Global and Planetary Change最新文献

{"title":"Evaluating hydroclimatic persistence signals in Antarctic snowfall accumulation and sea salt sodium records","authors":"Matthew S. Armstrong,Anthony S. Kiem,George Kuczera,Tessa R. Vance","doi":"10.1016/j.gloplacha.2026.105747","DOIUrl":"https://doi.org/10.1016/j.gloplacha.2026.105747","url":null,"abstract":"","PeriodicalId":55089,"journal":{"name":"Global and Planetary Change","volume":"167 1","pages":"105747"},"PeriodicalIF":3.9,"publicationDate":"2026-10-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"149091368","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":1,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

{"title":"Two-epoch (2003–2023) assessment of the Antarctic ice sheet elevation and mass change using SARAL/AltiKa Ka-band radar and ICESat laser altimetry","authors":"Purvee Joshi,Priyanka Patel,Naveen Tripathi,Sushil Kumar Singh,Ritesh Agrawal,Yogesh Ray,Sandip R. Oza,Rashmi Sharma","doi":"10.1016/j.gloplacha.2026.105762","DOIUrl":"https://doi.org/10.1016/j.gloplacha.2026.105762","url":null,"abstract":"","PeriodicalId":55089,"journal":{"name":"Global and Planetary Change","volume":"17 1","pages":"105762"},"PeriodicalIF":3.9,"publicationDate":"2026-10-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"149209738","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":1,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

{"title":"From slab to surface response: Spatial variability of exhumation and uplift in the Calabrian Arc","authors":"Nicolas Villamizar-Escalante,Christoph von Hagke,Thomas Pollhammer,Fabian Dremel,Moritz Liebl,Bernhard Salcher,Jörg Robl,Bjarne Friedrichs,Marco Meschis","doi":"10.1016/j.gloplacha.2026.105748","DOIUrl":"https://doi.org/10.1016/j.gloplacha.2026.105748","url":null,"abstract":"","PeriodicalId":55089,"journal":{"name":"Global and Planetary Change","volume":"147 1","pages":"105748"},"PeriodicalIF":3.9,"publicationDate":"2026-10-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"149091366","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":1,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

{"title":"High-resolution temperature and precipitation variations in Southwest China over the past 2000 years modulated by differential time-varying forcings","authors":"Rui Ke,Xiayun Xiao,Yan Zhao,Chunmei Ma,Jun Cheng,Zhuo Zheng,Xiaojian Zhang,Changting Chi,Baoyan Jia,Weiru Tu","doi":"10.1016/j.gloplacha.2026.105775","DOIUrl":"https://doi.org/10.1016/j.gloplacha.2026.105775","url":null,"abstract":"","PeriodicalId":55089,"journal":{"name":"Global and Planetary Change","volume":"37 1","pages":"105775"},"PeriodicalIF":3.9,"publicationDate":"2026-10-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"149209739","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":1,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

{"title":"Foraminiferal Nd isotope evidence for Burdigalian–Langhian water mass reorganization in the Adana and Adıyaman basins, Eastern Mediterranean (Türkiye)","authors":"Halvard Caux,Filip Scheiner,Lukáš Ackerman,Atike Nazik,Katarína Holcová","doi":"10.1016/j.gloplacha.2026.105763","DOIUrl":"https://doi.org/10.1016/j.gloplacha.2026.105763","url":null,"abstract":"","PeriodicalId":55089,"journal":{"name":"Global and Planetary Change","volume":"32 1","pages":"105763"},"PeriodicalIF":3.9,"publicationDate":"2026-10-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"149209740","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":1,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

{"title":"Corrigendum to “Discriminating biogenic and authigenic apatite in deep-sea sediments: Insights into phosphorus burial heterogeneity” [Glob. Planet. Change 263 (2026) 105513]","authors":"Xuran Liang,Yi-Gang Xu,Zongqi Zou,Qiong Wu,Xiaolong Ma,Shengxiong Yang,Shengping Qian","doi":"10.1016/j.gloplacha.2026.105731","DOIUrl":"https://doi.org/10.1016/j.gloplacha.2026.105731","url":null,"abstract":"","PeriodicalId":55089,"journal":{"name":"Global and Planetary Change","volume":"170 1","pages":"105731"},"PeriodicalIF":3.9,"publicationDate":"2026-09-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"149049263","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":1,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

