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Editorial preface to special issue: The Earth System during icehouse Climate Modes: Evidence from glacial records in China Glob. Planet. Change (IF 3.9) Pub Date : 2024-04-10 Xianguo Lang, Bing Shen, Jitao Chen, Matthew Dodd
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An updated chronostratigraphic framework for the Cenozoic sediments of southeast margin of the Tibetan Plateau: Implications for regional tectonics Glob. Planet. Change (IF 3.9) Pub Date : 2024-04-10 Shihu Li, Robert A. Spicer, Tao Su, Zhekun Zhou, Chenglong Deng
As one of the most important accommodation zones during the India-Asia collision, the southeast margin of the Tibetan Plateau (SEMTP) is characterized by many large-scale strike-slip faults, a regional low-relief relict that has been deeply incised by several continental scale rivers that originate from central Tibet, and numerous plant and vertebrate fossil biotas residing in Cenozoic sedimentary
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Cycling of rare earth elements at the Precambrian-Cambrian boundary Glob. Planet. Change (IF 3.9) Pub Date : 2024-04-04 J.G.T. Armstrong, J. Parnell
The Great Unconformity at the Precambrian-Cambrian boundary marks a global erosion surface, and a time gap which in places exceeded a billion years. The weathered sub-Cambrian rocks include abundant granites and pegmatites. These rocks and others were mineralized in several regions. The basal Cambrian sediments show that rare commodities including gold and rare earth elements (REEs) were concentrated
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Soil inorganic carbon stock and its changes across the Tibetan Plateau during the 1980s–2020s Glob. Planet. Change (IF 3.9) Pub Date : 2024-04-04 Honghong Lin, Xingwu Duan, Yifan Dong, Ronghua Zhong, Hua Zheng, Yun Xie, Li Rong, Haijuan Zhao, Shengzhao Wei
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Effects of varied modern pollen-climate calibration-set establishment approaches on quantitative climate reconstructions Glob. Planet. Change (IF 3.9) Pub Date : 2024-03-31 Chen Liang, Yan Zhao, Qiaoyu Cui, Zhuo Zheng, Xiayun Xiao, Chunmei Ma
A representative modern calibration dataset is an essential prerequisite for a reliable quantitative reconstruction of paleoclimate. However, there has been a notable lack of systematic research on the optimal filtering of calibration sets. Four representative high-resolution pollen records were selected to repeatedly reconstruct paleoclimate using multiple approaches such as geographical distance
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Orbital hydroclimate variability revealed by grain-size evidence in the tropical Pacific Islands since 140 ka Glob. Planet. Change (IF 3.9) Pub Date : 2024-03-31 Xiaojie Tang, Zhaojie Yu, Zhengyao Lu, Lina Song, Zehua Song, Christophe Colin, Giuseppe Siani, Xiaoying Kang, Fengming Chang, Franck Bassinot, Shiming Wan
The past evolution of precipitation and atmospheric convection in the Western Pacific Warm Pool (WPWP) is critical for global climate changes but is under debate because of its forcing mechanisms. Here, we present a high temporal resolution (∼156 years) grain-size record of core MD01–2385 over the last 140 kyr, in offshore northern New Guinea to reveal sediment dynamics as a proxy for precipitation
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Pliocene CO2 rise due to sea-level fall as a mechanism for the delayed ice age Glob. Planet. Change (IF 3.9) Pub Date : 2024-03-28 Shiling Yang, Yongda Wang, Xiaofang Huang, Minmin Sun, Jingtai Han, Xu Wang, Zuoling Chen, Shihao Zhang, Wenying Jiang, Zihua Tang, Zhaoyan Gu, Shangfa Xiong, Zhongli Ding
Global sea level fell progressively during the Pliocene in response to the growth of ice sheets at high northern latitudes. However, not until ∼2.7 Ma did the climate system actually generate and maintain major ice sheets in the Northern Hemisphere. A decline in atmospheric CO levels (CO) is thought to be responsible for the Pleistocene ice ages. However, the link between CO and Pliocene glaciations
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Integrating paleolimnological hydrogen and oxygen isotope records during the Holocene on the Tibetan Plateau Glob. Planet. Change (IF 3.9) Pub Date : 2024-03-28 Xiaoxue Gao, Zhe Sun, Xiaohuan Hou, Kejia Ji, Mingda Wang, Juzhi Hou
Stable isotopes are effective proxy indicators for past climate and environment changes. Paleolimnological hydrogen and oxygen isotopes have been used to reconstruct changes in precipitation isotopes and continental climates. However, the stable hydrogen and oxygen isotope records from lakes are rarely compared and integrated directly to study past changes in climate and environment due to their different
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Are longer and more intense heatwaves more prone to extreme precipitation? Glob. Planet. Change (IF 3.9) Pub Date : 2024-03-26 Peng Sun, Yaojin Bian, Shifang Yu, Rui Yao, Zhongtian Wang, Qiang Zhang, Wenhui Chen, Chenhao Ge, Zice Ma, Wenying Du
