1
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Ro S, Park J, Yoo H, Han C, Lee A, Lee Y, Kim M, Han Y, Svensson A, Shin J, Ro CU, Hong S. Millennial-scale variability of Greenland dust provenance during the last glacial maximum as determined by single particle analysis. Sci Rep 2024; 14:2040. [PMID: 38263283 PMCID: PMC10805741 DOI: 10.1038/s41598-024-52546-x] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [Grants] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 12/13/2023] [Accepted: 01/19/2024] [Indexed: 01/25/2024] Open
Abstract
Greenland ice core records exhibited 100-fold higher dust concentrations during the Last Glacial Maximum (LGM) than during the Holocene, and dust input temporal variability corresponded to different climate states in the LGM. While East Asian deserts, the Sahara, and European loess have been suggested as the potential source areas (PSAs) for Greenland LGM dust, millennial-scale variability in their relative contributions within the LGM remains poorly constrained. Here, we present the morphological, mineralogical, and geochemical characteristics of insoluble microparticles to constrain the provenance of dust in Greenland NEEM ice core samples covering cold Greenland Stadials (GS)-2.1a to GS-3 (~ 14.7 to 27.1 kyr ago) in the LGM. The analysis was conducted on individual particles in microdroplet samples by scanning electron microscopy with energy dispersive X-ray spectroscopy and Raman microspectroscopy. We found that the kaolinite-to-chlorite (K/C) ratios and chemical index of alteration (CIA) values were substantially higher (K/C: 1.4 ± 0.7, CIA: 74.7 ± 2.9) during GS-2.1a to 2.1c than during GS-3 (K/C: 0.5 ± 0.1, CIA: 65.8 ± 2.8). Our records revealed a significant increase in Saharan dust contributions from GS-2.1a to GS-2.1c and that the Gobi Desert and/or European loess were potential source(s) during GS-3. This conclusion is further supported by distinctly different carbon contents in particles corresponding to GS-2.1 and GS-3. These results are consistent with previous estimates of proportional dust source contributions obtained using a mixing model based on Pb and Sr isotopic compositions in NEEM LGM ice and indicate millennial-scale changes in Greenland dust provenance that are probably linked to large-scale atmospheric circulation variabilities during the LGM.
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Affiliation(s)
- Seokhyun Ro
- Department of Ocean Sciences, Inha University, 100 Inha-ro, Michuhol-gu, Incheon, 22212, Republic of Korea
- Division of Glacial Environment Research, Korea Polar Research Institute, 26 Songdomirae-ro, Yeonsu-gu, Incheon, 21990, Republic of Korea
| | - Jonghyeon Park
- Department of Chemistry, Inha University, 100 Inha-ro, Michuhol-gu, Incheon, 22212, Republic of Korea
- Marine Environment Research Department, Ara Consulting and Technology, 30 Songdomirae-ro, Yeonsu-gu, Incheon, 21990, Republic of Korea
| | - Hanjin Yoo
- Department of Chemistry, Inha University, 100 Inha-ro, Michuhol-gu, Incheon, 22212, Republic of Korea
- Particle Pollution Research and Management Center, Inha University, 36 Gaetbeol-ro, Yeonsu-gu, Incheon, 21999, Republic of Korea
| | - Changhee Han
- Department of Water Environmental Safety Management, Korea Water Resources Corporation, 200 Sintanjin-ro, Daedeok-gu, Daejeon, 34350, Republic of Korea
| | - Ahhyung Lee
- Department of Ocean Sciences, Inha University, 100 Inha-ro, Michuhol-gu, Incheon, 22212, Republic of Korea
- Unit of Frontier Exploration, Korea Polar Research Institute, 26 Songdomirae-ro, Yeonsu-gu, Incheon, 21990, Republic of Korea
| | - Yoojin Lee
- Department of Chemistry, Inha University, 100 Inha-ro, Michuhol-gu, Incheon, 22212, Republic of Korea
| | - Minjeong Kim
- Division of Glacial Environment Research, Korea Polar Research Institute, 26 Songdomirae-ro, Yeonsu-gu, Incheon, 21990, Republic of Korea
- Department of Chemistry, Inha University, 100 Inha-ro, Michuhol-gu, Incheon, 22212, Republic of Korea
| | - Yeongcheol Han
- Division of Glacial Environment Research, Korea Polar Research Institute, 26 Songdomirae-ro, Yeonsu-gu, Incheon, 21990, Republic of Korea
| | - Anders Svensson
- Centre for Ice and Climate, Niels Bohr Institute, University of Copenhagen, Julian 10 Maries Vej 30, 2100, Copenhagen, Denmark
| | - Jinhwa Shin
- Division of Glacial Environment Research, Korea Polar Research Institute, 26 Songdomirae-ro, Yeonsu-gu, Incheon, 21990, Republic of Korea
| | - Chul-Un Ro
- Department of Chemistry, Inha University, 100 Inha-ro, Michuhol-gu, Incheon, 22212, Republic of Korea.
- Particle Pollution Research and Management Center, Inha University, 36 Gaetbeol-ro, Yeonsu-gu, Incheon, 21999, Republic of Korea.
| | - Sungmin Hong
- Department of Ocean Sciences, Inha University, 100 Inha-ro, Michuhol-gu, Incheon, 22212, Republic of Korea.
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2
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Moreno J, Ramos AM, Raposeiro PM, Santos RN, Rodrigues T, Naughton F, Moreno F, Trigo RM, Ibañez-Insa J, Ludwig P, Shi X, Hernández A. Identifying imprints of externally derived dust and halogens in the sedimentary record of an Iberian alpine lake for the past ∼13,500 years - Lake Peixão, Serra da Estrela (Central Portugal). THE SCIENCE OF THE TOTAL ENVIRONMENT 2023; 903:166179. [PMID: 37572895 DOI: 10.1016/j.scitotenv.2023.166179] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Subscribe] [Scholar Register] [Received: 03/07/2023] [Revised: 08/04/2023] [Accepted: 08/07/2023] [Indexed: 08/14/2023]
Abstract
Iberian lacustrine sediments are a valuable archive to document environmental changes since the last glacial termination, seen as key for anticipating future climate/environmental changes and their far-reaching implications for generations to come. Herein, multi-proxy-based indicators of a mountain lake record from Serra da Estrela were used to reconstruct atmospheric (in)fluxes and associated climatic/environmental changes over the last ∼13.5 ka. Depositions of long-range transported dust (likely from the Sahara) and halogens (primarily derived from seawater) were higher for the pre-Holocene, particularly in the late Bølling-Allerød-Younger Dryas period, compared to the Holocene. This synchronous increase could be related to a recognized dust-laden atmosphere, along with the combined effect of (i) an earlier proposed effective transport of Sahara dust for higher latitudes during cold periods and (ii) the progressive Polar Front expansion southwards, with the amplification of halogen activation reactions in lower latitudes due to greater closeness to snow/sea ice (halide-laden) surfaces. Additionally, the orographic blocking of Serra da Estrela may have played a critical role in increasing precipitation of Atlantic origin at higher altitudes, with the presence of snow prompting physical and chemical processes involving halogen species. In the Late Holocene, the dust proxy records highlighted two periods of enhanced input to Lake Peixão, the first (∼3.5-2.7 ka BP) after the end of the last African Humid Period and the second, from the 19th century onwards, agreeing with the advent of commercial agriculture, and human contribution to land degradation and dust emission in the Sahara/Sahel region. The oceanic imprints throughout the Holocene matched well with North Atlantic rapid climatic changes that, in turn, coincided with ice-rafted debris or Bond events and other records of increased storminess for the European coasts. Positive parallel peaks in halogens were found in recent times, probably connected to fire extinction by halogenated alkanes and roadway de-icing.