{"title":"Corrigendum to “Millennial cold-dry events during marine isotope stage 11a based on sedimentary records from the Heqing Basin and their global climatic dynamical responses” [Glob. Planet. Chang. 265 (2026) 105634]","authors":"Guohui Liu,Xinwen Xu,Shenghui Wang,Lirong Hou,Yuqing Zhang,Liu Yang,Jingfang Zhang,Yuzhu Zhang,Hui Zhao,Chaofeng Fu,Xiaoke Qiang,Wen Liu,Yi He","doi":"10.1016/j.gloplacha.2026.105724","DOIUrl":"https://doi.org/10.1016/j.gloplacha.2026.105724","url":null,"abstract":"","PeriodicalId":55089,"journal":{"name":"Global and Planetary Change","volume":"3 1","pages":"105724"},"PeriodicalIF":3.9,"publicationDate":"2026-09-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"149021524","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":1,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

{"title":"Persistence and resilience on Mount Etna's active flank: An integrated geological and archaeological perspective","authors":"Carla Bottari ,&nbsp;Alessandro Luppino ,&nbsp;Salvatore Claudio Alparone ,&nbsp;Francesca Forni ,&nbsp;Gianluca Groppelli ,&nbsp;Mimmo Palano ,&nbsp;Francesco Sortino ,&nbsp;Salvatore Giammanco","doi":"10.1016/j.gloplacha.2026.105327","DOIUrl":"10.1016/j.gloplacha.2026.105327","url":null,"abstract":"<div><div>Volcanic environments illustrate how human communities have learned to persist within dynamic, hazardous landscapes by balancing risk and opportunity. Mount Etna (Sicily, Italy) – one of the world's most active volcanoes – provides an outstanding natural laboratory to investigate the interplay between geodynamic and volcanic processes as well as human adaptation. The site of Santa Venera al Pozzo (SVP) exemplifies this duality: archaeological and geological evidence reveal a persistent human presence since the Late Neolithic, sustained by fault-controlled hydrothermal discharge and a geomorphological position that ensured long-term stability outside major lava flow pathways.</div><div>This study integrates geological, geochemical, geodetic, seismological, and archaeological data to examine how tectonic and magmatic processes sustained hydrothermal activity and supported enduring settlement. Results indicate that (i) deformation was largely accommodated by creeping faults, in turn enhancing permeability and maintaining spring discharge; (ii) the site's distal position from eruptive rift zones provided geomorphological stability; and (iii) cultural practices promoted the adaptive reuse of geothermal resources over the time.</div><div>The case of SVP demonstrates that the same Earth processes generating hazards also maintain vital resources, enabling long-term human resilience. This integrated geological–archaeological perspective provides a transferable framework for understanding sustainability and risk in volcanically active regions worldwide.</div></div>","PeriodicalId":55089,"journal":{"name":"Global and Planetary Change","volume":"259 ","pages":"Article 105327"},"PeriodicalIF":4.0,"publicationDate":"2026-04-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"146048396","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":1,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

