the Arabian-Nubian Shield. Gondwana Res 21:341–352
Cox GM, Halverson GP, Minarik WG, Le Heron DP, Macdonald FA, Bellefroid EJ, Strauss JV (2013) Neoproterozoic iron formation: an evaluation of its temporal, environmental and tectonic significance. Chem Geol 362:232–249
Cox GM, Halverson GP, Stevenson RK, Vokaty M, Poirier A, Kunzmann M, Li Z-X, Denyszyn SW, Strauss JV, Macdonald FA (2016) Continental flood basalt weathering as a trigger for Neoproterozoic Snowball Earth. Earth Planet Sci Lett 446:89–99
Cox GM, Foden J, Collins AS (2018) Late Neoproterozoic adakitic magmatism of the eastern Arabian Nubian Shield. Geosci Front 10:1981–1992
Cui H, Kaufman AJ, Zou H, Kattan FH, Trusler P, Smith J, Ivantsov A, Rich TH, Al Qubsani A, Yazedi A, Liu X-M, Johnson P, Goderis S, Claeys P, Vickers-Rich P (2020) Primary or secondary? A dichotomy of the strontium isotope anomalies in the Ediacaran carbonates of Saudi Arabia. Precambr Res 343:
Dabbagh ME, Rogers JJW (1983) Depositional environments and tectonic significance of the Wajid Sandstone of southern Saudi Arabia. J Afr Earth Sci 1:47–57
Dalziel IWD (1997) Neoproterozoic-paleozoic geography and tectonics: review, hypothesis, environmental speculation. Geol Soc Am Bull 109:16–42
Davies FB (1985) Explanatory notes to the geologic map of the Al Wajh Quadrangle, Kingdom of Saudi Arabia. Geoscience Map GM-83, scale 1:250,000, sheet 26B. Deputy Ministry for Mineral Resources, Ministry of Petroleum and Mineral Resources, Kingdom of Saudi Arabia, p 27
Davies J, Nairn AEM, Ressetar R (1980) The palaeomagnetism of certain late Precambrian and early Palaeozoic rocks from the Red Sea Hills, eastern desert, Egypt. J Geophys Res 85:3699–3710
De Souza Filho CR, Drury SA (1998) A Neoproterozoic supra-subduction terrane in northern Eritrea, NE Africa. J Geol Soc London 155:551–566
Delfour J (1970) Le Groupe de J’Balah, une nouvelle unite du Bouclier Arabe. Bureau de Recherche Geologique et Minieres Bulletin 4:19–32
Denèle Y, Leroy S, Pelleter E, Pik R, Talbot JY, Kahanbari K (2012) The Cryogenian juvenile Arc formation and successive high-K calc-alkaline plutons intrusion of Socotra Island Yemen. Arab J Geosci 5:903–924
Deynoux M, Affaton P, Trompette R, Villeneuve M (2006) Pan-African tectonic evolution and glacial events registered in Neoproterozoic to Cambrian cratonic and foreland basins of West Africa. J Afr Earth Sc 46:397–426
Dohrmann M, Wörheide G (2019) Dating early animal evolution using phylogenomic data. Nat Sci Reports 7:3599
Donnadieu Y, Goddéris Y, Ramstein G, Nédélec A, Meert J (2004) A ‘snowball Earth’ climate triggered by continental break-up through changes in runoff. Nature 428:303–306
Dor YB, Harlavan Y, Avigad D (2018) Provenance of the great Cambrian sandstone succession of northern Gondwana unraveled by strontium, neodymium and lead isotopes of feldspars and clays. Sedimentology 65:2595–2620
Drury SA, Berhe SM (1993) Accretion tectonics in northern Eritrea revealed by remotely sensed imagery. Geol Mag 130:177–190
El-Shazly AK, Khalil KI (2016) Metamorphic and geochronologic constraints on the tectonic evolution of the Central Eastern Desert of Egypt. Precambr Res 283:144–168
El-Shazly AK, Khalil KI, Helba HA (2019) Geochemistry of banded iron formations and their host rocks from the Central Eastern Desert of Egypt: a working genetic model and tectonic implications. Precambr Res 325:192–216
Ernst RE, Wingate MTD, Buchan KL, Li ZX (2008) Global record of 1600–700 Ma Large Igneous Provinces (LIPs): implications for the reconstruction of the proposed Nuna (Columbia) and Rodinia supercontinents. Precambr Res 160:59–178
Etemad-Saeed N, Hosseini-Barzi M, Adabi M, Miller NR, Sadeghi A, Stockli Houshmandzadeh DF (2016) Evidence for ~560 Ma Ediacaran glaciation in the Kahar Formation, Central Alborz Mountains, northern Iran. Gondwana Res 31:164–183
Evans D (2000) Stratigraphic, geochronological, and paleomagneticconstraints upon the Neoproterozoic climatic paradox. Am J Sci 300:347–433
Evans D, Raub TD (2011) Neoproterozoic glacial palaeolatitudes: a global update. In: Arnaud E, Halverson GP, Shields-Shou G (eds) The geological record of Neoproterozoic glaciations. Geological Society of London, London, pp 93–112
Eyal M, Be’eri-Shlevin Y, Eyal Y, Whitehouse MJ, Litvinovsky B (2014) Three successive proterozoic island arcs in the northern arabian–nubian shield: evidence from SIMS U–Pb dating of zircon. Gondwana Res 25:338–357
Fairchild IJ, Spiro B, Herrington PM (2000) Controls on Sr and C isotope compositions of Neoproterozoic Sr-rich limestones of East Greenland and North China. In: Grotzinger JP, James NP (eds) Carbonate sedimentation and diagenesis in an evolving precambrian world, SEPM Special Publication vol 67, pp 297–313
Fairchild IJ, Spencer T, Ali D, Anderson R, Anderton R, Boomer I, Dove D, Evans J, Hambrey M, Howe J, Sawaki Y, Wang Z, Shields G, Zhou Y, Skelton A, Tucker M (2018) Tonian-Cryogenian boundary sections of Argyll, Scotland. Precambr Res 319:37–64
Feulner G (2012) The faint young Sun problem. Rev Geophys 50:364–370
Fike DA, Grotzinger JP, Pratt LM, Summons RE (2006) Oxidation of the Ediacaran Ocean. Nature 444:744–747
