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      Nile waterscapes facilitated the construction of the Giza pyramids during the 3rd millennium BCE

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          Significance

          The pyramids of Giza constitute one of the world’s most iconic cultural landscapes and have fascinated humanity for thousands of years. Indeed, the Great Pyramid of Giza (Khufu Pyramid) was one of the Seven Wonders of the Ancient World. It is now accepted that ancient Egyptian engineers exploited a former channel of the Nile to transport building materials and provisions to the Giza plateau. However, there is a paucity of environmental evidence regarding when, where, and how these ancient landscapes evolved. New palaeoecological analyses have helped to reconstruct an 8,000-year fluvial history of the Nile in this area, showing that the former waterscapes and higher river levels around 4,500 years ago facilitated the construction of the Giza Pyramid Complex.

          Abstract

          The pyramids of Giza originally overlooked a now defunct arm of the Nile. This fluvial channel, the Khufu branch, enabled navigation to the Pyramid Harbor complex but its precise environmental history is unclear. To fill this knowledge gap, we use pollen-derived vegetation patterns to reconstruct 8,000 y of fluvial variations on the Giza floodplain. After a high-stand level concomitant with the African Humid Period, our results show that Giza’s waterscapes responded to a gradual insolation-driven aridification of East Africa, with the lowest Nile levels recorded at the end of the Dynastic Period. The Khufu branch remained at a high-water level (∼40% of its Holocene maximum) during the reigns of Khufu, Khafre, and Menkaure, facilitating the transportation of construction materials to the Giza Pyramid Complex.

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          Migrations and dynamics of the intertropical convergence zone.

          Rainfall on Earth is most intense in the intertropical convergence zone (ITCZ), a narrow belt of clouds centred on average around six degrees north of the Equator. The mean position of the ITCZ north of the Equator arises primarily because the Atlantic Ocean transports energy northward across the Equator, rendering the Northern Hemisphere warmer than the Southern Hemisphere. On seasonal and longer timescales, the ITCZ migrates, typically towards a warming hemisphere but with exceptions, such as during El Niño events. An emerging framework links the ITCZ to the atmospheric energy balance and may account for ITCZ variations on timescales from years to geological epochs.
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            Climate-controlled Holocene occupation in the Sahara: motor of Africa's evolution.

            Radiocarbon data from 150 archaeological excavations in the now hyper-arid Eastern Sahara of Egypt, Sudan, Libya, and Chad reveal close links between climatic variations and prehistoric occupation during the past 12,000 years. Synoptic multiple-indicator views for major time slices demonstrate the transition from initial settlement after the sudden onset of humid conditions at 8500 B.C.E. to the exodus resulting from gradual desiccation since 5300 B.C.E. Southward shifting of the desert margin helped trigger the emergence of pharaonic civilization along the Nile, influenced the spread of pastoralism throughout the continent, and affects sub-Saharan Africa to the present day.
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              La2010: a new orbital solution for the long-term motion of the Earth

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                Author and article information

                Journal
                Proc Natl Acad Sci U S A
                Proc Natl Acad Sci U S A
                pnas
                PNAS
                Proceedings of the National Academy of Sciences of the United States of America
                National Academy of Sciences
                0027-8424
                1091-6490
                29 August 2022
                13 September 2022
                1 March 2023
                : 119
                : 37
                : e2202530119
                Affiliations
                [1] aAix Marseille Université, CNRS, IRD, INRA, Collège de France, CEREGE , 13545 Aix-en-Provence Cedex 04, France;
                [2] bEuropôle méditerranéen de l’Arbois, Institut Méditerranéen de Biodiversité et d’Ecologie - IMBE (Aix Marseille Univ, Avignon Université, CNRS, IRD) , 13545 Aix-en-Provence Cedex 04, France;
                [3] cTRACES, UMR 5608 CNRS, Université Toulouse Jean Jaurès, Maison de la Recherche , 31058 Toulouse Cedex 9, France;
                [4] dDépartement de Biologie et Géosciences, Université Paul Sabatier - Toulouse 3 , 31062 Toulouse Cedex 9, France;
                [5] eCNRS, ThéMA, Université de Franche-Comté, UMR 6049, MSHE Ledoux , 25030 Besançon, France;
                [6] fDepartment of Geography and GIS, Faculty of Arts, Ain Shams University , 11516 Ain Shams Cairo, Egypt;
                [7] gSKLEC-State Key Laboratory of Estuarine and Coastal Research, East China Normal University ECNU , Shanghai 200062, China;
                [8] hNational Research Institute of Astronomy and Geophysics , 11421 Helwan, Egypt;
                [9] iEPHE-Section des Sciences Historiques et Philologiques, AOROC, UMR 8546 - Archéologie et Philologie d’Orient et d’Occident, CNRS/PSL, École Normale Supérieure, 75230 Paris Cedex 5, France
                Author notes
                1To whom correspondence may be addressed. Email: sheisha@ 123456cerege.fr .