Simultaneous/sequential occurrence of multiple extreme climate events has the tendency to inflict greater damage compared to isolated extreme climate events. The exploration of simultaneous or continuous extreme events holds profound implications for disaster risk prevention. Therefore, we identified the compound heatwaves and extreme precipitation events (CHP, extreme precipitation events following
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Future projections of compound temperature and precipitation extremes and corresponding population exposure over global land Glob. Planet. Change (IF 3.9) Pub Date : 2024-03-26 Yang Yang, Na Zhao
Extreme climate events are hotspots in global change. However, research on the changes in future compound events and population exposure is still limited. Leveraging from the data of the sixth phase of the Coupled Model Intercomparison Project (CMIP6), this paper aims to analyze the temporal and spatial changes of global compound temperature and precipitation extreme events in the future. We also predict
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Holocene Sea-level impacts on Venice Lagoon's coastal wetlands Glob. Planet. Change (IF 3.9) Pub Date : 2024-03-26 David Kaniewski, Nick Marriner, Matteo Vacchi, Dario Camuffo, Alexandra Bivolaru, Giovanni Sarti, Duccio Bertoni, Luc Diatta, Nirefs Markakis, Amedeo Martella, Thierry Otto, Frédéric Luce, Diego Calaon, Daniela Cottica, Christophe Morhange
Venice Lagoon (Italy), the largest wetland in the Mediterranean basin, is extremely vulnerable to variations in relative sea level (RSL) which is locally defined by an average rising rate of about 2.5mm per year, resulting from both sea-level change and vertical land movements. The environmental pressures stemming from projected higher RSL rising rates will have a profound impact on Venetian coastal
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Differences in soil fungal communities under salinity gradients in arid and semiarid regions Glob. Planet. Change (IF 3.9) Pub Date : 2024-03-22 Yuxi Wei, Lijuan Chen, Zhenliang Yin, Qi Feng, Haiyang Xi, Chengqi Zhang, Kaiyuan Gan, Tian Yong
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Circumpolar Deep Water upwelling is a primary source of 10Be in Antarctic continental shelf sediments Glob. Planet. Change (IF 3.9) Pub Date : 2024-03-21 Matthew R. Jeromson, Toshiyuki Fujioka, David Fink, Krista Simon, James Smith, Claus-Dieter Hillenbrand, Gerhard Kuhn, Alexandra L. Post, Jose Tonatiuh Sánchez-Palacios, Marcello Blaxell, T. Gabriel Enge, Duanne A. White
Beryllium-10 (Be) has been proposed as a potential proxy for investigating ice shelf presence and absence, or meltwater discharge in coastal polar environments. However, the sources and distribution of atmospherically produced meteoric-Be in the Antarctic marine realm are yet to be fully characterized, making any inferences about its concentration in sediments challenging. We present a dataset of Be
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Reconstruction of cropland cover in topographically complex areas: The case of Sichuan Province, China, from 1671 to 2019 Glob. Planet. Change (IF 3.9) Pub Date : 2024-03-21 Fahao Wang, Yu Ye, Xiuqi Fang
Accurately reconstructing cropland cover in topographically complex areas has long been challenging for historical anthropogenic land cover change (ALCC) datasets. Sichuan Province, one of the most topographically complex areas in China, was chosen as a case study. This study integrated historical gazetteers and modern cropland statistics and survey data to examine and correct the prefecture-level
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Increased late Holocene dust activity revealed by loess accumulation rates in Central Asia Glob. Planet. Change (IF 3.9) Pub Date : 2024-03-21 Yijiao Fan, Jia Jia, Junhuai Yang, Lai Zhao, Jianye Li, Jinmeng Tang, Fuyuan Gao, Dunsheng Xia
Dust from the vast arid and semi-arid regions of arid Central Asia (ACA) makes a large contribution to global-scale dust cycles. However, systematic and regional-scale reconstructions of dust activity in ACA are lacking, thus hindering the exploration of its relationship with climate change. Aeolian loess deposits provide valuable records of past dust activity and its linkages to climate. We constructed
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Responses of gross primary productivity in different types of terrestrial ecosystems to interannual variation in the northern boundary of the East Asian summer monsoon Glob. Planet. Change (IF 3.9) Pub Date : 2024-03-16 Zhikai Wang, Wen Chen, Jinling Piao, Shangfeng Chen, Jin-Soo Kim, Lin Wang, Ruowen Yang, Tiantian Yu