Fitzsimons ICW (2000) Grenville-age basement provinces in east Antarctica: evidence for three separate collisional orogens. Geology 28:879–882
Fowler A, Hassen I, Hassan M (2015) Tectonic evolution and setting of the Sa’al Complex, southern Sinai, Egypt: a Proterozoic continental back-arc rift model. J Afr Earth Sci 104:103–131
Fritz H, Abdelsalam M, Ali KA, Bingen B, Collins AS, Fowler AR, Ghebreab W, Hauzenberger CA, Johnson PR, Kusky TM, Macey P, Muhongo S, Stern RJ, Viola G (2013) Orogen styles in the East African Orogen: a review of the Neoproterozoic to Cambrian tectonic evolution. J Afr Earth Sci 86:65–106
Gad S, Kusky T (2007) ASTER spectral ratioing for lithological mapping in the Arabian-Nubian shield, the Neoproterozoic Wadi Kid area, Sinai, Egypt. Gondwana Res 11:326–335
Garfunkel Z (1999) History and paleogeography during the Pan-African orogen to stable platform transition: reappraisal of the evidence from the Elat area and the northern Arabian-Nubian Shield. Israel J Earth Sci 48:135–157
Garland CR (1980) Geology of the Adigrat area. Ministry of Mines Memoir No. 1, p 51. Addis Ababa 1:250,000 map
Gernon TM, Hincs TK, Tyrrell T, Rohling EJ, Palmer MR (2016) Snowball Earth ocean chemistry driven by extensive ridge volcanism during Rodinia breakup. Nat Geosci 9:242–248
Ghebreab W (1999) Tectono-metamorphic history of Neoproterozoic rocks in eastern Eritrea. Precambr Res 98:83–105
Glennie KW, Boeuf MGA, Hughes-Clarke MW, Moody-Stuart M, Pilaar WFH, Reinhardt BM (1974) Geology of the Oman mountains. Verhandelingen van het Koninklijk Nederlands geologisch mijnbouwkundig Genootschap 31:423
Goddéris Y, Donnadieu Y, Nédélec A, Dupré B, Dessert C, Grard A, Ramstein G, François LM (2003) The Sturtian “snowball” glaciation: fire and ice. Earth Planet Sci Lett 211:1–12
Gong Z, Kodama KP, Li YX (2017) Rock magnetic cyclostratigraphy of the Doushantuo Formation, South China and its implications for the duration of the Shuram carbon isotope excursion. Precambr Res 289:62–74
Gostin VA, McKirdy DM, Webster LJ, Williams GE (2010) Ediacaran ice-rafting and coeval asteroid impact, South Australia: insights into the terminal Proterozoic environment. Aust J Earth Sci 57:859–869
Gray DR, Foster DA, Meert JG, Goscombe BD, Armstrong R, Truow RAJ, Passchier CW (2008) A Damaran perspective on the assembly of southwestern Gondwana. Geol Soc London, Special Publications 294:257–278
Grotzinger JP, Fike DA, Fischer WW (2011) Enigmatic origin of the largest-known carbon isotope excursion in Earth’s history. Nat Geosci 4:285–292
Guilbaud R, Poulton SW, Butterfield NJ, Zhu M, Shields-Zhou GA (2015) A global transition to ferruginous conditions in the early Neoproterozoic oceans. Nat Geosci 8:466–470
Hadley DG (1974) The taphrogeosynclinal Jubaylah Group in the Mashhad area, northwestern Hijaz. Saudi Arabian Directorate General of Mineral Resources Bulletin 10, p 18
Hadley DG (1986) Explanatory notes to the geologic map of the Sahl Al Matran Quadrangle, Kingdom of Saudi Arabia. Geoscience Map GM-86 C, scale 1:250,000, sheet 26C. Deputy Ministry for Mineral Resources, Ministry of Petroleum and Mineral Resources, Kingdom of Saudi Arabia. p 24
Hailu T (1975) Geological map of Adi Arkay. Adis Ababa, Geological Survey of Ethiopia Technical Report, scale 1:250,000
Halverson GP (2006) A Neoproterozoic chronology. In: Xiao S, Kaufman AJ (eds) Neoproterozoic geobiology and paleobiology: dordrecht. Springer, Netherlands, pp 231–271
Halverson GP, Hoffman PF, Schrage DP, Maloof AC, Rice AHN (2005) Toward a Neoproterozoic composite carbon-isotope record. Geol Soc Am Bull 117:1181–1207
Halverson GP, Dudás FÖ, Maloof AC, Bowring SA (2007a) Evolution of the 87Sr/86Sr composition of Neoproterozoic seawater. Palaeogeogr Palaeoclimatol Palaeoecol 256:103–129
Halverson GP, Maloof AC, Schrag DP, Dudás FÖ, Hurtgen M (2007b) Stratigraphy and geochemistry of a ca 800 Ma negative carbon isotope interval in northeastern Svalbard. Chem Geol 237:5–27
Halverson GP, Cox GM, Théou-Hubert L, Schmitz M, Hagadorn JW, Johnson P, Sansjofre P, Kunzmann M, Schumann D (2013) A multi-proxy geochemical record from a late Neoproterozoic volcano-sedimentary basin, eastern Arabian Shield. McGill University, Canada, unpublished poster
Halverson GP, Porter SM, Gibson TM (2018) Dating the late Proterozoic stratigraphic record. Emerg Top Life Sci 2:137–147
Hargrove US (2006a) Crustal evolution of the Neoproterozoic Bi’r Umq suture zone, Kingdom of Saudi Arabia. Geochronological, Isotopic, and Geochemical Constraints. Ph.D. Thesis, University of Texas, Dallas, TX, USA
Hargrove US, Stern RJ, Kimura J-I, Manton WI, Johnson PR (2006) How juvenile if the Arabian-Nubian Shield? Evidence from Nd isotopes and pre-Neoproterozoic inherited zircon in the Bi’r Umq suture zone, Saudi Arabia. Earth Planet Sci Lett 252:308–326
Harland WB (1964) Evidence of late Precambrian glaciation and its significance. In: Nairn AEM (ed) Problems in palaeoclimatology. Interscience, London, pp 119–149
Hassanlouei BT, Rajabzadeh MA (2019) Iron ore deposits associated with Hormuz evaporitic series in Hormuz and Pohl salt diapirs, Hormuzgan province, southern Iran. J Asian Earth Sci 172:30–55
