Quaternary Science Reviews最新文献

{"title":"A review on Pyrenean Pleistocene leopards paleoecology, paleobiogeography and adaptative convergences with snow leopards","authors":"Maria Prat-Vericat ,&nbsp;Adrian Marciszak ,&nbsp;Saverio Bartolini-Lucenti ,&nbsp;Darío Fidalgo ,&nbsp;Isaac Rufí ,&nbsp;Clàudia Tura-Poch ,&nbsp;Víctor Vizcaíno-Varo ,&nbsp;Silvia Jovells-Vaqué ,&nbsp;Nil Ramada ,&nbsp;Celia Díez-Canseco ,&nbsp;Pere Gelabert ,&nbsp;Carles Tornero ,&nbsp;Xavier Terradas ,&nbsp;Lorenzo Rook ,&nbsp;Joan Madurell-Malapeira","doi":"10.1016/j.quascirev.2025.109327","DOIUrl":"10.1016/j.quascirev.2025.109327","url":null,"abstract":"<div><div>—In this study, we review and analyze one of the most scarcely recorded carnivorans of the European Quaternary, the leopard (<em>Panthera pardus</em>), focusing on its presence in the Pyrenean Mountain range. Our data reveal a progressive increase in both the number of records and the body mass of leopards throughout the Pleistocene, beginning with the earliest specimens from the Early Pleistocene. Our analysis also demonstrated reduced sexual dimorphism compared to modern leopards, as well as a preference for mountain environments. Additionally, we identified several cranial and post-cranial anatomical convergences with snow leopards, which were also sporadically recorded in Europe. These convergences, discussed in detail, may be the result of interspecific competition, environmental pressures, or habitat preferences.</div></div>","PeriodicalId":20926,"journal":{"name":"Quaternary Science Reviews","volume":"358 ","pages":"Article 109327"},"PeriodicalIF":3.2,"publicationDate":"2025-04-15","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"143833400","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":"Retreat of the Boothia-Lancaster ice stream from its Last Glacial Maximum extent and its role in the origin of Baffin Bay Detrital Carbonate (BBDC) events 0, 1 and 2","authors":"Anne Jennings ,&nbsp;Kimberley Jenner ,&nbsp;Alexandre Normandeau ,&nbsp;Wendy Roth ,&nbsp;John Andrews ,&nbsp;Robert Kelleher ,&nbsp;Juliette Girard ,&nbsp;Brendan Reilly ,&nbsp;Calvin Campbell ,&nbsp;Robbie Bennett","doi":"10.1016/j.quascirev.2025.109353","DOIUrl":"10.1016/j.quascirev.2025.109353","url":null,"abstract":"<div><div>We combine geomorphological and sediment core evidence to investigate phases of ice margin stability and instability during retreat of the Boothia Lancaster Ice Stream (BLIS) of the NE Laurentide Ice Sheet (LIS) since the Last Glacial Maximum (LGM). Sediment cores 2008029-059 PC and TWC (59CC) and 2013029-064 PC (64 PC) from Lancaster Sound and Baffin Bay, respectively, represent LGM through Holocene environments, including three Baffin Bay Detrital Carbonate (BBDC) events that have been thought to manifest calving events within Lancaster Sound. Previous mapping of glacigenic landforms shows that 64 PC lies within the LGM limit of the convergent BLIS and Tasiujaq Ice Stream (TIS) on the northeastern Baffin Island shelf, while 59CC terminates within subglacial/ice marginal sediments termed the Baffin Shelf Drift (BSD), capturing the history of BLIS retreat from 15.3 cal ka BP onward. In 64 PC, a basal sediment gravity flow deposit is overlain by dolomite-rich BBDC 2, which is re-interpreted here as a subglacial/ice marginal deposit and renamed GZ-BBDC. Both gravity flows are interpreted to have formed during retreat of the confluent TIS and BLIS from the LGM maximum extent. Overlying GZ-BBDC, in 64 PC, is a finely laminated lithofacies interpreted as an ice-shelf facies formed beneath the ice shelf fronting the confluent TIS and BLIS when it occupied a large LGM grounding zone wedge (GZW) in northern Baffin Bay. The ice-shelf facies indicates temporary stabilization of the conjoined TIS and BLIS. The overlying thin black glaciomarine diamicton records disintegration of the ice shelf and retreat of the TIS. Ice retreat over Cretaceous and younger bedrock into Lancaster Sound is recorded by dark brown diamicton and glaciomarine sediments in 59CC. The overlying tan, detrital carbonate-rich glaciomarine diamicton, BBDC 1 in 59 PC, manifests calving retreat of the BLIS onto the Paleozoic carbonate bedrock within Lancaster Sound by 15 cal ka BP. A slightly later onset of BBDC 1 in 64 PC, of ca.14.5 cal ka BP, points to the influence of local conditions such as sea ice and local iceberg calving on the distribution of IRD off of Pond Inlet. The pause in ice rafting and detrital carbonate deposition between BBDC 1 and BBDC 0 within the Younger Dryas chron likely results from BLIS readvance to Devon Island and its stabilization there until 11.6 cal ka BP. BLIS retreat into Prince Regent Inlet marks the onset of BBDC 0. These new results indicate multiple periods of instability of the BLIS, which are responsible for BBDC events identified throughout Baffin Bay.