{"title":"Holocene relative sea-level changes from the Atlantic coasts of South America","authors":"K. Rubio-Sandoval ,&nbsp;T.A. Shaw ,&nbsp;M. Vacchi ,&nbsp;N. Khan ,&nbsp;B.P. Horton ,&nbsp;J.R. Angulo ,&nbsp;M. Pappalardo ,&nbsp;A.L. Ferreira-Júnior ,&nbsp;S. Richiano ,&nbsp;M.C. de Souza ,&nbsp;P.C. Giannini ,&nbsp;D.D. Ryan ,&nbsp;E.J. Gowan ,&nbsp;A. Rovere","doi":"10.1016/j.gloplacha.2026.105315","DOIUrl":"10.1016/j.gloplacha.2026.105315","url":null,"abstract":"<div><div>Holocene relative sea-level (RSL) changes along the Atlantic coast of South America reflect a complex interplay between ice equivalent sea-level, glacio-isostatic adjustment (GIA), regional tectonics, and local sedimentary processes. However, the uneven spatial and temporal resolution of existing Holocene RSL data has hindered regional assessments. Here, we compile and standardize 1108 RSL data points from Brazil, Uruguay, Argentina, and Chilean Tierra del Fuego, creating the first comprehensive database for the southwestern Atlantic. The data reveals a widespread Mid-Holocene highstand between 7000 and 4000 years BP, with RSL rising 2 to 4 m above present-day sea level, followed by a gradual fall to present. This pattern is consistent with GIA model predictions across the region's &gt; 50° latitudinal span. Peak rates of RSL change occurred during the Early to Mid-Holocene transition, reaching up to 17.2 mm/yr in Tierra del Fuego and decreasing to 1.6 mm/yr near the Amazon delta. After 5000 years cal BP, RSL started to fall at 0.5 mm/yr. This Atlantic coast of South America database fills a critical geographic gap and provides a robust framework for refining GIA models and understanding sea-level evolution during the Holocene in the Southern Hemisphere.</div></div>","PeriodicalId":55089,"journal":{"name":"Global and Planetary Change","volume":"259 ","pages":"Article 105315"},"PeriodicalIF":4.0,"publicationDate":"2026-04-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"145995747","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":1,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

{"title":"Late Cenozoic transtensional deformation along the Chenghai fault zone and its constraint on micro-block clockwise rotation in the southeastern Tibetan Plateau","authors":"Xiaolong Huang ,&nbsp;Zhichao Li ,&nbsp;Zhonghai Wu ,&nbsp;Xiaojin Huang ,&nbsp;Kungang Wu ,&nbsp;Feipeng Huang","doi":"10.1016/j.gloplacha.2026.105320","DOIUrl":"10.1016/j.gloplacha.2026.105320","url":null,"abstract":"<div><div>The Chenghai fault zone is a crucial component of the Dali fault system, essential for understanding Cenozoic crustal deformation along the southeastern Tibetan Plateau. This study involved detailed remote sensing and field mapping to examine the geometry and kinematics of the fault zone, with the purpose of analyzing the late Cenozoic deformation in the study area. Findings reveal that the Chenghai fault zone extends for 200 km from Jinguan to the southern end of the eastern Midu Basin, where it intersects and follows the trace of the Red River Fault. The Chenghai fault zone has left-lateral, normal-slip kinematics, with the normal-slip component being pronounced along most fault segments. The transtensional slip likely began in the early Pliocene (ca. 7 Ma) based on the analysis of thermochronology data and the sedimentary age of the Sanying Formation. The maximum dip- and left-slip rates are about 0.2–0.3 mm/yr and 0.8–0.9 mm/yr, respectively, since. ca. 7 Ma. Through the analysis of the geometry, kinematics, and seismic activity of the Chenghai fault zone, the study concludes that the Chenghai fault zone exhibits significant rotation, which can be attributed to the clockwise rotation of the Dali fault system. Combined geodetic velocity profiles, we infer that the deformation of the Dali fault system is primarily influenced by the non-uniform rotation of the southeastern Tibetan Plateau. To the west of the Dali fault system, clockwise rotation remains uninterrupted, whereas to the east, material extrusion between the Dali fault system and the Xianshuihe-Xiajiang fault zone is inhibited by the Red River fault zone. The left-lateral motion along the Chenghai fault zone is predominantly governed by clockwise rotation, while the normal faulting is chiefly controlled by differential rotation. Consequently, we infer that the Dali rift system is a manifestation of differential rotation along the southeastern margin of the Tibetan Plateau. By comparing it with the Pamir Plateau and the Aegean Sea region, we propose that pre-existing structures and block rotation are crucial mechanisms driving lateral deformation in the peripheral zones of continent-continent collision orogens.</div></div>","PeriodicalId":55089,"journal":{"name":"Global and Planetary Change","volume":"259 ","pages":"Article 105320"},"PeriodicalIF":4.0,"publicationDate":"2026-04-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"146015048","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":1,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}