Hebert CL, Kaufman AJ, Penniston-Dorland SC, Martin AJ (2010) Radiometric and stratigraphic constraints on terminal Ediacaran (post-Gaskiers) glaciation and metazoan evolution. Precambr Res 182:402–412
Hedge CE (1984) Precambrian geochronology of part of northwestern Saudi Arabia, Kingdom of Saudi Arabia. US Geological Survey Open File Report 83–381, p 12
Helmy HM, Morad AE, Abdel Rahman HB (2021) Um Zariq formation, southeast sinai, Egypt: a new record of the Sturtian Snowball Earth event in the Arabian Nubian Shield. J Afr Earth Sc 173:
Hill AC, Arouri K, Gorjan P, Walter MR (2000) Geochemistry of marine and nonmarine environments of a Neoproterozoic cratonic carbonate/evaporite: the Bitter Springs Formation, Central Australia. In: Grotzinger JP, James NP (eds) Carbonate sedimentation and diagenesis in the evolving precambrian world. SEPM, 327–344 (Spec. Pub. 67)
Hoffman PF (1999) The break-up of Rodinia, birth of Gondwana, true polar wander and the snowball earth. J Afr Earth Sci 29:17–33
Hoffman PF (2013) The great oxidation and a Siderian snowball Earth: MIF-S based correlation of Paleoproterozoic glacial epochs. Chem Geol 362:143–156
Hoffman PF, Schrag DP (2002) The snowball Earth hypothesis: testing the limits of global change. Terra Nova 14:129–155
Hoffman PF, Kaufman AJ, Halverson GP, Schrag DP (1998) A Neoproterozoic snowball earth. Science 281:1342–1346
Hoffman PF, Halverson GP, Domack EW, Husson JM, Higgins JA, Schrag DP (2007) Are basal Ediacaran (635 Ma) post-glacial “cap dolostones” diachronous? Earth Planet. Sci Lett 258:114–131
Hoffman PF, Abbot DS, Ashkenazy Y, Benn DI, Brocks JJ, Cohen PA, Cox GM, Creveling JR, Donnadieu Y, Erwin DH, Fairchild IJ, Ferreira D, Goodman JC, Halverson GP, Jansen MF, Le Hir G, Love GD, Macdonald FA, Maloof AC, Partin CA, Ramstein G, Rose BEJ, Sadler PM, Tziperman E, Voigt A, Warren SG (2017) Snowball earth climate dynamics and cryogenian geology-geobiology. Sci Adv 3:e1600983
Horton F (2015) Did phosphorus derived from the weathering of large igneous provinces fertilize the Neoproterozoic ocean? Geochem Geophys Geosystems 1:1723–1738
Husson JM, Maloof AC, Schoene B, Chen CY, Higgins JA (2015) Stratigraphic expression of Earth’s deepest δ13C excursion in the Wonoka Formation of South Australia. Am J Sci 315:1–45
Hyde WT, Crowley TJ, Baum SK, Peltier WR (2000) Neoproterozoic ‘Snowball Earth’ simulations with a coupled climate/icesheet model. Nature 405:425–429
Jacobs J, Thomas RJ (2004) Himalayan-type indenter-escape tectonics model for the southern part of the late Neoproterozoic-early Paleozoic East African-Antarctic orogen. Geology 32:721–724
Jacobs J, Bauer W, Fanning CM (2003) Late Neoproterozoic/Early Palaeozoic events in central Dronning Maud Land and significance for the southern extension of the East African Orogen into East Antarctica. Precambr Res 126:27–53
Jarrar GH, Wachendorf H, Zellmer D (1991) The Saramuj Conglomerate: evolution of a Pan-African molasse sequence from southwest Jordan. N Jb Geol Palaontol Mh 6:335–356
Jarrar GH, Wachendorf H, Zachmann D (1993) A Pan-African alkaline pluton intruding the Saramuj Conglomerate, southwest Jordan. Geol Rundschau 82:121–135
Javoy M, Pineau F, Delorme H (1986) Carbon and nitrogen isotopes in the mantle. Chem Geol 57:41–62
Johnson PR (1995) Proterozoic geology of Western Saudi Arabia—North-Central Sheet: explanatory notes on precambrian stratigraphic relations. Saudi Arabian Deputy Ministry for Mineral Resources, Jiddah, Saudi Arabia, USGS-OF-95-5, pp 1–44
Johnson PR (2003) Post-amalgamation basins of the NE Arabian shield and implications for Neoproterozoic III tectonism in the northern East African Orogen. Precambr Res 123:321–337
Johnson PR (2014) An expanding Arabian-Nubian Shield geochronologic and isotopic dataset: defining limits and confirming the tectonic setting of a Neoproterozoic accretionary orogen. Open Geol J 8:3–33
Johnson P, Kattan F (2008) Lithostratigraphic revision in the Arabian Shield: the impacts of geochronology and tectonic analysis. Arab J Sci Eng 33:3–16
Johnson PR, Kattan FH (2012) The geology of the Saudi Arabian Shield. Saudi Geological Survey, Jiddah, Saudi Arabia, pp 1–479
Johnson PR, Stewart ICF (1995) Magnetically inferred basement structure in central Saudi Arabia. Tectonophysics 245:37–52
Johnson PR, Woldehaimanot B (2003) Development of the Arabian-Nubian Shield: perspectives on accretion and deformation in the northern East African Orogen and the assembly of Gondwana. In: Yoshida M, Windley BF, Dasgupta S (eds) Proterozoic East Gondwana: supercontinent assembly and breakup, Geological Society, London, Spec. Pub. 206, pp 289–325
Johnson PR, Abdelsalam MG, Stern RJ (2003) The Bi’r Umq-Nakasib Suture Zone in the Arabian-Nubian Shield: a key to understanding crustal growth in the East African Orogen. Gondwana Res 6:523–530
Johnson PR, Andresen A, Collins AS, Fowler AR, Fritz H, Ghebreab W, Kusky T, Stern RJ (2011) Late cryogenian-ediacaran history of the Arabian-Nubian Shield: a review of depositional, plutonic, structural, and tectonic events in the closing stages of the northern East African Orogen. J Afr Earth Sci 61:167–232