The northern boundary of the East Asian summer monsoon (EASMNB), located in the transitional zone from humid to arid regions, is characterized by significant north-south fluctuations. These fluctuations can exert profound impacts on the photosynthetic activity of vegetation by causing anomalous climate conditions, and thus play an important role in the carbon cycle over large parts of northern China
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Anelasticity of the lower mantle inferred from the pole and lunar monthly tides using global DORIS coordinate time series Glob. Planet. Change (IF 3.9) Pub Date : 2024-03-16 Chuanyi Zou, Hao Ding, Wei Luan
Global mantle anelasticity reflects the dissipation mechanism of Earth's interior structure. Nevertheless, there is still an ongoing debate regarding the anelastic properties of the lower mantle (660–2900 km depth). Advancements in data accuracy and record expansion have enabled geodetic technology to offer novel methods for determining the anelastic properties of the lower mantle. This study utilizes
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iLOSCAR: interactive Long-term Ocean-atmosphere-Sediment CArbon cycle Reservoir model v1.0 Glob. Planet. Change (IF 3.9) Pub Date : 2024-03-11 Shihan Li, Richard E. Zeebe, Shuang Zhang
Computationally inexpensive carbon cycle models serve as critical and efficient tools for illuminating the complex dynamics of the carbon cycle and its interplay with the climate system, offering insights into how our planet has responded to climate perturbations throughout its history. During geologic hyperthermal events, carbon cycle models are employed to trace the trajectory of carbon emissions
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Holocene Thermal Maximum paleofloods improve flood frequency analyses in the lower Tennessee River Basin (USA) Glob. Planet. Change (IF 3.9) Pub Date : 2024-03-11 M.A. Lisa Davis, Ray Lombardi, Miles Yaw, Curt Jawdy, Matthew D. Gage
Extreme floods are underrepresented in instrumented flow records. Consequently, flood frequency model estimates of extreme floods contain large uncertainty. The lower Tennessee River (LTR) Basin is located within the southeastern United States and is a large, regulated, and socio-economically significant North American river. The flood-of-record for the LTR occurred in 1867 CE. The 1867 flood-of-record
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Historical catastrophic floods at the southern edge of the Atacama Desert: A multi-archive reconstruction of the Copiapó river extreme events Glob. Planet. Change (IF 3.9) Pub Date : 2024-03-11 Tatiana Izquierdo, Ai-ling Rivera, Ángela Galeano, Diego Gallardo, Verónica Salas, Olga Aparicio, Jan-Pieter Buylaert, Francisco Ruiz, Manuel Abad
The last hydrometeorological extreme event that caused large floods in the southern Atacama Desert in March 2015 raised concern about how little was known about the fluvial dynamic of these arid basins. Understanding the response of intermittent and ephemeral rivers in drylands to the present context of global change is critical to preserve the ecological and human systems they support, to sustainably
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Asynchronous Holocene human population changes in north and south China as related to animal resource utilization Glob. Planet. Change (IF 3.9) Pub Date : 2024-03-08 Yanyan Yu, Jie Yu, Haibin Wu, Feng He, Stephen J. Vavrus, Amber Johnson, Wenchao Zhang, Qin Li, Zhengtang Guo
During the Holocene, rich Neolithic and Bronze cultures developed in the middle and lower reaches of Yellow River valley (north China) and Yangtze River valley (south China), making them the core areas of past human activities. Thus, it is important to reveal the process and driving mechanism of regional population change. Agriculture development has always been taken as the key driver of population
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Low-latitude forcing on 4.2 ka event indicated by records in the Asian monsoon region Glob. Planet. Change (IF 3.9) Pub Date : 2024-03-08 Xin Zhou, Xiaoyan Liu, Tao Zhan, Dorcas B. Oyebanji, Jixiao Zhang, Luyao Tu, Shiwei Jiang
The 4.2 ka event is an important climatic event of the Holocene that is expected to considerably influence the development of human civilizations. However, the forcing mechanism of the 4.2 ka event remains unclear, with current evidence being divided between high-latitude and low-latitude forcings. The Asian climate system contains strong summer and winter monsoon circulations, and thus the region
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Holocene forcing of aeolian dust activity over the Tibetan Plateau and its surroundings Glob. Planet. Change (IF 3.9) Pub Date : 2024-03-08 Junhuai Yang, Haoyu Wang, Fuyuan Gao, Zhenqian Wang, Shuyuan Wang, Yijiao Fan, Tuoyu Li, Xin Liu, Wenxi Qu, Jianye Li, Yixiao Zhang, Zixuan Chen, Li Liu, Ramamoorthy Ayyamperumal, Shengli Yang, Dunsheng Xia
Aeolian deposits on the Tibetan Plateau (TP) and its surroundings provide crucial source materials for the Asian dust cycle, which significantly affects Asian and global ecosystems and climate. However, it is unclear how the dust dynamics of the TP and its surroundings are linked to Earth's climate system. To address this issue, we examined the grain size and accumulation rate of six Holocene aeolian