</div></div>","PeriodicalId":20926,"journal":{"name":"Quaternary Science Reviews","volume":"358 ","pages":""},"PeriodicalIF":3.2,"publicationDate":"2025-04-13","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"143825010","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":"The potential use of the Argentine Continental Shelf during the human colonization of southern South America. Paleogeographic models and archaeological expectations","authors":"A.F.J. Zangrando ,&nbsp;J.F. Ponce","doi":"10.1016/j.quascirev.2025.109331","DOIUrl":"10.1016/j.quascirev.2025.109331","url":null,"abstract":"<div><div>The analysis of human colonization of the southern tip of South America involves exploring diverse environmental and ecological changes, in addition to the important geographic transformations due to the retreat of ice fields and marine transgression during the late Pleistocene. In this paper, we examine the process of human colonization in southern Patagonia (south of parallel 47°) between 15,000 and 10,000 cal yr BP by means of the following procedure. First, we performed a detailed bathymetric analysis and generated a series of palaeogeographic models using a Geographic Information System (GIS) and Digital Elevation Models (DEM). Secondly, based on the palaeogeographic reconstructions and available archaeological evidence, we examined hypothetical dispersal pathways in the region using GIS-generated Least Cost Path Analysis simulation models with special emphasis on sea level changes and physical spatial conditions. The results suggest that the Argentine Continental Shelf (ACS) may have played an important role in the early dispersal of hunter-gatherers in southern Patagonia, either by presenting lower impediments or costs for human mobility, possible ecological niches without analogues in other sectors of Patagonia, and favorable environmental conditions for human habitation. This expectation is also integrated within an existing framework of discussion about a geographically discontinuous distribution of human occupations recorded in the plateau sector of the region during the Pleistocene-Holocene transition, which possibly interacted with denser population nodes in the continental shelf sector.</div></div>","PeriodicalId":20926,"journal":{"name":"Quaternary Science Reviews","volume":"358 ","pages":"Article 109331"},"PeriodicalIF":3.2,"publicationDate":"2025-04-12","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"143823198","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":"Sensitivity to climate and vegetation dynamics of a peatland record from central Cameroon during the African Humid Period","authors":"Valentine Schaaff ,&nbsp;Vincent Grossi ,&nbsp;Matthew Makou ,&nbsp;Yannick Garcin ,&nbsp;Pierre Deschamps ,&nbsp;Bruno Hamelin ,&nbsp;Christopher A. Kiahtipes ,&nbsp;David Sebag ,&nbsp;Benjamin Ngounou Ngatcha ,&nbsp;Guillemette Ménot","doi":"10.1016/j.quascirev.2025.109307","DOIUrl":"10.1016/j.quascirev.2025.109307","url":null,"abstract":"<div><div>Significant climatic and vegetation changes have occurred in tropical Africa over the Holocene, especially during the African Humid Period (AHP). However, the complexity of interpreting and comparing several proxies from diverse sites complicates the characterization and differentiation of climatic and environmental changes at local, regional and global scales. This study investigates a 6-m peat core from the Ngaoundaba maar volcanic crater (Northeastern Cameroon, later simply called Ngaoundaba), spanning the last 10 ka using pollen analysis and a large panel of lipid biomarkers. We produce new high-resolution, continuous, multiproxy records of vegetation, temperature, and precipitation spanning most of the Holocene. All of these proxies indicate a substantial transition approximately 5.7–5.6 ka cal BP, which is supported by cluster analyses and marks the end of the AHP. A shift from an open-water to a vegetated peatland, the disappearance of some wooded species, and the expansion of grass and sedge pollen all indicate significant local and regional changes. The gradual terrestrialization of peat surfaces