Johnson PR, Halverson GP, Kusky TM, Stern RJ, Pease V (2013) Volcanosedimentary Basins in the Arabian-Nubian Shield: markers of repeated exhumation and denudation in a neoproterozoic accretionary orogen. Geosciences 3:389–445
Jones DS, Maloof AC, Hurtgen MT, Rainbird RH, Schrag DP (2010) Regional and global chemostratigraphic correlation of the early Neoproterozoic Shaler Supergroup, Victoria Island, Northwestern Canada. Precambr Res 181:43–63
Kaufman AJ, Jacobsen SB, Knoll AH (1993) TheVendian record of Sr and C isotopic variations in seawater: implications for tectonics and paleoclimate. Earth Planet Sci Lett 84:27–41
Kaufman AJ, Knoll AH, Narbonne GM (1997) Isotopes, ice ages, and terminal Proterozoic earth history. Proc Natl Acad Sci USA 94:6600–6605
Keller CB, Husson JM, Mitchell RN, Bottke WF, Gernon TM, Boehnke P, Bell EA, Swanson-Hysell NL, Peters SE (2020) Neoproterozoic glacial origin of the Great Unconformity. Proc Nat Academy Sci 116:1136–1145
Kemp J (1981) Geologic map of the Wadi Al Ays Quadrangle, Sheet 25C, Kingdom of Saudi Arabia, Saudi Arabian Deputy Ministry for Mineral Resources: Jiddah, Saudi Arabia, GM 53, pp 1–39
Kemp J, Gros Y, Prian JP (1982) Geologic Map of the Mahd adh Dhahab Quadrangle, Sheet 23E, Kingdom of Saudi Arabia, Saudi Arabian Deputy Ministry for Mineral Resources: Jiddah, Saudi Arabia, GM 64, pp 1–39
Kempf O, Kellerhals P, Lowrie W, Matter A (2000) Palaeomagnetic directions in late Precambrian glaciomarine sediments of the Mirbat Sandstone Formation, Oman. Earth Planet Sci Lett 175:181–190
Kennedy A, Johnson PR, Kattan FH (2004) SHRIMP geochronology in the Northern Arabian Shield Part I: data acquisition; Saudi geological survey: Jiddah, Saudi Arabia, SGS-OF-2004-11, pp 1–28
Kennedy A, Johnson PR, Kattan FH (2005) SHRIMP geochronology in the Northern Arabian Shield Part II: data acquisition 2004, Saudi Geological Survey: Jiddah, Saudi Arabia, SGS-OF-2005–10, pp 1–44
Kennedy A, Kozdroj W, Kattan FH, Ziolkowska-Kozdroj M, Johnson PR (2010a) SHRIMP Geochronology in the Arabian Shield (Midyan Terrane, Afif Terrane, Ad Dawadi Terrane) and Nubian Shield (Central Eastern Desert Terrane) Part IV: data acquisition 2008; Saudi Geological Survey: Jiddah, Saudi Arabia; SGS-OF-2010-10, pp 1–101
Kennedy A, Kozdroj W, Kadi K, Ziolkowska-Kozdroj M, Johnson PR (2010b) SHRIMP geochronology of the Arabian Shield (Midyan Terrane, Afif Terrane) and Nubian Shield (Central Eastern Desert Terrane), Part V: data acquisition 2009; Saudi Geological Survey, Jiddah, Saudi Arabia, SGS-OF-2010-11, p 80
Kidane T, Bachtadse V, Alene M (2014) Quaternary remagnetization of the Neoproterozoic limestone of Negash Synclinorium (Arabian–Nubian Shield, northern Ethiopia): With implications of no paleomagnetic testing for the proposed Snowball Earth events. Phys Earth Planet Inter 235:1–12
Kilner B, Conall MN, Brasier M (2005) Low-latitude glaciation in the Neoproterozoic of Oman. Geology 33:413–416
Kirschvink JL (1992) Late Proterozoic low-latitude global glaciation: the snowball Earth. In: Schopf JW, Klein C (eds) The Proterozoic biosphere—a multidisciplinary study. Cambridge University Press, Cambridge, pp 51–52
Kiyokawa S, Suzuki T, El-Dokouny HA, Dawoud M, Abuelhasan AA (2020) Stratigraphy, petrology, and geochemistry of a Neoproterozoic banded iron sequence in the El-Dabbah Group, central Eastern Desert, Egypt. J Afr Earth Sc 168:
Klaebe RM, Smith MP, Fairchild IJ, Fleming EJ, Kennedy MJ (2018) Facies-dependent d13C variation and diagenetic overprinting at the onset of the Sturtian glaciation in north-east Greenland. Precambr Res 319:96–113
Knoll AH, Walter MR, Narbonne GM, Christie-Blick N (2004) The Ediacaran Period: a new addition to the geologic time scale. Lethaia 39:13–30
Knoll AH, Walter MR, Narbonne GM, Christie-Blick N (2006) A new period the geologic time scale. Science 205:621–622
Kröner A (2001) The mozambique belt of East Africa and madagascar: significance of zircon and Nd model ages for Rodinia and Gondwana supercontinent formation and dispersal. S Afr J Geol 104:151–166
Kröner A, Muhongo S, Hegner E, Wingate MTD (2003) Single zircon geochronology and Nd isotopic systematics of Proterozoic highgrade rocks from the Mozambique belt of southern Tanzania (Masasi area): implications for Gondwana assembly. J Geol Soc London 160:645–757
Kusky TM, Matsah MI (2003) Neoproterozoic dextral faulting on the Najd fault system, Saudi Arabia, preceded sinistral faulting and escape tectonics related to closure of the Mozambique Ocean. Geol Soc Spec Publ 206:327–361
Küster D, Liégeois J-P, Matukov D, Sergeev S, Lucassen F (2008) Zircon geochronology and Sr, Nd, Pb isotope geochemistry of granitoids from Bayuda Desert and Sabaloka (Sudan): evidence for a Bayudian event (920–900 Ma) preceding the Pan-African orogenic cycle (860–590 Ma) at the eastern boundary of the Saharan Metacraton. Precambr Res 164:16–39
Kuznetsov AB, Semikhatov MA, Maslov AV, Gorokhov IM, Prasolov EM, Krupenin MT, Kislova IV (2006) New data on Sr-and C-isotopic chemostratigraphy of the Upper Riphean type section (Southern Urals). Stratigr Geol Correl 14:602–628
Le Guerroué E (2010) Duration and synchroneity of the largest negative carbon isotope excursion on Earth: the Shuram/Wonoka anomaly. CR Geosci 342:204–214