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The Pacific-North American teleconnection in the Cenozoic Glob. Planet. Change (IF 3.9) Pub Date : 2024-03-08 Zhibo Li, Yongyun Hu, Jian Zhang, Xiang Li, Jiaqi Guo, Jiawenjing Lan, Qifan Lin, Shuai Yuan, Mengyu Wei, Zihan Yin, Qiang Wei, Xiujuan Bao, Jing Han, Jun Yang, Yonggang Liu, Ji Nie
The Pacific-North American teleconnection (PNA) is one of the most important atmospheric modes in the Northern Hemisphere in modern climate. Through the PNA teleconnection, climate variations in the tropical Pacific have significant impacts on North America. However, whether there existed the PNA-like mode in the deep-time climate and how it evolved remain unknown. Here, we study the evolution of the
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Contrasted changes of sea-surface salinity in the southern and northern Okinawa Trough since the mid-Holocene Glob. Planet. Change (IF 3.9) Pub Date : 2024-03-04 Dongling Li, Yanjuan Wu, Marit-Solveig Seidenkrantz, Anne de Vernal, Bangqi Hu, Bing Song, Hui Jiang, Longbin Sha
A reconstruction of sea-surface salinity (SSS) in the southern Okinawa Trough (OT) since 6800 cal. yr BP has been presented in this study. We found that the SSS record increased gradually from the middle to late Holocene, indicating reduced summer precipitation in Taiwan. Our results also suggest regional patterns of SSS with SSS increasing in the southern OT and decreasing in the northern OT since
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Abrupt intensification of AMOC and monsoonal winds during mid-MIS4 (Heinrich Event 6) in the western Arabian Sea Glob. Planet. Change (IF 3.9) Pub Date : 2024-03-04 Hidayatullah Khan, Pawan Govil, Rajani Panchang, Shailesh Agrawal, Pankaj Kumar, Brijesh Kumar, Divya Verma
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Widespread increase in plant transpiration driven by global greening Glob. Planet. Change (IF 3.9) Pub Date : 2024-03-02 Han Chen, Yizhao Wei, Jinhui Jeanne Huang
Global plant transpiration (PT) is a crucial component of the Earth's hydrological cycle and plays a significant role in regulating the exchange of water and energy between the land surface and the atmosphere. However, the long-term trend and the underlying driver of global PT remain unclear due to the significant uncertainties in estimating PT on a global scale. This study uses two sub-Mixture Density
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Surface oceanographic changes from ∼ 25,000 to 3500 cal yr BP in the eastern Arabian Sea Glob. Planet. Change (IF 3.9) Pub Date : 2024-03-01 Jeet Majumder, Anil K. Gupta, Prasanta Sanyal, Pankaj Kumar, Rudra Narayan Mohanty, Rajveer Sharma, Mohan Kuppusamy, Mruganka K. Panigrahi
Multiproxy data of pteropods and planktic foraminifera from Core SK291/GC17 suggest significant surface paleoceanographic shifts from ∼25,000 to 3500 calibrated years before present (cal yr BP) in the eastern Arabian Sea (EAS). Increased values of the global ice-volume free stable oxygen isotope ratio of seawater (δO IVF) and stable oxygen isotope ratio in pteropod (δO IVF), as well as lower percentages
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Evaluating the isotopic composition of leaf organic compounds in fog-dependent Tillandsia landbeckii across the coastal Atacama Desert: Implications for hydroclimate reconstructions at the dry limit Glob. Planet. Change (IF 3.9) Pub Date : 2024-02-28 Andrea Jaeschke, Christoph Böhm, Jan H. Schween, Enno Schefuß, Marcus A. Koch, Claudio Latorre, Sergio Contreras, Janet Rethemeyer, Holger Wissel, Andreas Lücke
Fog is an important component of the coastal climate of northern Chile and southern Peru. Moisture and nutrients from fog maintain highly endemic vegetation (lomas) as well as unique ecosystems that thrive at elevations of ca. 900–1200 m asl. Although this epiphytic CAM bromeliad is well adapted to the extreme climate, declining stocks observed over the past decades question the long-term survival
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Marine redox fluctuations during the Marinoan glaciation Glob. Planet. Change (IF 3.9) Pub Date : 2024-02-27 Zekun Meng, Zhenfei Wang, Pengcheng Ju, Xiqiang Zhou, Chao Li, Zihu Zhang, Xingliang Zhang, Kang-Jun Huang
The proliferation of eukaryotes preceding the Cryogenian Marinoan glaciation (650–635 Ma) and the subsequent radiation of early animals imply a conceivable linkage between global glaciation and complex life evolution. However, the marine redox condition remains enigmatic during the Cryogenian, impeding our understanding of the role of O on this biological innovation. To fill this gap, we comprehensively