                Edited by Linda Manzanilla, Universidad Nacional Autonóma de México, Mexico, D.F., Mexico; received February 13, 2022; accepted June 29, 2022

                Author contributions: H.S., D.K., N.M., and C.M. designed research; H.S., D.K., N.M., G.Y., and C.M. performed research; H.S., D.K., N.M., M.D., Z.C., G.E.-Q., A.S., A.V., and C.M. contributed new reagents/analytic tools; H.S., D.K., N.M., M.D., and C.M. analyzed data; and H.S., D.K., N.M., M.D., and C.M. wrote the paper.

                Author information
                https://orcid.org/0000-0001-6569-3184
                https://orcid.org/0000-0002-7916-6059
                https://orcid.org/0000-0002-2270-5357
                https://orcid.org/0000-0003-0580-6057
                https://orcid.org/0000-0002-5444-1851
                https://orcid.org/0000-0003-2634-8737
                https://orcid.org/0000-0002-0933-4053
                https://orcid.org/0000-0002-1910-151X
                Article
                202202530
                10.1073/pnas.2202530119
                9477388
                36037388
                fa81d412-5610-4bf3-9cee-d0b8eaa5df4a
                Copyright © 2022 the Author(s). Published by PNAS.

                This article is distributed under Creative Commons Attribution-NonCommercial-NoDerivatives License 4.0 (CC BY-NC-ND).

                History
                : 29 June 2022
                Page count
                Pages: 6
                Funding
                Funded by: the ARKAIA institute
                Award ID: Giza project
                Award Recipient : David Kaniewski Award Recipient : Nick Marriner Award Recipient : Zhongyuan Chen Award Recipient : Christophe Morhange
                Funded by: the China National Natural Science Foundation
                Award ID: 41620104004
                Award Recipient : David Kaniewski Award Recipient : Nick Marriner Award Recipient : Zhongyuan Chen Award Recipient : Christophe Morhange
                Funded by: the CEREGE laboratory (APIC research project)
                Award ID: 00000
                Award Recipient : David Kaniewski Award Recipient : Nick Marriner Award Recipient : Zhongyuan Chen Award Recipient : Christophe Morhange
                Funded by: the Excellence Initiative of Aix-Marseille University
                Award ID: 00000
                Award Recipient : David Kaniewski Award Recipient : Nick Marriner Award Recipient : Zhongyuan Chen Award Recipient : Christophe Morhange
                Funded by: the A*MIDEX, a French "Investissements d'Avenir" programme
                Award ID: 00000
                Award Recipient : David Kaniewski Award Recipient : Nick Marriner Award Recipient : Zhongyuan Chen Award Recipient : Christophe Morhange
                Funded by: the MITI-CNRS (Evénements rares program) (AQUASANMARCO project)
                Award ID: 00000
                Award Recipient : David Kaniewski Award Recipient : Nick Marriner Award Recipient : Zhongyuan Chen Award Recipient : Christophe Morhange
                Funded by: the MSHE - Université de Franche-Comte
                Award ID: GIZAPORT project
                Award Recipient : David Kaniewski Award Recipient : Nick Marriner Award Recipient : Zhongyuan Chen Award Recipient : Christophe Morhange
                Categories
                402
                417
                Physical Sciences
                Environmental Sciences
                Biological Sciences
                Anthropology

                great pyramid,nile,giza harbour
                great pyramid, nile, giza harbour

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