Letalenet J (1979) Explanatory notes to the geologic map of the ‘Afif Quadrangle, Kingdom of Saudi Arabia. Geoscience Map GM-47C, scale 1:250,000, sheet 23F. Deputy Ministry for Mineral Resources, Ministry of Petroleum and Mineral Resources, Kingdom of Saudi Arabia, p 20
Li ZX, Bogdanova SV, Collins AS, Davidson A et al (2008) Assembly configuration and break-up history of Rodinia: a synthesis. Precambr Res 160:179–210
Li Z-X, Evans DAD, Halverson GP (2013) Neoproterozoic glaciations in a revised global palaeogeography from the breakup of Rodinia to the assembly of Gondwanaland. Sed Geol 294:219–232
Li X-H, Abd El-Rahman Y, Abu Anbar M, Li J, Ling X-X, Wu L-G, Masoud AE (2018) Old continental crust underlying juvenile oceanic arc: evidence from northern Arabian-Nubian Shield, Egypt. Geophys Res Lett 45:3001–3008
Linneman U, Pidal AP, Hofmann M, Drost K, Quesada C, Gerdes A, Marko L, Gärtner A, Zieger J, Ulrich J, Krause R, Vickers-Rich P, Horak J (2018) A ~565 Ma old glaciation in the Ediacaran of peri-Gondwanan West Africa. Int J Earth Sci https://doi.org/10.1007/s00531-017-1520-7
Liu Y, Peltier WR (2013) Sea level variations during snowball Earth formation: 1. A preliminary analysis. J Geophys Res 118:4410–4434
Love GD, Grosjean E, Stalvies C, Fike DA, Grotzinger JP, Bradley AS, Kelly AE, Bhatia M, Bowring SA, Condon DJ, Summons RE (2009) Fossil steroids record the appearance of demospongiae during the cryogenian. Nature 457:718–722
Macdonald FA, Schmitz MD, Crowley JL, Roots CF, Jones DS, Maloof AC, Strauss JV, Cohen PA, Johnston DT, Schrag DP (2010a) Calibrating the cryogenian. Science 327:1241–1243
Macdonald FA, Strauss JV, Rose CV, Dudas F, Schrag DP (2010b) Stratigraphy of the port Nolloth Group of Namibia and South Africa and implications for the age of neoproterozoic iron formations. Am J Sci 310:862–888
MacLennan SA, Park Y, Swanson-Hysell NL, Maloof AC, Schoene B, Gebreslassie M, Antilla E, Tesema T, Alene M, Haileab B (2018) The arc of the Snowball: U–Pb dates constrain the Islay anomaly and the initiation of the Sturtian glaciation. Geology 46:539–542
Maloof AC, Schrag DP, Crowley JL, Bowring SA (2005) An expanded record of early Cambrian carbon cycling from the Anti-Atlas Margin, Morocco. Can J Earth Sci 42:2195–2216
Maloof AC, Halverson GP, Kirschvink JL, Schrag DP, Weiss BP, Hoffman PF (2006) Combined paleomagnetic, isotopic, and stratigraphic evidence for true polar wander from the Neoproterozoic Akademikerbreen Group, Svalbard, Norway. GSA Bulletin 118:1024–1099
Master S, Wendorff M (2011) Neoproterozoic glaciogenic diamictites of the Katanga Supergroup, Central Africa. In: Arnaud E et al (eds) The geological record of neoproterozoic glaciations. Geol Soc London Memoir 36:173–183
McCaffrey MA, Moldowan JM, Lipton PA, Summons RE, Peters KE, Jeganathan A, Watt DS (1994) Paleoenvironmental implications of novel C30 steranes in Precambrian to Cenozoic age petroleum and bitumen. Geochimica et Cosmochimica Acta 58:529–532
Meert J (2003) A synopsis of events related to the assembly of eastern Gondwana. Tectonophysics 362:1–40
Meert JG, Lieberman BS (2008) The Neoproterozoic assembly of Gondwana and its relationship to the Ediacaran-Cambrian radiation. Gondwana Res 14:5–21
Meert JG, Van Der Voo R (1997) The assembly of Gondwana 800–550 Ma. J Geodyn 23:223–235
Miller NR, Alene M, Sacchi R, Stern R, Conti A, Kröner A, Zuppi G (2003) Significance of the Tambien Group (Tigre, N. Ethiopia) for snowball Earth events in the Arabian-Nubian Shield. Precambr Res 121:263–283
Miller N, Schilman B, Avigad D, Stern RJ, Beyth M (2006) Neoproterozoic Snowball Earth—the northern Ethiopia record. Abstract presented in the “Snowball Earth 2006” conference, Monte Verita, Switzerland, pp 74–75
Miller N, Johnson P, Stern R (2008) Marine versus non-marine environments for the Jibalah Group, NW Arabian Shield: a sedimentological and geochemical survey and report of possible Metazoa in the Dhaiqa Formation. Arab J Sci Eng 22:55–77
Miller NR, Stern RJ, Avigad D, Beyth M, Schilman B (2009) Neoproterozoic carbonate-slate sequences of the Tambien Group, N. Ethiopia (I): pre-‘Sturtian’ chemostratigraphy and regional correlation. Precambr Res 170:129–156
Miller NR, Avigad D, Stern RJ, Beyth M (2011) The Tambien Group, northern Ethiopia (Tigre). In: Arnaud E et al (eds) The geological record of Neoproterozoic glaciations. Geol Soc London Memoir 36:263–276
Moghazi A-KM, Ali KA, Wilde SA, Zhou Q, Andersen T, Andresen A, El-Enen MMA, Stern RJ (2012) Geochemistry, geochronology, and Sr–Nd isotopes of the Late Neoproterozoic Wadi Kid volcano-sedimentary rocks, Southern Sinai, Egypt: implications for tectonic setting and crustal evolution. Lithos 154:147–165
Morag N, Avigad D, Gerdes A, Belousova E, Harlavan Y (2011a) Crustal evolution and recycling in the northern Arabian-Nubian Shield: new perspectives from zircon Lu–Hf and U–Pb systematics. Precambr Res 186:101–116
Morag N, Avigad D, Gerdes A, Belousova E, Harlavan Y (2011b) Detrital zircon Hf isotopic composition indicates long-distance transport of North Gondwana Cambrian-Ordovician sandstones. Geology 39:955–958