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Affiliation(s)
- J Moreno
- Universidade de Lisboa, Faculdade de Ciências, Instituto Dom Luiz, 1749-016 Lisboa, Portugal.
| | - A M Ramos
- Universidade de Lisboa, Faculdade de Ciências, Instituto Dom Luiz, 1749-016 Lisboa, Portugal; Institute of Meteorology and Climate Research, Karlsruhe Institute of Technology, Karlsruhe, Germany
| | - P M Raposeiro
- CIBIO, Centro de Investigação em Biodiversidade e Recursos Genéticos, InBIO Laboratório Associado, Pólo dos Açores, Rua da Mãe de Deus, 9500-321 Ponta Delgada, Portugal; Faculdade de Ciências e Tecnologia, Universidade dos Açores, Rua da Mãe de Deus, 9500-321 Ponta Delgada, Portugal
| | - R N Santos
- Instituto Português do Mar e da Atmosfera (IPMA), Rua C do Aeroporto, 1749-077 Lisboa, Portugal
| | - T Rodrigues
- Instituto Português do Mar e da Atmosfera (IPMA), Rua C do Aeroporto, 1749-077 Lisboa, Portugal; Centro de Ciências do Mar (CCMAR), Universidade do Algarve, Estrada da Penha, 8005-139 Faro, Portugal
| | - F Naughton
- Instituto Português do Mar e da Atmosfera (IPMA), Rua C do Aeroporto, 1749-077 Lisboa, Portugal; Centro de Ciências do Mar (CCMAR), Universidade do Algarve, Estrada da Penha, 8005-139 Faro, Portugal
| | - F Moreno
- Independent Researcher, Caminho da Portela, n. ° 97, Cascalha, 4940-061 Bico PCR, Portugal
| | - R M Trigo
- Universidade de Lisboa, Faculdade de Ciências, Instituto Dom Luiz, 1749-016 Lisboa, Portugal; Departamento de Meteorologia, Universidade Federal do Rio de Janeiro, Rio de Janeiro, 21941-919, Brazil
| | - J Ibañez-Insa
- Geosciences Barcelona (GEO3BCN-CSIC), Lluís Solé i Sabarís s/n, E-08028 Barcelona, Spain
| | - P Ludwig
- Institute of Meteorology and Climate Research, Karlsruhe Institute of Technology, Karlsruhe, Germany
| | - X Shi
- Alfred Wegener Institute, Helmholtz Center for Polar and Marine Research, Bremerhaven, Germany; Southern Marine Science and Engineering Guangdong Laboratory (Zhuhai), China
| | - A Hernández
- Universidade da Coruña, GRICA Group, Centro Interdisciplinar de Química e Bioloxía (CICA), Rúa As Carballeiras, 15071 A Coruña, Spain
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3
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Armstrong E, Tallavaara M, Hopcroft PO, Valdes PJ. North African humid periods over the past 800,000 years. Nat Commun 2023; 14:5549. [PMID: 37684244 PMCID: PMC10491769 DOI: 10.1038/s41467-023-41219-4] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [Grants] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 01/03/2023] [Accepted: 08/24/2023] [Indexed: 09/10/2023] Open
Abstract
The Sahara region has experienced periodic wet periods over the Quaternary and beyond. These North African Humid Periods (NAHPs) are astronomically paced by precession which controls the intensity of the African monsoon system. However, most climate models cannot reconcile the magnitude of these events and so the driving mechanisms remain poorly constrained. Here, we utilise a recently developed version of the HadCM3B coupled climate model that simulates 20 NAHPs over the past 800 kyr which have good agreement with NAHPs identified in proxy data. Our results show that precession determines NAHP pacing, but we identify that their amplitude is strongly linked to eccentricity via its control over ice sheet extent. During glacial periods, enhanced ice-albedo driven cooling suppresses NAHP amplitude at precession minima, when humid conditions would otherwise be expected. This highlights the importance of both precession and eccentricity, and the role of high latitude processes in determining the timing and amplitude of the NAHPs. This may have implications for the out of Africa dispersal of plants and animals throughout the Quaternary.
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Affiliation(s)
- Edward Armstrong
- Department of Geosciences and Geography, University of Helsinki, Helsinki, Finland.
| | - Miikka Tallavaara
- Department of Geosciences and Geography, University of Helsinki, Helsinki, Finland
| | - Peter O Hopcroft
- School of Geography, Earth and Environmental Sciences, University of Birmingham, Birmingham, UK
| | - Paul J Valdes
- School of Geographical Sciences, University of Bristol, Bristol, UK
- Cabot Institute, University of Bristol, Bristol, UK
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4
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Ruan J, Timmermann A, Raia P, Yun KS, Zeller E, Mondanaro A, Di Febbraro M, Lemmon D, Castiglione S, Melchionna M. Climate shifts orchestrated hominin interbreeding events across Eurasia. Science 2023; 381:699-704. [PMID: 37561879 DOI: 10.1126/science.add4459] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [MESH Headings] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 08/29/2022] [Accepted: 04/19/2023] [Indexed: 08/12/2023]
Abstract
When, where, and how often hominin interbreeding happened is largely unknown. We study the potential for Neanderthal-Denisovan admixture using species distribution models that integrate extensive fossil, archaeological, and genetic data with transient coupled general circulation model simulations of global climate and biomes. Our Pleistocene hindcast of past hominins' habitat suitability reveals pronounced climate-driven zonal shifts in the main overlap region of Denisovans and Neanderthals in central Eurasia. These shifts, which influenced the timing and intensity of potential interbreeding events, can be attributed to the response of climate and vegetation to past variations in atmospheric carbon dioxide and Northern Hemisphere ice-sheet volume. Therefore, glacial-interglacial climate swings likely played an important role in favoring gene flow between archaic humans.