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Organic matter imports to the Atacama Desert using polycyclic aromatic hydrocarbons as tracer Glob. Planet. Change (IF 3.9) Pub Date : 2024-02-26 Ramona Mörchen, Humay Rahimova, Barbara Fuentes Siegmund, Franko Arenas Diaz, Bol Roland, Eva Lehndorff
The Atacama Desert, despite its extreme hostile conditions, still harbours traces of life in its dusty surface. Until now, it remains open whether organic molecules found in topsoils have their origin from in-situ biotic processes in the hyper-arid core, or whether and to which degree they stem from outside the desert and its border regions. In order to trace atmospheric organic matter input, we analyzed
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A new algorithm for the energy–water balance model to quantitatively reconstruct Holocene precipitation and vegetation: a case study from Dali Lake, North China Glob. Planet. Change (IF 3.9) Pub Date : 2024-02-24 Yuwen Zhou, Xianyan Wang, Xusheng Li, Yuqiang Zeng, Zhiyong Han
Quantitatively reconstructing precipitation is an important component of paleoclimate research. The mean annual precipitation (MAP) of a closed-basin lake can be estimated by the energy–water balance model (EWBM). The EWBM can be divided into linear and nonlinear models, with determination of evaporation over water and land surface being the main components. However, the influence of vegetation changes
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Quantitative Holocene climate reconstruction and anthropogenic impact analysis based on the pollen records in peat sediment in Southern China Glob. Planet. Change (IF 3.9) Pub Date : 2024-02-24 Lin Zhao, Yaoyao Zeng, Zhiguo Rao, Chao Huang, Yunxia Li, Lidan Liu, Chunmei Ma
The quantitative reconstruction of Holocene paleoclimate is pivotal for unraveling the evolution of East Asian Monsoon (EAM). Some recent studies have highlighted the escalating human activities in the late Holocene, which could potentially pose significant challenges to the precise quantitative reconstruction of paleoclimate. In this study, we undertake a quantitative reconstruction of Holocene climate
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Hydroclimatic changes in eastern China during the Holocene based on pollen data and climate modeling Glob. Planet. Change (IF 3.9) Pub Date : 2024-02-24 Qin Li, Haibin Wu, Jun Cheng, Wenchao Zhang, Yanyan Yu, Aizhi Sun, Yunli Luo
The Asian monsoon system represents one of the world's most dynamic interactions of the cryosphere-continent-ocean-atmosphere system. Understanding and responding to changes in monsoonal precipitation is a major component of environmental management in this region, given its profound influence on socioeconomic activity in monsoonal Asia. In particular, characterizing the spatiotemporal variability
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Unusual weakening trend of the East Asian winter monsoon during MIS 8 revealed by Chinese loess deposits and its implications for ice age dynamics Glob. Planet. Change (IF 3.9) Pub Date : 2024-02-21 Qingzhen Hao, Shuzhen Peng, Xinbo Gao, Slobodan B. Marković, Sheng-Hua Li, Junjie Zhang, Fengjiang Li, Long Han, Yu Fu, Xuechao Wu, Luo Wang, Bing Xu, Yansong Qiao, Jimin Yu, Zhengtang Guo
A fundamental aspect of marine benthic foraminiferal δO records of the last one million years is their “saw-tooth” pattern, characterized by gradual cooling to full glacial conditions followed by very rapid glacial terminations. Understanding the mechanism of this pattern is crucial for understanding ice age dynamics. We investigated the climatic trend within each glacial of the last 880 kyr by comparing
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Orbital-paced silicate weathering intensity and climate evolution across the Eocene-Oligocene transition in the southeastern margin of the Tibetan Plateau Glob. Planet. Change (IF 3.9) Pub Date : 2024-02-17 He Tang, Hao Cui, Shu-Feng Li, Robert A. Spicer, Shi-Hu Li, Tao Su, Zhe-Kun Zhou, Caitlyn R. Witkowski, Vittoria Lauretano, Gang-Jian Wei
The Eocene-Oligocene transition (EOT, ∼33.9 Ma), a period of dramatic global cooling marking the onset of the Antarctic ice sheet. However, paleoclimatic reconstructions indicate a notable spatial heterogeneity in both the marine and terrestrial realms. While limited temporal resolution terrestrial records have hindered the precise understanding of short-term climate events and orbital-scale changes
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Probing the optical and molecular properties of sedimentary dissolved organic matter in the laminated diatom mats from the southern Mariana Trench Glob. Planet. Change (IF 3.9) Pub Date : 2024-02-15 Tingcang Hu, Kexin Zheng, Min Luo, Jingqian Xie, Yulin Qi, Yunping Xu, Duofu Chen
Laminated diatom mats (LDMs) deposition, formed by the aggregation of giant diatoms (e.g., ), are recognized as a crucial driver of the global carbon and silicon cycles due to their substantial contribution to the flux of organic carbon and biogenic silica. The biogenic silica-rich sediment is one of the typical sediment types in the deep-sea setting of the tropical Pacific Ocean. Here, we analyzed