Nairn AEM, Perry TA, Ressetar R, Rogers S (1987) A palaeomagnetic study of the Dokhan volcanic formation and younger granites, eastern desert of Egypt. J Afr Earth Sc 6:353–365
Nettle D (2009) A sequence stratigraphic, geochronological and chemostratigraphic investigation of the Ediacaran Antaq Basin, Eastern Arabian Shield, Saudi Arabia. Unpublished Honours Thesis, Geology and Geophysics, University of Adelaide, Australia; Saudi Geological Survey Technical Report SGSTR-2010-5, p 83
Nettle D, Halverson GP, Cox GM, Collins AS, Schmitz M, Gehling J, Johnson PR, Kadi K (2013) A middle-late Ediacaran volcano-sedimentary record from the Eastern Arabian-Nubian Shield. Terra Nova 26:120–129
Newman MJ, Rood RT (1977) Implications of solar evolution for the Earth’s early atmosphere. Science 198:1035–1037
Nicholson PG, Janjou DLA, Fanning CM, Heaman LM, Grotzinger JP (2008) Deposition, age, and Pan-Arabian correlation of late Neoproterozoic outcrops in Saudi Arabia (abstract), 8th Middle East Geoscience Conference and exhibition, GEO 2008, Manama, Bahrain AAPG Search and Discovery Magazine, article 90077
Och LM, Shields-Zhou GA (2012) The Neoproterozoic oxygenation event: environmental perturbations and biogeochemical cycling. Earth Sci Rev 110:26–57
Pallister JS, Stacey JS, Fischer LB, Premo WR (1988) Precambrian ophiolites of Arabia: geologic settings, U–Pb geochronology, Pb-isotope characteristics, and implications for continental accretion. Precambr Res 38:1–54
Park U, Swanson-Hysell NL, MacLennan SA, Maloof AC, Gebreslassie M, Tremblay MM, Schoene B, Alene M, Anttila ESC, Tesema T, Haileab B (2019) The lead-up to the Sturtian Snowball Earth: neoprotoerozoic chemostratigraphy time-calibrated by the Tambien Group of Ethiopia. GSA Bulletin 132:1119–1149
Patchett PJ, Chase CG (2002) Role of transform continental margins in major crustal growth episodes. Geology 30:39–42
Pellaton C (1979) Geologic map of the Yanbu’al Bahr Quadrangle, Sheet 24C, Kingdom of Saudi Arabia. Saudi Arabian Directorate General of Mineral Resources, Jiddah, Saudi Arabia
Pisarevsky SA, Murphy JB, Cawood PA, Collins AS (2008) Late Neoproterozoic and early Cambrian palaeogeography: models and problems. Geol Soc, London 294:9–31 Special Publications
Pisarevsky SA, McCausland PJ, Hodych JP, O’Brien SJ, Tait JA, Murphy JB, Colpron M (2011) Paleomagnetic study of the late Neoproterozoic Bull Arm and Crown Hill formations (Musgravetown Group) of eastern Newfoundland: Implications for Avalonia and West Gondwana paleogeography. Can J Earth Sci 49:308–327
Planavsky NJ, Reinhard CT, Wang X, Thomson D, McGoldrick P, Rainbird RH, Johnson T, Fischer WW, Lyons TW (2014) Low mid-Proterozoic atmospheric oxygen levels and the delayed rise of animals. Science 346:635–638
Pollard D, Kasting JF (2005) Snowball Earth: a thin-ice solution with flowing sea glaciers. J Geophys Res 110:C07010
Poulton SW, Canfield DE (2011) Ferruginous conditions: a dominant feature of the ocean through Earth’s history. Elements 7:107–112
Powell JH, Abed A, Jarrar GH (2015) Ediacaran araba complex of jordan. GeoArabia 20:99–156
Pu JP, Bowring SA, Ramezani J, Myrow P, Raub TD, Landing E, Mills A, Hodgin E, Macdonald FA (2016) Dodging snowballs: geochronology of the Gaskiers glaciation and the first appearance of the Ediacaran biota. Geology 44:955–958
Ramsay CR (1986) Geologic Map of the Rabigh Quadrangle, Sheet 22D, Kingdom of Saudi Arabia. Saudi Arabian Deputy Ministry for Mineral Resources: Jiddah, Saudi Arabia, GM 84:1–49
Rieu R, Allen PA, Cozzi A, Kosler J, Bussy F (2007) A composite stratigraphy for the Neoproterozoic Huqf Supergroup of Oman: integrating new litho-, chemo- and chronolstratigraphic data of the Mirbat area, southern Oman. J Geol Soc, London 164:997–1009
Rooney AD, Chew DM, Selbey D (2011) Re–Os geochronology of the Neoproterozoic-Cambrian Dalradian Supergroup of Scotland and Ireland: Implications for Neoproterozoic stratigraphy, glaciations and Re–Os systematics. Precambr Res 185:202–214
Rooney AD, Macdonald FA, Strauss JV, Dudás FÖ, Hallmann C, Selby D (2014) Re-Os geochronology and coupled Os-Sr isotope constraints on the Sturtian snowball Earth. Proc Natl Acad Sci 111:51–56
Rooney AD, Strauss JV, Brandon AD, Macdonald FA (2015) A Cryogenian chronology: two long-lasting, synchronous Neoproterozoic snowball Earth glaciations. Geology 43:459–462
Rooney AD, Cantine MD, Bergmann KD, Gómez-Pérez I, Al Baloushi B, Boag TH, Busch JF, Sperling EA, Strauss JV (2020) Calibrating the coevolution of Ediacaran life and environment. Proc Nat Acad Sci 117:16824–16830
Rothman DH, Hayes JM, Summons RE (2003) Dynamics of the Neoproterozoic carbon cycle. Proc Natl Acad Sci 100:8124–8129
Runnegar B (2000) Loophole for snowball earth. Nature 405:403–404
Sahoo SK, Planavsky NJ, Kendall B, Wang X, Shi X, Scott C, Anbar AD, Lyons TW, Jiang G (2012) Ocean oxygenation in the wake of the Marinoan glaciation. Nature 489:546–549
Sandler A, Teutsch N, Avigad D (2012) Sub-Cambrian pedogenesis recorded in weathering profiles of the Arabian-Nubian Shield. Sedimentology 59:1305–1320
Sawaki Y, Kawai T, Shibuya T, Tahata M, Omori S, Tsuyoshi K, Yoshida N, Hirata T, Ohno T, Windley BF, Shigenori M (2010) 87Sr/86Sr chemostratigraphy of Neoproterozoic Dalradian carbonates below the Port Askaig Glaciogenic Formation, Scotland. Precambr Res 179:150–164