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Affiliation(s)
- Jiaoyang Ruan
- Center for Climate Physics, Institute for Basic Science, Busan, South Korea
- Center for Climate Physics, Pusan National University, Busan, South Korea
| | - Axel Timmermann
- Center for Climate Physics, Institute for Basic Science, Busan, South Korea
- Center for Climate Physics, Pusan National University, Busan, South Korea
| | - Pasquale Raia
- DiSTAR, Monte Sant'Angelo, Napoli Università di Napoli Federico II, Naples, Italy
| | - Kyung-Sook Yun
- Center for Climate Physics, Institute for Basic Science, Busan, South Korea
- Center for Climate Physics, Pusan National University, Busan, South Korea
| | - Elke Zeller
- Center for Climate Physics, Institute for Basic Science, Busan, South Korea
- Department of Climate System, Pusan National University, Busan, South Korea
| | | | - Mirko Di Febbraro
- Department of Biosciences and Territory, University of Molise, C. da Fonte Lappone, Pesche, Italy
| | - Danielle Lemmon
- Center for Climate Physics, Institute for Basic Science, Busan, South Korea
- Center for Climate Physics, Pusan National University, Busan, South Korea
| | - Silvia Castiglione
- DiSTAR, Monte Sant'Angelo, Napoli Università di Napoli Federico II, Naples, Italy
| | - Marina Melchionna
- DiSTAR, Monte Sant'Angelo, Napoli Università di Napoli Federico II, Naples, Italy
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5
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Ait Brahim Y, Sha L, Wassenburg JA, Azennoud K, Cheng H, Cruz FW, Bouchaou L. The spatiotemporal extent of the Green Sahara during the last glacial period. iScience 2023; 26:107018. [PMID: 37416475 PMCID: PMC10320408 DOI: 10.1016/j.isci.2023.107018] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Download PDF] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 10/11/2022] [Revised: 03/19/2023] [Accepted: 05/30/2023] [Indexed: 07/08/2023] Open
Abstract
The Sahara Desert, one of today's most inhospitable environments, has known periods of enhanced precipitation that supported pre-historic humans. However, the Green Sahara timing and moisture sources are not well known due to limited paleoclimate information. Here, we present a multi-proxy (δ18O, δ13C, Δ17O, and trace elements) speleothem-based climate record from Northwest (NW) Africa. Our data document two Green Sahara periods during Marine Isotope Stage (MIS) 5a and the Early to Mid-Holocene. Consistency with paleoclimate records across North Africa highlights the east-west geographical extent of the Green Sahara, whereas millennial-scale North Atlantic cooling (Heinrich) events consistently resulted in drier conditions. We demonstrate that an increase in westerly-originating winter precipitation during MIS5a resulted in favorable environmental conditions. The comparison of paleoclimate data with local archaeological sequences highlights the abrupt climate deterioration and the decline in human density in NW Africa during the MIS5-4 transition, which suggests climate-forced dispersals of populations, with possible implications for pathways into Eurasia.
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Affiliation(s)
- Yassine Ait Brahim
- International Water Research Institute, Mohammed VI Polytechnic University, Benguerir, Morocco
| | - Lijuan Sha
- Institute of Global Environmental Change, Xi’an Jiaotong Uniersity, Xi’an, China
| | - Jasper A. Wassenburg
- Center for Climate Physics, Institute for Basic Science, Busan, 46241, Republic of Korea
- Pusan National University, Busan, 46241, Republic of Korea
| | - Khalil Azennoud
- International Water Research Institute, Mohammed VI Polytechnic University, Benguerir, Morocco
| | - Hai Cheng
- Institute of Global Environmental Change, Xi’an Jiaotong Uniersity, Xi’an, China
| | - Francisco W. Cruz
- Instituto de Geociências, University of Sao Paulo, Sao Paulo, Brazil
| | - Lhoussaine Bouchaou
- International Water Research Institute, Mohammed VI Polytechnic University, Benguerir, Morocco
- Laboratory of Applied Geology and Geo-Environmental, Ibn Zohr University, Agadir, Morocco
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6
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Guo Q, He Z, Wang Z. Long-term projection of future climate change over the twenty-first century in the Sahara region in Africa under four Shared Socio-Economic Pathways scenarios. ENVIRONMENTAL SCIENCE AND POLLUTION RESEARCH INTERNATIONAL 2023; 30:22319-22329. [PMID: 36284044 DOI: 10.1007/s11356-022-23813-z] [Citation(s) in RCA: 5] [Impact Index Per Article: 5.0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 08/17/2022] [Accepted: 10/19/2022] [Indexed: 06/16/2023]
Abstract
Climate change affects air quality and people's health. Therefore, accurate prediction of future climate change is of great significance for human beings to better adapt and mitigate climate change. Using the projection simulation dataset of the CMIP6 multi-model ensemble, the future climate change in the Sahara region under the four scenarios (SSP1-2.6, SSP2-4.5, SSP3-7.0, and SSP5-8.5) is analyzed. The results show that annual and seasonal average surface air temperature in the Sahara region will continue to rise throughout the twenty-first century relative to the baseline period 1995-2014 if greenhouse gas (GHG) concentrations continue increasing. Under the four SSPs scenarios, the warming in the Sahara region will be more pronounced than in the whole world through the twenty-first century. The annual maximum temperature (TX), the annual minimum temperature (TN), the annual count of days with maximum temperature above 35 °C (TX 35), and the annual count of days with maximum temperature above 40 °C (TX 40) in the Sahara region will continue to increase until the end of the twenty-first century under the four scenarios. The results of climate change prediction can provide scientific reference for climate policy-making.
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Affiliation(s)
- Qingchun Guo
- School of Geography and Environment, Liaocheng University, Liaocheng, 252000, China.
- State Key Laboratory of Loess and Quaternary Geology, Institute of Earth Environment, Chinese Academy of Sciences, Xi'an, 710061, China.
| | - Zhenfang He
- School of Geography and Environment, Liaocheng University, Liaocheng, 252000, China.
- State Key Laboratory of Urban and Regional Ecology, Research Center for Eco-Environmental Sciences, Chinese Academy of Sciences, Beijing, 100085, China.
| | - Zhaosheng Wang
- National Ecosystem Science Data Center, Key Laboratory of Ecosystem Network Observation and Modeling, Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences, Beijing, 100101, China.
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7
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Pleistocene drivers of Northwest African hydroclimate and vegetation. Nat Commun 2022; 13:3552. [PMID: 35729104 PMCID: PMC9213457 DOI: 10.1038/s41467-022-31120-x] [Citation(s) in RCA: 4] [Impact Index Per Article: 2.0] [Reference Citation Analysis] [Abstract] [Track Full Text] [Download PDF] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 04/22/2021] [Accepted: 06/06/2022] [Indexed: 11/09/2022] Open
Abstract
Savanna ecosystems were the landscapes for human evolution and are vital to modern Sub-Saharan African food security, yet the fundamental drivers of climate and ecology in these ecosystems remain unclear. Here we generate plant-wax isotope and dust flux records to explore the mechanistic drivers of the Northwest African monsoon, and to assess ecosystem responses to changes in monsoon rainfall and atmospheric pCO2. We show that monsoon rainfall is controlled by low-latitude insolation gradients and that while increases in precipitation are associated with expansion of grasslands into desert landscapes, changes in pCO2 predominantly drive the C3/C4 composition of savanna ecosystems.
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8
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Past 200 kyr hydroclimate variability in the western Mediterranean and its connection to the African Humid Periods. Sci Rep 2022; 12:9050. [PMID: 35641528 PMCID: PMC9156737 DOI: 10.1038/s41598-022-12047-1] [Citation(s) in RCA: 1] [Impact Index Per Article: 0.5] [Reference Citation Analysis] [Abstract] [Track Full Text] [Download PDF] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 11/05/2021] [Accepted: 04/21/2022] [Indexed: 11/30/2022] Open
Abstract
The Iberian Peninsula is located at the intersection between the subtropical and temperate climate zones and the paleoclimate records from this region are key to elucidate the varying humidity and changing dominance of atmospheric circulation patterns in the Mediterranean-North African region in the past. Here we present a quantitative hydroclimate reconstruction for the last ca. 200 kyr from southern Iberian Peninsula based on pollen data from the Padul lake sediment record. We use the newly developed Scale-normalized Significant Zero crossing (SnSiZer) method to detect not only the statistically significant precipitation changes but also to estimate the relative magnitude of these oscillations in our reconstruction. We identify six statistically significant main humid phases, termed West Mediterranean Humid Periods (WMHP 1–6). These humid periods correlate with other West/Central Mediterranean paleohydrological records, suggesting that similar climatic factors affected different areas of the Mediterranean. In addition, the WMPHs are roughly coeval with the African Humid Periods (AHPs) during high seasonality, suggesting the same North Atlantic ocean-atmospheric dynamics and orbital forcing as main drivers of both areas. In contrast, during low seasonality periods, the West Mediterranean still appears to be affected by the westerlies and the local Mediterranean rainfall systems with moderate-to-high precipitation, whereas West Africa was characterized by droughts.