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Impact of Chondrites on trace metal distribution in the sapropel S7 (ODP Site 966): Implications for paleoenvironmental and paleoceanographic reconstructions Glob. Planet. Change (IF 3.9) Pub Date : 2024-02-15 Ricardo D. Monedero-Contreras, Francisco J. Rodríguez-Tovar, Francisca Martínez-Ruiz
Organic-rich deposits are valuable paleo-archives, recording significant paleoceanographic changes linked to past climate variations and marine deoxygenation events. The deposition of organic-rich sediments stops when bottom-water reventilation/oxygenation occurs. This impedes organic matter preservation, enabling macro and micro burrowing-organisms to recover and bioturbate the seafloor. In this sense
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Genetic diversity of the Atacama Desert shrub Huidobria chilensis in the context of geography and climate Glob. Planet. Change (IF 3.9) Pub Date : 2024-02-10 K. Bechir Ferchichi, T. Böhnert, B. Ritter, D. Harpke, A. Stoll, P. Morales, S. Fiedler, F. Mu, J. Bechteler, C. Münker, M.A. Koch, T. Wiehe, D. Quandt
Survival in hyperarid deserts is a major challenge for life in general and for plants in particular. The Atacama Desert presents harsh conditions such as limited rainfall, crusted soils, high soil salinity, high altitude, and intense solar radiation. These conditions, together with paleoclimatic variations over the last 10 million years, have influenced the genetic structure and connectivity of plant
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On the attribution of historical and future dryness/wetness changes in China incorporating surface resistance response to elevated CO2 Glob. Planet. Change (IF 3.9) Pub Date : 2024-02-10 Shanlei Sun, Rongfan Chai, Yifang Zhang, Jia Wang, Zaoying Bi, Jinjian Li, Botao Zhou, Haishan Chen
Considering impacts of elevated CO-induced increases in surface resistance on potential evapotranspiration (PET), to revisit and attribute the changes in dryness/wetness is necessary for accurately understanding evolutions of the historical and future drying and wetting conditions. Therefore, we comprehensively investigated the historical (1965–2011) and future (2019–2098; including four scenarios)
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Sediment provenance changes in the southwestern Okhotsk Sea since MIS 5 and their implications for sediment transport dynamics Glob. Planet. Change (IF 3.9) Pub Date : 2024-02-10 Anqi Wang, Zhengquan Yao, Xuefa Shi, Kunshan Wang, Yanguang Liu, Jianjun Zou, Yuriy Vasilenko, Fengdeng Shi, Zhi Dong, Xiaojing Wang, Aimei Zhu, Zhengfan Lin, Xinqing Zou, Sergey Gorbarenko, Alexander Bosin
The Okhotsk Sea, located between the Asian continent and the western Pacific, is a natural laboratory for investigating sediments source-to-sink influenced by atmosphere–ocean–land–sea ice interactions. However, despite their paleoenvironmental significance, changes in sediment provenance within the Okhotsk Sea are still debated due to the diversity of sediment sources and transport processes. Here
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Asymmetric impacts of El Niño-Southern Oscillation on summer temperature over the eastern Qinghai-Tibetan Plateau, as revealed by the blue intensity of Picea purpurea Glob. Planet. Change (IF 3.9) Pub Date : 2024-02-10 Shuhua Qiao, Yang Deng, Linlin Gao, Yiyun Yuan, Qianling Huang, Xiaohua Gou
The Qinghai-Tibetan Plateau (QTP) is a region exceptionally sensitive to climate change. Warming in the QTP has more than doubled the global average temperature over the past 50 years. Numerous studies have aimed to assess recent warming by reconstructing the past climate of the QTP through tree-ring analysis. However, these studies primarily utilize ring width as the parameter. Our study marks the
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Indian summer monsoon drives synchronous interdecadal hydroclimate changes in the Tibetan Plateau and surroundings Glob. Planet. Change (IF 3.9) Pub Date : 2024-02-10 Keyan Fang, Zepeng Mei, Hao Wu, Feifei Zhou, Heikki Seppä, Zhengtang Guo
The interdecadal relationship (10–100 years) between the Indian Summer Monsoon (ISM) and arid climate is pivotal in comprehending Asian hydroclimate dynamics. Despite extensive tree-ring based climate reconstructions conducted across both monsoonal and arid regions in the Tibetan Plateau (TP) and surroundings, the correlation between the ISM and arid climate on interdecadal scales remains contentious
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Temperature variability revealed by lacustrine brGDGTs in northeastern China since the Last Glacial Maximum Glob. Planet. Change (IF 3.9) Pub Date : 2024-02-10 Chengcheng Leng, Qiaoyu Cui, Yan Zhao, Can Zhang, Xiaoshuang Sun, Tianlong Yan, Cheng Zhao