also had an impact on lipid biomarker proxies. An unusual extensive variation in hydrogen isotopic composition (D/H) of long-chain <em>n</em>-alkanes during the Holocene, in contrast to other records from West and Central Africa, may be attributed to the increased contribution from local wetland plants, including sedges and grasses, which thrive in peat water that is more D-enriched than rainwater, peat water being the water accumulating in the wetland. Likewise, temperature variations reconstructed using bacterial branched glycerol dialkyl glycerol tetraethers (brGDGTs) are influenced by confounding factors, like changes in peat pH or moisture levels, which may be constrained using our multiproxy methodology. The temperature record from Ngaoundaba indicates a slight increase in temperature during the mid-Holocene relative to pre-industrial levels. The Ngaoundaba peat deposit documents a massive and abrupt shift in vegetation at the end of the AHP, linked with changes in precipitation amount and/or seasonality, which also significantly affected the peat microbial community. The Ngaoundaba peat record, because of its high sensitivity to climatic and environmental changes, is a crucial new source for understanding the end of the African Humid Period in Western Central Africa.</div></div>","PeriodicalId":20926,"journal":{"name":"Quaternary Science Reviews","volume":"358 ","pages":"Article 109307"},"PeriodicalIF":3.2,"publicationDate":"2025-04-11","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"143816869","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 ‘The change in convection over the Indo-Pacific warm pool in the mid-Holocene and its influence on South Asian precipitation’ [Quat. Sci. Rev. 322 (2023) 108399]","authors":"Xinquan Zhou ,&nbsp;Xiaobo Jin ,&nbsp;Xiaoxu Shi ,&nbsp;Chuanlian Liu","doi":"10.1016/j.quascirev.2025.109352","DOIUrl":"10.1016/j.quascirev.2025.109352","url":null,"abstract":"","PeriodicalId":20926,"journal":{"name":"Quaternary Science Reviews","volume":"358 ","pages":"Article 109352"},"PeriodicalIF":3.2,"publicationDate":"2025-04-10","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"143807451","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":"Isotopes in Palaeoenvironmental Research – A 20 year update","authors":"Melanie J. Leng","doi":"10.1016/j.quascirev.2025.109322","DOIUrl":"10.1016/j.quascirev.2025.109322","url":null,"abstract":"<div><div>This special issue of Quaternary Science Reviews comprises a series of review papers which discuss the application of stable isotopes to different types of Quaternary records. This is an update of the 2004 special issue of Quaternary Science Reviews on “Isotopes in Quaternary Paleoenvironmental Reconstruction (ISOPAL)”, volume 23, issue 7–8, pages 739–992. The last 2 decades have seen huge advances in methods and interpretation of the common stable isotopes in air, liquid and solid materials but there have also been advancements in the so-called rarer isotopes in difficult matrices. The volume will include updates and reviews on recent advances in some of the potentially faster moving disciplines which include isotopes in: the anthropocene, bones and teeth, chironomid head capsules, as well as isotopes in coastal (organic matter) and marine (benthic foraminifera) sediments. Updates on silicon isotopes and isotopes in biomarkers (focussing in on peatlands) are discussed and there is also a review on how isotopes are used in sclerochronology.</div></div>","PeriodicalId":20926,"journal":{"name":"Quaternary Science Reviews","volume":"357 ","pages":""},"PeriodicalIF":3.2,"publicationDate":"2025-04-09","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"143807027","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":"Evaluating adaptability of early cereal consumption during Holocene climate fluctuation: Integrated insights from macro-botanical remains, fossil pollen records and species distribution modeling in northern China","authors":"Yumeng Qu","doi":"10.1016/j.quascirev.2025.109350","DOIUrl":"10.1016/j.quascirev.2025.109350","url":null,"abstract":"<div><div>Agricultural production began with the selective adaptation of wild crops. While extensive archaeological evidence indicates that northern China was one of the earliest regions to develop systematic cereal cultivation, the dynamics of early subsistence adaptation remain insufficiently understood, primarily due to limited knowledge regarding the distribution, abundance, and variation of