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9
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Gosling WD, Scerri EML, Kaboth-Bahr S. The climate and vegetation backdrop to hominin evolution in Africa. Philos Trans R Soc Lond B Biol Sci 2022; 377:20200483. [PMID: 35249389 PMCID: PMC8899624 DOI: 10.1098/rstb.2020.0483] [Citation(s) in RCA: 2] [Impact Index Per Article: 1.0] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 12/22/2022] Open
Abstract
The most profound shift in the African hydroclimate of the last 1 million years occurred around 300 thousand years (ka) ago. This change in African hydroclimate is manifest as an east-west change in moisture balance that cannot be fully explained through linkages to high latitude climate systems. The east-west shift is, instead, probably driven by a shift in the tropical Walker Circulation related to sea surface temperature change driven by orbital forcing. Comparing records of past vegetation change, and hominin evolution and development, with this breakpoint in the climate system is challenging owing to the paucity of study sites available and uncertainties regarding the dating of records. Notwithstanding these uncertainties we find that, broadly speaking, both vegetation and hominins change around 300 ka. The vegetative backdrop suggests that relative abundance of vegetative resources shifted from western to eastern Africa, although resources would have persisted across the continent. The climatic and vegetation changes probably provided challenges for hominins and are broadly coincident with the appearance of Homo sapiens (ca 315 ka) and the emergence of Middle Stone Age technology. The concomitant changes in climate, vegetation and hominin evolution suggest that these factors are closely intertwined. This article is part of the theme issue 'Tropical forests in the deep human past'.
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Affiliation(s)
- William D Gosling
- Institute for Biodiversity and Ecosystem Dynamics, University of Amsterdam, Amsterdam, The Netherlands
| | - Eleanor M L Scerri
- Max Planck Institute for the Science of Human History, Jena, Germany.,Department of Classics and Archaeology, University of Malta, Msida, Malta.,Department of Prehistoric Archaeology, University of Cologne, 50931 Cologne, Germany
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10
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Cooper JC, Crouch NMA, Ferguson AW, Bates JM. Climatic refugia and reduced extinction correlate with underdispersion in mammals and birds in Africa. Ecol Evol 2022; 12:e8752. [PMID: 35356571 PMCID: PMC8941498 DOI: 10.1002/ece3.8752] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Download PDF] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 10/07/2021] [Revised: 02/18/2022] [Accepted: 03/03/2022] [Indexed: 11/16/2022] Open
Abstract
Macroevolutionary patterns, often inferred from metrics of community relatedness, are often used to ascertain major evolutionary processes shaping communities. These patterns have been shown to be informative of biogeographic barriers, of habitat suitability and invasibility (especially with regard to environmental filtering), and of regions that function as evolutionary cradles (i.e., sources of diversification) or museums (i.e., regions of reduced extinction). Here, we analyzed continental datasets of mammal and bird distributions to identify primary drivers of community evolution on the African continent for mostly endothermic vertebrates. We find that underdispersion (i.e., relatively low phylogenetic diversity compared to species richness) closely correlates with specific ecoregions that have been identified as climatic refugia in the literature, regardless of whether these specific regions have been touted as cradles or museums. Using theoretical models of identical communities that differ only with respect to extinction rates, we find that even small suppressions of extinction rates can result in underdispersed communities, supporting the hypothesis that climatic stability can lead to underdispersion. We posit that large‐scale patterns of under‐ and overdispersion between regions of similar species richness are more reflective of a particular region’s extinction potential, and that the very nature of refugia can lead to underdispersion via the steady accumulation of species richness through diversification within the same ecoregion during climatic cycles. Thus, patterns of environmental filtering can be obfuscated by environments that coincide with biogeographic refugia, and considerations of regional biogeographic history are paramount for inferring macroevolutionary processes.
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Affiliation(s)
- Jacob C Cooper
- Committee on Evolutionary Biology University of Chicago Chicago Illinois USA.,Negaunee Integrative Research Center Field Museum Chicago Illinois USA.,Present address: University of Kansas Biodiversity Institute Lawrence Kansas USA
| | - Nicholas M A Crouch
- Department of Geophysical Sciences University of Chicago Chicago Illinois USA
| | - Adam W Ferguson
- Gantz Family Collections Center Field Museum Chicago Illinois USA
| | - John M Bates
- Negaunee Integrative Research Center Field Museum Chicago Illinois USA
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11
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Lupien RL, Russell JM, Pearson EJ, Castañeda IS, Asrat A, Foerster V, Lamb HF, Roberts HM, Schäbitz F, Trauth MH, Beck CC, Feibel CS, Cohen AS. Orbital controls on eastern African hydroclimate in the Pleistocene. Sci Rep 2022; 12:3170. [PMID: 35210479 PMCID: PMC8873222 DOI: 10.1038/s41598-022-06826-z] [Citation(s) in RCA: 5] [Impact Index Per Article: 2.5] [Reference Citation Analysis] [Abstract] [Track Full Text] [Download PDF] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 07/21/2021] [Accepted: 02/07/2022] [Indexed: 11/24/2022] Open
Abstract
Understanding eastern African paleoclimate is critical for contextualizing early human evolution, adaptation, and dispersal, yet Pleistocene climate of this region and its governing mechanisms remain poorly understood due to the lack of long, orbitally-resolved, terrestrial paleoclimate records. Here we present leaf wax hydrogen isotope records of rainfall from paleolake sediment cores from key time windows that resolve long-term trends, variations, and high-latitude effects on tropical African precipitation. Eastern African rainfall was dominantly controlled by variations in low-latitude summer insolation during most of the early and middle Pleistocene, with little evidence that glacial–interglacial cycles impacted rainfall until the late Pleistocene. We observe the influence of high-latitude-driven climate processes emerging from the last interglacial (Marine Isotope Stage 5) to the present, an interval when glacial–interglacial cycles were strong and insolation forcing was weak. Our results demonstrate a variable response of eastern African rainfall to low-latitude insolation forcing and high-latitude-driven climate change, likely related to the relative strengths of these forcings through time and a threshold in monsoon sensitivity. We observe little difference in mean rainfall between the early, middle, and late Pleistocene, which suggests that orbitally-driven climate variations likely played a more significant role than gradual change in the relationship between early humans and their environment.