Reconstructing temperature and monsoon variability are important for comprehensive understanding of past climate changes in the Asian summer monsoon (ASM) region. Although changes in monsoon intensity and monsoon rainfall since the Last Glacial Maximum (LGM) have been extensively studied from various archives and proxies, the variability of terrestrial temperature changes in the ASM region is still
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Microbial hotspots in a relict fog-dependent Tillandsia landbeckii dune from the coastal Atacama Desert Glob. Planet. Change (IF 3.9) Pub Date : 2024-02-09 Andrea Jaeschke, S. Matthias May, Anna Hakobyan, Ramona Mörchen, Olaf Bubenzer, Stefano M. Bernasconi, Enno Schefuß, Dirk Hoffmeister, Claudio Latorre, Martina Gwozdz, Janet Rethemeyer, Claudia Knief
The hyperarid Atacama Desert in northern Chile is considered to be one of the most hostile habitats for microbial life. Despite the extreme environmental conditions, isolated patches of vegetation exist in an otherwise barren landscape. Unique dune ecosystems dominated by rootless vegetation occur at elevations of about 900–1200 m asl within the coastal mountain range and receive water and nutrients
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Sixteen mass extinctions of the past 541 My correlated with 15 pulses of Large Igneous Province (LIP) volcanism and the 4 largest extraterrestrial impacts Glob. Planet. Change (IF 3.9) Pub Date : 2024-02-08 Michael R. Rampino, Ken Caldeira, Sedelia Rodriguez
We find that Large Igneous Province (LIP) volcanism, mostly continental flood basalts (CFBs), along with the largest extraterrestrial impacts show significant correlations with mass-extinction events in the Phanerozoic geologic record. The ages of the 6 major marine mass extinctions (≥ 40% extinction of genera) of the last 541 My–the end-Ordovician (∼444 Ma), late Devonian (∼372 Ma), end-Guadalupian
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Analytical computation of local gravitational effects of mountain glacier mass change from polyhedral and prismatic modeling - test case Vernagtferner, Austrian Alps Glob. Planet. Change (IF 3.9) Pub Date : 2024-02-06 Georgia Gavriilidou, Christian Gerlach, Dimitrios Tsoulis
Gravimetric measurements allow monitoring mass transport in the Earth system and one example is temporal variations in the global water cycle including the cryosphere. Coupling gravity observations to the underlying processes requires modeling of the relevant mass elements. When observing the gravity field from space (i.e., by satellites), point mass models or simple spherical surface layers (mascons)
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Drought determines the growth stability of different dominant conifer species in Central Asia Glob. Planet. Change (IF 3.9) Pub Date : 2024-02-03 Dashi Du, Liang Jiao, Xuan Wu, Ruhong Xue, Mengyuan Wei, Peng Zhang, Qian Li, Xuge Wang
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Interannual variations in stable isotopes of atmospheric water in arid Central Asia due to changes in atmospheric circulation Glob. Planet. Change (IF 3.9) Pub Date : 2024-02-01 Shengjie Wang, Gahong Yang, John Bershaw, Xiaokang Liu, Kei Yoshimura, Yanqiong Xiao, Mingjun Zhang
The oxygen isotope compositions in atmospheric water including water vapor and precipitation have been widely used to trace moisture sources and to reconstruct past climates. However, the environmental controls of stable isotopes in atmospheric water depend on the time scales. Because of limited observations in arid Central Asia, factors controlling interannual variations in atmospheric water isotopes
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Latest Permian and earliest Triassic geomagnetic polarity timescale: A polarity reversal marks the greatest mass extinction Glob. Planet. Change (IF 3.9) Pub Date : 2024-01-28 Yan Chen, Haishui Jiang, James G. Ogg, Paul B. Wignall, Xulong Lai
The establishment of the latest Permian geomagnetic polarity time scale has been inhibited by the inconsistent polarity patterns published by different teams for the section at Meishan, which hosts the Global Boundary Stratotype Section and Points (GSSPs) for the Permian-Triassic boundary (PTB) and base of the underlying Changhsingian Stage. We have analyzed the magnetostratigraphy of the Shangsi section
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Depositional and circulation changes at the Chukchi margin, Arctic Ocean, during the last two glacial cycles Glob. Planet. Change (IF 3.9) Pub Date : 2024-01-18 Wenshen Xiao, Leonid Polyak, Taoliang Zhang, Rujian Wang, Xiao Duan, Yan Tu, Yangqing Hu, Yanyan Pan
The shallow Chukchi-East Siberian margin of the Arctic Ocean was repeatedly impacted by Pleistocene glaciations and related changes in sea level and circulation. The depositional history across the last two Arctic glacial cycles is investigated in sediment core ARC6-C15 from the foot of the Chukchi Rise, an extension of the Chukchi Sea shelf that was impacted by the East Siberian Ice Sheet (ESIS).