Schrag DP, Higgins JA, Macdonald FA, Johnston DT (2013) Authigenic carbonate and the history of the global carbon cycle. Science 339:540–543
Shang CK, Morteani G, Satir M, Taubald H (2010) Neoproterozoic continental growth prior to Gondwana assembly: constraints from zircon-titanite geochronology, geochemistry and petrography of ring complex granitoids, Sudan. Lithos 118:61–81
Shields GA, Mills BJW, Zhu M, Raub RD, Daines SJ, Lenton TM (2019) Unique Neoproterozoic carbon isotope excursions sustained by coupled evaporite dissolution and pyrite burial. Nat Geosci 12:823–827
Shields-Zhou GA, Denoux M, Och L (2011) The record of Neoproterozoic glaciation in the Taoudéni Basin, NW Africa. In: Arnaud E et al (eds) The geological record of Neoproterozoic glaciations. Geol Soc London Memoir 36:163–171
Shields-Zhou GA, Porter S, Halverson GP (2016) A new rock-based definition for the Cryogenian Period (circa 720–635 Ma). Episodes 39:3–8
Sifeta K, Roser BP, Kimura JI (2005) Geochemistry, provenance, and tectonic setting of Neoproterozoic metavolcanic and metasedimentary units, Werri area, Northern Ethiopia. J Afr Earth Sc 41:212–223
Spence GH, Le Heron DP, Fairchild IJ (2016) Sedimentological perspectives on climatic, atmospheric and environmental change in the Neoproterozoic Era. Sedimentology 63:253–306
Squire RJ, Campbell IH, Allen CM, Wilson CJ (2006) Did the Transgondwanan Supermountain trigger the explosive radiation of animals on Earth? Earth Planet. Sci Lett 250:116–133
Stein M (2003) Tracing the plume material in the Arabian-Nubian Shield. Precambr Res 123:223–234
Stern RJ (1985) The najd fault system, Saudi Arabia and Egypt: a late Precambrian rift-related transform system? Tectonics 4:497–511
Stern RJ (1994) Arc-assembly and continental collision in the Neoproterozoic African Orogen: implications for the consolidation of Gondwanaland. Annu Rev Earth Planet Sci 22:319–351
Stern RJ (2002) Crustal evolution in the East African Orogen: a neodymium isotopic perspective. J Afr Earth Sci 34:109–117
Stern RJ (2018) The evolution of plate tectonics. Philosophical Transactions A, 376, 20170406. https://doi.org/10.1098/rsta.2017.0406
Stern RJ, Abdelsalam MG (1998) Formation of juvenile continental crust in the Arabian-Nubian Shield: evidence from granitic rocks of the Nakasib suture. NE Sudan Geol Rundschau 87:150–160
Stern RJ, Johnson P (2010) Continental lithosphere of the Arabian Plate: a geologic, petrologic, and geophysical synthesis. Earth Sci Rev 101:29–67
Stern RJ, Miller NR (2018) Did the transition to plate tectonics cause Neoproterozoic snowball Earth? Terra Nova 30:87–94
Stern RJ, Miller NR (2019) Neoproterozoic glaciation—snowball earth hypothesis. Encyclopedia of geology, 2nd ed. https://doi.org/10.1016/B978-0-12-409548-9.12107-4
Stern RJ, Avigad D, Miller NR, Beyth M (2006) Geological society of Africa presidential review: evidence for the snowball earth hypothesis in the Arabian-Nubian Shield and the East African Orogen. J Afr Earth Sc 44:1–20
Stern RJ, Johnson PR, Ali KA, Mukherjee S (2011) Evidence for early and mid-cryogenian glaciation in the northern Arabian-Nubian Shield (Egypt, Sudan, and western Arabia). In: The geological record of neoproterozoic glaciation. In: Arnaud E, Halverson GP, Shield-Zhou G (eds) Geol Soc London, UK, 2011; Memoirs 36, 277–284
Stewart SA (2016) Structural geology of the Rub’ Al-Khali Basin, Saudi Arabia. Tectonics 35:2417–2438
Stoeser DB, Stacey JS (1988) Evolution, U–Pb geochronology, and isotope geology of the Pan-African Nabitah orogenic belt of the Saudi Arabian Shield. In: El-Gaby S, Greiling RO (eds) The Pan-African Belt of NE Africa and adjacent areas, Friedr. Vieweg & Sohn, Braunschweig, pp 227–289
Sultan M, Arvidson RE, Duncan I, Stern RJ, El Kaliouby M (1988) Extension of the Najd Shear System from Saudi Arabia to the Central Eastern Desert of Egypt based on Integrated Field and Landsat Observations. Tectonics 7:1291–1306
Swanson-Hysell NL, Rose CV, Calmet CC, Halverson GP, Hurtgen MT, Maloof AC (2010) Cryogenian glaciation and the onset of carbon-isotope decoupling. Science 328:608–611
Swanson-Hysell NL, Maloof AC, Condon DJ, Jenkin GR, Alene M, Tremblay MM, Tesema T, Rooney AD, Haileab B (2015) Stratigraphy and geochronology of the Tambien Group, Ethiopia: evidence for globally synchronous carbon isotope change in the Neoproterozoic. Geology 43:323–326
Tadesse T (1997) The geology of axum area (ND 37-6). Ethiopian Institute of Geological Surveys, Addis Ababa (Memoir No. 9)
Tadesse T (1999) Axum sheet geological map. Geological Survey of Ethiopia, Addis Ababa, Ethiopia. 1:250,000 map
Tadesse T, Hoshino M, Suzuki K, Iizumi S (2000) Nd, Rb–Sr and Th–U–Pb zircon ages of syn- and post-tectonic granitoids from the Axum area of northern Ethiopia. J Afr Earth Sci 30:313–327
Tait J, Delpomdor F, Préat A, Tack A, Straathof G, Nkula VK (2011) Neoproterozoic sequences of the West Congo and Lindi/Ubangi Supergroups in the Congo Craton, Central Africa. In: Arnaud E et al (eds) The geological record of Neoproterozoic glaciations. Geol Soc London Memoir 36:185–193