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Affiliation(s)
- Rachel L Lupien
- Department of Earth, Environmental, and Planetary Sciences, Brown University, Providence, RI, 02912, USA. .,Biology and Paleo Environment, Lamont-Doherty Earth Observatory of Columbia University, Palisades, NY, 10964, USA.
| | - James M Russell
- Department of Earth, Environmental, and Planetary Sciences, Brown University, Providence, RI, 02912, USA
| | - Emma J Pearson
- School of Geography, Politics & Sociology, Newcastle University, Newcastle Upon Tyne, NE1 7RU, UK
| | - Isla S Castañeda
- Department of Geosciences, University of Massachusetts Amherst, Amherst, MA, 01003, USA
| | - Asfawossen Asrat
- Department of Mining and Geological Engineering, Botswana International University of Science and Technology, Private Bag 16, Palapye, Botswana.,School of Earth Science, Addis Ababa University, Addis Ababa, Ethiopia
| | - Verena Foerster
- Institute for Geography Education, University of Cologne, 50931, Cologne, Germany
| | - Henry F Lamb
- Department of Geography and Earth Sciences, Aberystwyth University, Aberystwyth, SY23 3DB, UK.,Botany Department, Trinity College Dublin, Dublin 2, Ireland
| | - Helen M Roberts
- Department of Geography and Earth Sciences, Aberystwyth University, Aberystwyth, SY23 3DB, UK
| | - Frank Schäbitz
- Institute for Geography Education, University of Cologne, 50931, Cologne, Germany
| | - Martin H Trauth
- Institute of Geosciences, University of Potsdam, 14476, Potsdam, Germany
| | - Catherine C Beck
- Geosciences Department, Hamilton College, Clinton, NY, 13323, USA
| | - Craig S Feibel
- Department of Earth and Planetary Sciences, Rutgers University, Piscataway, NJ, 08854, USA
| | - Andrew S Cohen
- Department of Geosciences, University of Arizona, Tucson, AZ, 85721, USA
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12
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Walas Ł, Taib A. Environmental regionalization and endemic plant distribution in the Maghreb. ENVIRONMENTAL MONITORING AND ASSESSMENT 2022; 194:100. [PMID: 35032243 PMCID: PMC8761123 DOI: 10.1007/s10661-021-09707-6] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Figures] [Subscribe] [Scholar Register] [Received: 09/28/2021] [Accepted: 12/23/2021] [Indexed: 06/14/2023]
Abstract
Clustering methods based on environmental variables are useful in the planning of conservation strategies for species and ecosystems. However, there is a lack of work on the regionalization of the vast space of North Africa and the distribution of plant species. The current lists of endemic plants are focused mostly on an occurrence at the country level and not on regions with different conditions. The aim of this work was to lay out an environmental scheme for northwest Africa and to collect data about the occurrence of endemic plants in this area. Clustering with 12 of 33 tested environmental rasters was performed to divide the Maghreb into environmental clusters. Then, a list of 1618 endemic plant taxa (1243 species and 375 subspecies) was prepared and their distribution in estimated environmental clusters was examined. Eleven clusters with different conditions were estimated. The main drivers of regionalization were temperature amplitude, precipitation seasonality, and precipitation of the warmest quarter. According to the occurrence of endemic plants, northwest Africa may be divided into three zones: Atlas, Mediterranean (two environmental clusters), and southern zone (eight environmental clusters). The presented results provide a good basis for understanding the spatial patterns of the Maghreb, including its environment and species diversity. A designed list of endemic plant species together with environmental data may facilitate the planning of future research in north Africa and arranging methods of biodiversity protection.
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Affiliation(s)
- Łukasz Walas
- Institute of Dendrology Polish Academy of Sciences, Parkowa 5, 62-035 Kórnik, Poland
| | - Asma Taib
- Ecole Nationale Supérieure Agronomique, El Harrach, Algeria
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13
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Hempel E, Westbury MV, Grau JH, Trinks A, Paijmans JLA, Kliver S, Barlow A, Mayer F, Müller J, Chen L, Koepfli KP, Hofreiter M, Bibi F. Diversity and Paleodemography of the Addax ( Addax nasomaculatus), a Saharan Antelope on the Verge of Extinction. Genes (Basel) 2021; 12:genes12081236. [PMID: 34440410 PMCID: PMC8394336 DOI: 10.3390/genes12081236] [Citation(s) in RCA: 5] [Impact Index Per Article: 1.7] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Download PDF] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 07/17/2021] [Revised: 08/05/2021] [Accepted: 08/08/2021] [Indexed: 12/18/2022] Open
Abstract
Since the 19th century, the addax (Addax nasomaculatus) has lost approximately 99% of its former range. Along with its close relatives, the blue antelope (Hippotragus leucophaeus) and the scimitar-horned oryx (Oryx dammah), the addax may be the third large African mammal species to go extinct in the wild in recent times. Despite this, the evolutionary history of this critically endangered species remains virtually unknown. To gain insight into the population history of the addax, we used hybridization capture to generate ten complete mitochondrial genomes from historical samples and assembled a nuclear genome. We found that both mitochondrial and nuclear diversity are low compared to other African bovids. Analysis of mitochondrial genomes revealed a most recent common ancestor ~32 kya (95% CI 11–58 kya) and weak phylogeographic structure, indicating that the addax likely existed as a highly mobile, panmictic population across its Sahelo–Saharan range in the past. PSMC analysis revealed a continuous decline in effective population size since ~2 Ma, with short intermediate increases at ~500 and ~44 kya. Our results suggest that the addax went through a major bottleneck in the Late Pleistocene, remaining at low population size prior to the human disturbances of the last few centuries.
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Affiliation(s)
- Elisabeth Hempel
- Evolutionary Adaptive Genomics, Institute of Biochemistry and Biology, Faculty of Science, University of Potsdam, Karl-Liebknecht-Straße 24-25, 14476 Potsdam, Germany; (J.H.G.); (M.H.)
- Museum für Naturkunde, Berlin, Leibniz Institute for Evolution and Biodiversity Science, Invalidenstraße 43, 10115 Berlin, Germany; (F.M.); (J.M.); (F.B.)
- Correspondence:
| | - Michael V. Westbury
- Evolutionary Adaptive Genomics, Institute of Biochemistry and Biology, Faculty of Science, University of Potsdam, Karl-Liebknecht-Straße 24-25, 14476 Potsdam, Germany; (J.H.G.); (M.H.)
- Section for Evolutionary Genomics, The GLOBE Institute, University of Copenhagen, Øster Voldgade 5-7, 1350 Copenhagen, Denmark;
| | - José H. Grau
- Evolutionary Adaptive Genomics, Institute of Biochemistry and Biology, Faculty of Science, University of Potsdam, Karl-Liebknecht-Straße 24-25, 14476 Potsdam, Germany; (J.H.G.); (M.H.)
- Museum für Naturkunde, Berlin, Leibniz Institute for Evolution and Biodiversity Science, Invalidenstraße 43, 10115 Berlin, Germany; (F.M.); (J.M.); (F.B.)
| | - Alexandra Trinks
- Evolutionary Adaptive Genomics, Institute of Biochemistry and Biology, Faculty of Science, University of Potsdam, Karl-Liebknecht-Straße 24-25, 14476 Potsdam, Germany; (J.H.G.); (M.H.)
- Institute of Pathology, Charité–Universitätsmedizin Berlin, Charitéplatz 1, 10117 Berlin, Germany;
| | - Johanna L. A. Paijmans
- Evolutionary Adaptive Genomics, Institute of Biochemistry and Biology, Faculty of Science, University of Potsdam, Karl-Liebknecht-Straße 24-25, 14476 Potsdam, Germany; (J.H.G.); (M.H.)
- Department of Zoology, University of Cambridge, Downing Street, Cambridge CB2 3EJ, UK;
| | - Sergei Kliver
- Institute of Molecular and Cellular Biology SB RAS, 8/2 Acad. Lavrentiev Ave, 630090 Novosibirsk, Russia;
| | - Axel Barlow
- Evolutionary Adaptive Genomics, Institute of Biochemistry and Biology, Faculty of Science, University of Potsdam, Karl-Liebknecht-Straße 24-25, 14476 Potsdam, Germany; (J.H.G.); (M.H.)