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Integrated cyclostratigraphy of the Cau core (SE Spain) - A timescale for climate change during the early Aptian Anoxic Event (OAE 1a) and the late Aptian Glob. Planet. Change (IF 3.9) Pub Date : 2024-01-16 Rafael Martínez-Rodríguez, Sietske J. Batenburg, José M. Castro, Ginés A. de Gea, Luis M. Nieto, Pedro A. Ruiz-Ortiz, Stuart Robinson
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Oxygen increase and the pacing of early animal evolution Glob. Planet. Change (IF 3.9) Pub Date : 2024-01-14 Kunio Kaiho, Atena Shizuya, Minori Kikuchi, Tsuyoshi Komiya, Zhong-Qiang Chen, Jinnan Tong, Li Tian, Paul Gorjan, Satoshi Takahashi, Aymon Baud, Stephen E. Grasby, Ryosuke Saito, Matthew R. Saltzman
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Terrestrial and marine dynamics on the brink of the Messinian salinity crisis: A wet scenario from the northern Mediterranean Glob. Planet. Change (IF 3.9) Pub Date : 2024-01-18 Adele Bertini, Gabriele Niccolini, Rocco Gennari, Francesca Lozar, Elena Menichetti, Marcello Natalicchio, Francesco Dela Pierre
The ongoing debate on the causes and modalities of the Messinian Salinity Crisis (MSC) from 5.971 Ma needs to be implemented by an in-depth knowledge of the events and changes, on a global to regional scale, that have preceded its onset. Here we use palynological (pollen and dinocysts) and micropaleontological (foraminifers and calcareous nannoplankton) quantitative analyses from the Govone sedimentary
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Enhanced primary productivity and perturbation of marine nitrogen cycling during the onset of the Cambrian SPICE event Glob. Planet. Change (IF 3.9) Pub Date : 2024-01-15 Gwen L. Barnes, Bradley D. Cramer
New high-resolution paired carbonate carbon (δ13Ccarb) and nitrogen (δ15Nbulk) isotope records of the Steptoean Positive Carbon Isotope Excursion (SPICE) from the Laurentian epicontinental platform reveal a transient negative excursion in δ15Nbulk that closely aligns with the onset of the SPICE event and the initiation of the positive δ13Ccarb excursion. The negative excursion in δ15Nbulk identified
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One catastrophic flood every millennium: Synchronicity of extreme floods and global warm periods in the multi-archive record of the Roman theatre of Guadix (Granada, SE Spain) Glob. Planet. Change (IF 3.9) Pub Date : 2024-01-14 A. Díez-Herrero, R.M. Mateos, D. Vázquez-Tarrío, A. López-Marcos, F.J. Brao-González
Past global changes are typically registered in both natural (e.g., geologic-geomorphological, atmospheric-climatic, hydrologic-glacial and biological) and cultural records (e.g., archaeological, historical and documentary sources). Nevertheless, there are few sites in the world where sedimentary and archaeological evidence combine to provide information about two or more past millennial climate changes
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Absolute age and temperature of belemnite rostra: Constraints on the Early Cretaceous cooling event Glob. Planet. Change (IF 3.9) Pub Date : 2024-01-14 Tianyang Wang, Peng Yang, Songlin He, René Hoffmann, Qinghai Zhang, Alex Farnsworth, Yue-xing Feng, Hasina Nirina Randrianaly, Jing Xie, Yahui Yue, Jian-xin Zhao, Lin Ding
Assessing the climatic perturbations during the Cretaceous when atmospheric CO2 levels were high is critical for understanding the nature of environmental responses to greenhouse forcing in the past and future. Paleoclimate reconstructions utilizing various geochemical proxies have revealed a disturbed interval during the Late Jurassic–Cretaceous period. This interval comprised multiple instances of
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The dynamic ocean redox evolution during the late Cambrian SPICE: Evidence from the I/Ca proxy Glob. Planet. Change (IF 3.9) Pub Date : 2024-01-08 Ruliang He, Alexandre Pohl, Ashley Prow, Ganqing Jiang, Chin Chai Huan, Matthew R. Saltzman, Zunli Lu
The late Cambrian Steptoean positive carbon isotope excursion (SPICE) is a distinct chemostratigraphic feature of the Paleozoic, marked by a 4–5‰ shift in carbonate δ13C that has been recognized across the globe during the Paibian Stage. The SPICE may be related to enhanced burial of organic matter and pyrite during the expansion of marine euxinia, which as a source of O2 also results in a pulse of
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