Teklay M, Kröner A, Mezger K (2001) Geochemistry, geochronology and isotope geology of Nakfa intrusive rocks, northern Eritrea: products of a tectonically thickened Neoproterozoic arc crust. J Afr Earth Sci 33:283–301
Tostevin R, Clarkson MO, Gangl S, Shields GA, Wood RA, Bowyer F, Penny AM, Stirling CH (2019) Uranium isotope evidence for an expansion of anoxia in terminal Ediacaran oceans. Earth Planet Sci Lett 506:104–112
Trindade RIF, Macouin M (2007) Palaeolatitude of glacial deposits and palaeogeography of Neoproterozoic ice ages. CR Geosci 339:200–211
Tschopp RH (1967) The general geology of Oman. In: Proceedings of the 7th world petroleum congress 2, pp 231–242
Tsige L, Abdelsalam MG (2005) Neoproterozoic-early Paleozoic gravitational tectonic collapse in the southern part of the Arabian-Nubian Shield: the Bulbul Belt of southern Ethiopia. Precambr Res 38:31–297
Tziperman E, Halevy I, Johnston DT, Knoll AH, Schrag DP (2011) Biologically induced initiation of Neoproterozoic snowball-Earth events. Proc Natl Acad Sci USA 108:15091–15096
Vail JR (1983) Pan-African crustal accretion in northeast Africa. J Afr Earth Sci 1:285–294
Veevers JJ (2003) Pan-African is Pan-Gondwanaland: oblique convergence drives rotation during 650–500 Ma assembly. Geology 31:501–504
Vernhet R, Youbi N, Chellai EH, Villeneuve M El, Archi A (2012) The Bou-Azzer glaciation: evidence for an Ediacaran glaciation on the West African Craton (Anti-Atlas, Morocco). Precambr Res 196–197:106–112
Verri P (1909) Contributo allo studio geografio Della Colonia Eritrea. Bollettino della Societa’ Geografica Italiana, 10, pp 251–320. Carta Geologica 1:1,500,000
Vickers-Rich P, Kozdroj W, Kattan FH, Leonov M, Ivantsov A, Johnson PR, Linnemann U, Hofmann M, Al Garni SM, Al Qubsani A, Shamari A, Al Baraki A, Al Kaff MH, Ziolkowska-Kozdroj M, Rich TH, Trusler P, Rich B (2010) Reconnaissance for an Ediacaran fauna, Kingdom of Saudi Arabia. Saudi Geological Survey, Technical Report, SGS-TR-2010-8, p 42, 74 figs., 1 table, 1 pl
Vickers-Rich P, Ivantsov A, Kattan FH, Johnson PR, Al Qubsani A, Kashghari W, Leonov M, Rich R, Linnemann U, Hofmann M, Trusler P, Smith J, Yazidi A, Rich B, Al Garni SM, Shamari A, Al Barakati A, Al Kaff MH (2013) In search of the Kingdom’s Ediacarans: the first genuine Metazoans (macroscopic body and trace fossils) from the Neoproterozoic Jibalah Group (Vendian/Ediacaran) on the Arabian Shield. Saudi Geological Survey Technical Report SGS-TR-2013-5, p 21., 19 figs., 1 table
Weissbrod T, Sneh A (2002) Sedimentology and paleogeography of the Late Precambrian–Early Cambrian arkosic and conglomeratic facies in the northern margins of the Arabo-Nubian Shield Bulletin. Geol Survey Israel 87:44
Whitehouse MJ, Pease V, Al-Khirbash S (2016) Neoproterozoic crustal growth at the margin of the East Gondwana continent—age and isotopic constraints from the easternmost inliers of Oman. Int Geol Rev 58:2046–2064
Wilde SA, Youssef K (2000) Significance of SHRIMP dating of the imperial porphyry and associated Dokhan volcanics, Gebel Dokhan, northeastern desert, Egypt. J Afr Earth Sci 31:403–413
Wilde SA, Youssef K (2002) A re-evaluation of the origin and setting of the late Precambrian Hammamat Group based on SHRIMP U–Pb dating of detrital zircons from Gebel Umm Tawat, North Eastern Desert, Egypt. J Geol Soc London 159:595–604
Williams GE (2008) Proterozoic (pre-Ediacaran) glaciation and the highobliquity, low-latitude ice, strong seasonality (HOLIST) hypothesis: principles and tests. Earth Sci Rev 87:61–93
Williams GE, Schmidt PW, Young GM (2016) Strongly seasonal Proterozoic glacial climate in low palaeolatitudes: radically different climate system on the pre-Ediacaran Earth. Geosci Front 7:555–571
Wu C, Yang T, Shields GA, Bian X, Bao B, Ye H, Li W (2020) Termination of Cryogenian ironstone deposition by deep ocean euxinia. Geochem Perspect Lett 15:1–5
Yin Z, Zhu M, Davidson EH, Bottjer DJ, Zhao F, Tafforeau P (2015) Sponge grade body fossil with cellular resolution dating 60 Myr before the Cambrian. Proc Nat Acad Sci 141:E1453–E1460
Zhou MT, Luo T, Huff WD, Yang Z, Zhou G, Gan T, Yang H, Zhange D (2018) Timing the termination of the Doushantuo negative carbon isotope excursion: evidence from U–Pb ages from the Dengying and Liuchapo formations, South China. Sci Bull 63:1431–1438
Zhou Y, Pogge von Strandmann PAE, Zhu M, Ling H, Manning C, Li D, He T, Shields GA (2020) Reconstructing Tonian seawater 87Sr/86Sr using calcite microspar. Geology 48:462–467
Zimmer M, Kröner A, Jochum KP, Reischmann R, Todt W (1995) The Gabal Gerf complex: a Precambrian N-MORB ophiolite in the Nubian Shield, NE Africa. Chem Geol 123:29–51
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We thank Peter Johnson and Yasser Abd El-Rahman for thoughtful reviews that improved the manuscript.
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Miller, N.R., Stern, R.J. (2021). Evolution of the Arabian Nubian Shield and Snowball Earth. In: Hamimi, Z., Fowler, AR., Liégeois, JP., Collins, A., Abdelsalam, M.G., Abd EI-Wahed, M. (eds) The Geology of the Arabian-Nubian Shield. Regional Geology Reviews. Springer, Cham. https://doi.org/10.1007/978-3-030-72995-0_7
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