- School of Science and Technology, Nottingham Trent University, Clifton Lane, Nottingham NG11 8NS, UK;
| | - Frieder Mayer
- Museum für Naturkunde, Berlin, Leibniz Institute for Evolution and Biodiversity Science, Invalidenstraße 43, 10115 Berlin, Germany; (F.M.); (J.M.); (F.B.)
| | - Johannes Müller
- Museum für Naturkunde, Berlin, Leibniz Institute for Evolution and Biodiversity Science, Invalidenstraße 43, 10115 Berlin, Germany; (F.M.); (J.M.); (F.B.)
| | - Lei Chen
- School of Ecology and Environment, Northwestern Polytechnical University, Xi’an 710072, China;
| | - Klaus-Peter Koepfli
- Smithsonian-Mason School of Conservation, George Mason University, Front Royal, VA 22630, USA;
- Smithsonian Conservation Biology Institute, Center for Species Survival, National Zoological Park, Front Royal, VA 22630, USA
- Computer Technologies Laboratory, ITMO University, 197101 Saint Petersburg, Russia
| | - Michael Hofreiter
- Evolutionary Adaptive Genomics, Institute of Biochemistry and Biology, Faculty of Science, University of Potsdam, Karl-Liebknecht-Straße 24-25, 14476 Potsdam, Germany; (J.H.G.); (M.H.)
| | - Faysal Bibi
- Museum für Naturkunde, Berlin, Leibniz Institute for Evolution and Biodiversity Science, Invalidenstraße 43, 10115 Berlin, Germany; (F.M.); (J.M.); (F.B.)
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14
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Lupien RL, Russell JM, Subramanian A, Kinyanjui R, Beverly EJ, Uno KT, de Menocal P, Dommain R, Potts R. Eastern African environmental variation and its role in the evolution and cultural change of Homo over the last 1 million years. J Hum Evol 2021; 157:103028. [PMID: 34216947 DOI: 10.1016/j.jhevol.2021.103028] [Citation(s) in RCA: 3] [Impact Index Per Article: 1.0] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 11/17/2020] [Revised: 05/20/2021] [Accepted: 05/20/2021] [Indexed: 10/21/2022]
Abstract
Characterizing eastern African environmental variability on orbital timescales is crucial to evaluating the hominin evolutionary response to past climate changes. However, there is a dearth of high-resolution, well-dated records of ecosystem dynamics from eastern Africa that cover long time intervals. In the last 1 Myr, there were significant anatomical and cultural developments in Homo, including the origin of Homo sapiens. There were also major changes in global climatic boundary conditions that may have affected eastern African environments, yet potential linkages remain poorly understood. We developed carbon isotopic records from plant waxes (δ13Cwax) and bulk organic matter (δ13COM) from a well-dated sediment core spanning the last ∼1 Myr extracted from the Koora Basin, located south of the Olorgesailie Basin, in the southern Kenya rift. Our record characterizes the climatic and environmental context for evolutionary events and technological advances recorded in the adjacent Olorgesailie Basin, such as the transition from Acheulean to Middle Stone Age tools by 320 ka. A significant shift toward more C4-dominated ecosystems and arid conditions occurred near the end of the mid-Pleistocene Transition, which indicates a link between equatorial eastern African and high-latitude northern hemisphere climate. Environmental variability increases throughout the mid- to late-Pleistocene, superimposed by precession-paced packets of variability modulated by eccentricity. An interval of particularly high-amplitude climate and environmental variability occurred from ∼275 ka to ∼180 ka, synchronous with evidence for the first H. sapiens fossils in eastern Africa. These results support the 'variability selection hypothesis' that increased environmental variability selected for adaptable traits, behaviors, and technology in our hominin ancestors.
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Affiliation(s)
- Rachel L Lupien
- Department of Earth, Environmental, and Planetary Sciences, Brown University, Providence, RI 02906, USA; Division of Biology and Paleo Environment, Lamont-Doherty Earth Observatory, Palisades, NY 10964, USA.
| | - James M Russell
- Department of Earth, Environmental, and Planetary Sciences, Brown University, Providence, RI 02906, USA
| | - Avinash Subramanian
- Department of Earth, Environmental, and Planetary Sciences, Brown University, Providence, RI 02906, USA
| | - Rahab Kinyanjui
- Department of Earth Sciences, National Museums of Kenya, Nairobi 00100, Kenya
| | - Emily J Beverly
- Department of Earth and Atmospheric Sciences, University of Houston, Houston, TX 77204, USA
| | - Kevin T Uno
- Division of Biology and Paleo Environment, Lamont-Doherty Earth Observatory, Palisades, NY 10964, USA
| | - Peter de Menocal
- Woods Hole Oceanographic Institution, Woods Hole, MA 02543, USA; Division of Biology and Paleo Environment, Lamont-Doherty Earth Observatory, Palisades, NY 10964, USA
| | - René Dommain
- Institute of Geosciences, University of Potsdam, 14476 Potsdam, Germany; Human Origins Program, National Museum of Natural History, Smithsonian Institution, Washington, DC 20560, USA
| | - Richard Potts
- Human Origins Program, National Museum of Natural History, Smithsonian Institution, Washington, DC 20560, USA; Department of Earth Sciences, National Museums of Kenya, Nairobi 00100, Kenya
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15
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Abstract
The greening of the Sahara, associated with the African Humid Period (AHP) between ca. 14,500 and 5,000 y ago, is arguably the largest climate-induced environmental change in the Holocene; it is usually explained by the strengthening and northward expansion of the African monsoon in response to orbital forcing. However, the strengthened monsoon in Early to Middle Holocene climate model simulations cannot sustain vegetation in the Sahara or account for the increased humidity in the Mediterranean region. Here, we present an 18,500-y pollen and leaf-wax δD record from Lake Tislit (32° N) in Morocco, which provides quantitative reconstruction of winter and summer precipitation in northern Africa. The record from Lake Tislit shows that the northern Sahara and the Mediterranean region were wetter in the AHP because of increased winter precipitation and were not influenced by the monsoon. The increased seasonal contrast of insolation led to an intensification and southward shift of the Mediterranean winter precipitation system in addition to the intensified summer monsoon. Therefore, a winter rainfall zone must have met and possibly overlapped the monsoonal zone in the Sahara. Using a mechanistic vegetation model in Early Holocene conditions, we show that this seasonal distribution of rainfall is more efficient than the increased monsoon alone in generating a green Sahara vegetation cover, in agreement with observed vegetation. This conceptual framework should be taken into consideration in Earth system paleoclimate simulations used to explore the mechanisms of African climatic and environmental sensitivity.
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16
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Quinn RL, Lepre CJ. Contracting eastern African C 4 grasslands during the extinction of Paranthropus boisei. Sci Rep 2021; 11:7164. [PMID: 33785831 PMCID: PMC8009881 DOI: 10.1038/s41598-021-86642-z] [Citation(s) in RCA: 5] [Impact Index Per Article: 1.7] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Download PDF] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 10/04/2020] [Accepted: 03/18/2021] [Indexed: 02/01/2023] Open
Abstract
The extinction of the Paranthropus boisei estimated to just before 1 Ma occurred when C4 grasslands dominated landscapes of the Eastern African Rift System (EARS). P. boisei has been characterized as an herbivorous C4 specialist, and paradoxically, its demise coincided with habitats favorable to its dietary ecology. Here we report new pedogenic carbonate stable carbon (δ13CPC) and oxygen (δ18OPC) values (nodules = 53, analyses = 95) from an under-sampled interval (1.4-0.7 Ma) in the Turkana Basin (Kenya), one of the most fossiliferous locales of P. boisei. We combined our new results with published δ13CPC values from the EARS dated to 3-0 Ma, conducted time-series analysis of woody cover (ƒWC), and compared the EARS ƒWC trends to regional and global paleo-environmental and -climatic datasets. Our results demonstrate that the long-term rise of C4 grasslands was punctuated by a transient but significant increase in C3 vegetation and warmer temperatures, coincident with the Mid-Pleistocene Transition (1.3-0.7 Ma) and implicating a short-term rise in pCO2. The contraction of C4 grasslands escalated dietary competition amongst the abundant C4-feeders, likely influencing P. boisei's demise.
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Affiliation(s)
- Rhonda L. Quinn
- grid.263379.a0000 0001 2172 0072Department of Sociology, Anthropology, Social Work and Criminal Justice, Seton Hall University, 400 South Orange Ave, South Orange, NJ 07079 USA ,grid.430387.b0000 0004 1936 8796Department of Earth and Planetary Sciences, Rutgers University, 610 Taylor Road, Piscataway, NJ 08854 USA
| | - Christopher J. Lepre
- grid.430387.b0000 0004 1936 8796Department of Earth and Planetary Sciences, Rutgers University, 610 Taylor Road, Piscataway, NJ 08854 USA
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17
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18
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Abstract
Glacial-interglacial cycles have constituted a primary mode of climate variability over the last 2.6 million years of Earth's history. While glacial periods cannot be seen simply as a reverse analogue of future warming, they offer an opportunity to test our understanding of the response of precipitation patterns to a much wider range of conditions than we have been able to directly observe. This review explores key features of precipitation patterns associated with glacial climates, which include drying in large regions of the tropics and wetter conditions in substantial parts of the subtropics and midlatitudes. I describe the evidence for these changes and examine the potential causes of hydrological changes during glacial periods. Central themes that emerge include the importance of atmospheric circulation changes in determining glacial-interglacial precipitation changes at the regional scale, the need to take into account climatic factors beyond local precipitation amount when interpreting proxy data, and the role of glacial conditions in suppressing the strength of Northern Hemisphere monsoon systems.
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Affiliation(s)
- David McGee
- Department of Earth, Atmospheric, and Planetary Sciences, Massachusetts Institute of Technology, Cambridge, Massachusetts 02139, USA;
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19
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Waelbroeck C, Lougheed BC, Vazquez Riveiros N, Missiaen L, Pedro J, Dokken T, Hajdas I, Wacker L, Abbott P, Dumoulin JP, Thil F, Eynaud F, Rossignol L, Fersi W, Albuquerque AL, Arz H, Austin WEN, Came R, Carlson AE, Collins JA, Dennielou B, Desprat S, Dickson A, Elliot M, Farmer C, Giraudeau J, Gottschalk J, Henderiks J, Hughen K, Jung S, Knutz P, Lebreiro S, Lund DC, Lynch-Stieglitz J, Malaizé B, Marchitto T, Martínez-Méndez G, Mollenhauer G, Naughton F, Nave S, Nürnberg D, Oppo D, Peck V, Peeters FJC, Penaud A, Portilho-Ramos RDC, Repschläger J, Roberts J, Rühlemann C, Salgueiro E, Sanchez Goni MF, Schönfeld J, Scussolini P, Skinner LC, Skonieczny C, Thornalley D, Toucanne S, Rooij DV, Vidal L, Voelker AHL, Wary M, Weldeab S, Ziegler M. Consistently dated Atlantic sediment cores over the last 40 thousand years. Sci Data 2019; 6:165. [PMID: 31477737 PMCID: PMC6718518 DOI: 10.1038/s41597-019-0173-8] [Citation(s) in RCA: 42] [Impact Index Per Article: 8.4] [Reference Citation Analysis] [Abstract] [Key Words] [Grants] [Track Full Text] [Download PDF] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 03/12/2019] [Accepted: 08/08/2019] [Indexed: 11/21/2022] Open
Abstract
Rapid changes in ocean circulation and climate have been observed in marine-sediment and ice cores over the last glacial period and deglaciation, highlighting the non-linear character of the climate system and underlining the possibility of rapid climate shifts in response to anthropogenic greenhouse gas forcing. To date, these rapid changes in climate and ocean circulation are still not fully explained. One obstacle hindering progress in our understanding of the interactions between past ocean circulation and climate changes is the difficulty of accurately dating marine cores. Here, we present a set of 92 marine sediment cores from the Atlantic Ocean for which we have established age-depth models that are consistent with the Greenland GICC05 ice core chronology, and computed the associated dating uncertainties, using a new deposition modeling technique. This is the first set of consistently dated marine sediment cores enabling paleoclimate scientists to evaluate leads/lags between circulation and climate changes over vast regions of the Atlantic Ocean. Moreover, this data set is of direct use in paleoclimate modeling studies.
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Affiliation(s)
- Claire Waelbroeck
- LSCE/IPSL, Laboratoire CNRS-CEA-UVSQ, 91191, Orme des Merisiers, France.
| | - Bryan C Lougheed
- LSCE/IPSL, Laboratoire CNRS-CEA-UVSQ, 91191, Orme des Merisiers, France
| | - Natalia Vazquez Riveiros
- LSCE/IPSL, Laboratoire CNRS-CEA-UVSQ, 91191, Orme des Merisiers, France
- Ifremer, Unité de Geosciences Marines, 29280, Plouzané, France
| | - Lise Missiaen
- LSCE/IPSL, Laboratoire CNRS-CEA-UVSQ, 91191, Orme des Merisiers, France
| | - Joel Pedro
- Uni Research, Nygårdsgaten 112, 5008, Bergen, Norway
| | - Trond Dokken
- Uni Research, Nygårdsgaten 112, 5008, Bergen, Norway
| | - Irka Hajdas
- Laboratory of Ion Beam Physics, ETH Zürich, 8093, Zürich, Switzerland
| | - Lukas Wacker
- Laboratory of Ion Beam Physics, ETH Zürich, 8093, Zürich, Switzerland
| | - Peter Abbott
- School of Earth and Ocean Sciences, Cardiff University, CF10 3AT, Cardiff, UK
- Institute of Geological Sciences and Oeschger Center for Climate Change Research, University of Bern, 3012, Bern, Switzerland
| | - Jean-Pascal Dumoulin
- LSCE/IPSL, Laboratoire CNRS-CEA-UVSQ, 91191, Orme des Merisiers, France
- LMC14, Université Paris-Saclay, F-91191, Gif-sur-Yvette, France
| | - François Thil
- LSCE/IPSL, Laboratoire CNRS-CEA-UVSQ, 91191, Orme des Merisiers, France
| | - Frédérique Eynaud
- EPOC, Université Bordeaux, Allée Geoffroy St Hilaire, 33615, Pessac, France
| | - Linda Rossignol
- EPOC, Université Bordeaux, Allée Geoffroy St Hilaire, 33615, Pessac, France
| | - Wiem Fersi
- LSCE/IPSL, Laboratoire CNRS-CEA-UVSQ, 91191, Orme des Merisiers, France
| | | | - Helge Arz
- Leibniz-Institute for Baltic Sea Research Warnemünde, Seestrasse 15, 18119, Rostock, Germany
| | | | - Rosemarie Came
- University of New Hampshire, 56 College Road, Durham, NH, 03824, USA
| | | | | | | | - Stéphanie Desprat
- EPOC, Université Bordeaux, Allée Geoffroy St Hilaire, 33615, Pessac, France
- Ecole Pratique des Hautes Etudes (EPHE, PSL), 4-14 rue Ferrus, 75014, Paris, France
| | - Alex Dickson
- Royal Holloway University of London, Egham, Surrey, TW20 0EX, UK
| | - Mary Elliot
- LPG-Nantes, Université de Nantes, 44300, Nantes, France
| | | | - Jacques Giraudeau
- EPOC, Université Bordeaux, Allée Geoffroy St Hilaire, 33615, Pessac, France
| | - Julia Gottschalk
- Lamont-Doherty Earth Observatory, Columbia University, 61 Route 9W - PO Box 1000, Palisades, NY, 10964-1000, USA
| | | | - Konrad Hughen
- Woods Hole Oceanographic Institution, 266 Woods Hole Rd., Woods Hole, MA, 02543-1050, USA
| | - Simon Jung
- University of Edinburgh, School of Geosciences, Edinburgh, EH9 3FE, UK
| | - Paul Knutz
- Geological Survey of Denmark and Greenland, Øster Voldgade 10, 1350, Copenhagen, Denmark
| | - Susana Lebreiro
- IGME - Instituto Geológico y Minero de España, Calle Ríos Rosas, 23, 28003, Madrid, Spain
| | - David C Lund
- University of Connecticut, 1080 Shennecossett Road, Groton, CT, 06340, USA
| | | | - Bruno Malaizé
- EPOC, Université Bordeaux, Allée Geoffroy St Hilaire, 33615, Pessac, France
| | | | | | | | - Filipa Naughton
- IPMA-DivGM, Avenida Doutor Alfredo Magalhães Ramalho, 6, 1495-165, Alges, Portugal
- CCMAR, Universidade do Algarve, Campus de Gambelas, 8005-139, Faro, Portugal
| | - Silvia Nave
- LNEG, Bairro do Zambujal, 2610-999, Amadora, Portugal
| | | | - Delia Oppo
- Woods Hole Oceanographic Institution, 266 Woods Hole Rd., Woods Hole, MA, 02543-1050, USA
| | - Victoria Peck
- UK British Antarctic Survey, Madingley Road, Cambridge, CB3 0ET, UK
| | - Frank J C Peeters
- Vrije Universiteit Amsterdam, De Boelelaan 1087, 1081 HV, Amsterdam, Netherlands
| | - Aurélie Penaud
- Université de Bretragne Occidentale, Technopôle Brest-Iroise, 29280, Plouzané, France
| | | | | | - Jenny Roberts
- Thermo Fisher Scientific, Hanna-Kunath Straße 11, Bremen, 28199, Germany
| | | | - Emilia Salgueiro
- IPMA-DivGM, Avenida Doutor Alfredo Magalhães Ramalho, 6, 1495-165, Alges, Portugal
- CCMAR, Universidade do Algarve, Campus de Gambelas, 8005-139, Faro, Portugal
| | - Maria Fernanda Sanchez Goni
- EPOC, Université Bordeaux, Allée Geoffroy St Hilaire, 33615, Pessac, France
- Ecole Pratique des Hautes Etudes (EPHE, PSL), 4-14 rue Ferrus, 75014, Paris, France
| | | | - Paolo Scussolini
- Vrije Universiteit Amsterdam, De Boelelaan 1087, 1081 HV, Amsterdam, Netherlands
| | - Luke C Skinner
- University of Cambridge, Godwin Laboratory for Palaeoclimate Research, Cambridge, CB2 3EQ, UK
| | | | | | - Samuel Toucanne
- Ifremer, Unité de Geosciences Marines, 29280, Plouzané, France
| | | | - Laurence Vidal
- Aix-Marseille Université, CNRS, IRD, INRA, Coll France, CEREGE, Europole de l'Arbois, 13545, Aix-en-Provence, France
| | - Antje H L Voelker
- IPMA-DivGM, Avenida Doutor Alfredo Magalhães Ramalho, 6, 1495-165, Alges, Portugal
- CCMAR, Universidade do Algarve, Campus de Gambelas, 8005-139, Faro, Portugal
| | - Mélanie Wary
- ICTA, Universitat Autònoma de Barcelona, 08193, Bellaterra, Barcelona, Spain
| | - Syee Weldeab
- University of California Santa Barbara, Santa Barbara, 1006 Webb Hall, CA, 93106-9630, USA
| | - Martin Ziegler
- University of Utrecht, Princetonlaan 8a, 3584 CB, Utrecht, Netherlands
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20
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Palchan D, Torfstein A. A drop in Sahara dust fluxes records the northern limits of the African Humid Period. Nat Commun 2019; 10:3803. [PMID: 31444347 PMCID: PMC6707271 DOI: 10.1038/s41467-019-11701-z] [Citation(s) in RCA: 12] [Impact Index Per Article: 2.4] [Reference Citation Analysis] [Abstract] [Track Full Text] [Download PDF] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 10/09/2018] [Accepted: 07/29/2019] [Indexed: 11/09/2022] Open
Abstract
Northern and eastern Africa were exposed to significantly wetter conditions relative to present during the early Holocene period known as the African Humid Period (AHP), although the latitudinal extent of the northward expansion of the tropical rain belt remains poorly constrained. New records of 230Thxs-normalized accumulation rates in marine sediment cores from the Red Sea and Gulf of Aden are combined with existing records of western Africa dust and terrestrial records across the Sahara Desert, revealing that fluxes of dust transported east from the Sahara decreased by at least 50% during the AHP, due to the development of wetter conditions as far north as ~22°N. These results provide the first quantitative record of sediment and dust accumulation rates in the Red Sea and the Gulf of Aden over the past 20 kyrs and challenge the paradigm of vast vegetative cover across the north and northeastern Sahara Desert during the AHP. Marine sediment cores from east of Africa show that Sahara dust fluxes decreased by at least 50% between the last deglaciation and the mid Holocene, while the Northern Sector of the Red Sea remained unchanged. This constrains the African Humid Period impact to have extended up to ca. 22°N, across a more limited region than previously thought.
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Affiliation(s)
- Daniel Palchan
- The Fredy & Nadine Herrmann Institute of Earth Sciences, The Hebrew University of Jerusalem, The Edmond J. Safra Campus, Givat Ram, Jerusalem, 91904, Israel. .,Interuniversity Institute for Marine Sciences, Eilat, 88103, Israel.
| | - Adi Torfstein
- The Fredy & Nadine Herrmann Institute of Earth Sciences, The Hebrew University of Jerusalem, The Edmond J. Safra Campus, Givat Ram, Jerusalem, 91904, Israel.,Interuniversity Institute for Marine Sciences, Eilat, 88103, Israel
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21
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Abstract
Editorial summaries of selected papers relevant to Quaternary science published in high-impact multidisciplinary journals between December 2018 and February 2019 [...]
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