cereals. This study integrates multiple lines of evidence, including macro-botanical data recovered from archaeological sites, pollen taxa analysis from high-resolution sediment samples, and species distribution modeling (SDM), to evaluate the interaction between wild cereal resources and human choices during Holocene climate fluctuations. The findings suggest that climatic amelioration following the Last Glacial Maximum (LGM) may facilitate the availability of wild broomcorn millet and rice in northern China. Their high abundance during the early Holocene may make these cereals dominant choices. In contrast, the climatic impact on wild foxtail millet was minimal, and its relatively lower availability likely constrained its early consumption. During the early Holocene, the composition of local vegetation may have influenced the proportion of cereals in daily diets. By the mid-Holocene, although climatic fluctuations diminished the availability of wild broomcorn millet and rice, the expansion of agriculture became the primary driver for the widespread dominance of foxtail millet. The assessment of early human adaptation reveals that the selective utilization of cereals was part of a complex ecological and economic dynamic, initially driven by disparities in plant resource availability resulting from Holocene climatic variations. Over time, however, population demands and agricultural development increasingly shaped this process.</div></div>","PeriodicalId":20926,"journal":{"name":"Quaternary Science Reviews","volume":"358 ","pages":"Article 109350"},"PeriodicalIF":3.2,"publicationDate":"2025-04-08","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"143792557","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":"Reconstruction of environmental and hydroclimate changes in the Adriatic region over the last 367 kyr from Modrič Cave (Croatia) speleothems","authors":"Maša Surić ,&nbsp;Petra Bajo ,&nbsp;Andrea Columbu ,&nbsp;Robert Lončarić ,&nbsp;Nina Lončar ,&nbsp;Russell N. Drysdale ,&nbsp;John C. Hellstrom","doi":"10.1016/j.quascirev.2025.109351","DOIUrl":"10.1016/j.quascirev.2025.109351","url":null,"abstract":"<div><div>We report the longest episodic stable isotope (δ¹⁸O, δ¹³C) speleothem record from the eastern Adriatic coast, obtained from three U-Th dated speleothems from Modrič Cave (Croatia), covering environmental changes at orbital (glacial-interglacial cycles) and sub-orbital (millennial-to-centennial) time scales. According to the age models, speleothems grew intermittently during the last 367 ka, i.e. the time span from Marine Isotope Stage (MIS) 10 to the present, with growth episodes during 367-342 ka, 331-278 ka, 244-233 ka, 200-155 ka, 69-34 ka and from 15 ka to the present. Speleothem deposition during every interglacial and glacial period, except for the MIS 8, along with the isotope record, suggest that intermittent calcite deposition was not entirely climate controlled, but depended upon the drip site specifics, as well.</div><div>As for the speleothem isotopic signal, δ¹³C variations were governed by local soil bioactivity, while the δ¹⁸O signal was a proxy for regional hydroclimate processes. As commonly found in the Mediterranean, δ¹⁸O was controlled by precipitation amount, except during the three detected periods when the source effect outweighed the amount effect. Most likely, due to the weakened Atlantic Meridional Overturning Circulation (AMOC), ¹⁸O-depleted Atlantic moisture was partially compensated with ¹⁸O-enriched Mediterranean-sourced moisture. Regional teleconection between the North Atlantic region and the central Mediterranean has been characterized by a rapid response to abrupt climate system reorganization during Termination TI. Although future anthropogenic climate changes will occur under different boundary conditions, understanding the persistence of such rapid, dynamic teleconnections over longer time scales is of significant interest to the climate community.</div></div>","PeriodicalId":20926,"journal":{"name":"Quaternary Science Reviews","volume":"358 ","pages":"Article 109351"},"PeriodicalIF":3.2,"publicationDate":"2025-04-08","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"143792555","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":"Coupled sea-level and hydroclimatic controls on the southern Red Sea sedimentation during the past 30 ka","authors":"Francesca Paraschos ,&nbsp;Andreas Koutsodendris ,&nbsp;Spyros Sergiou ,&nbsp;Maria Geraga ,&nbsp;Helen Kaberi ,&nbsp;Melissa Berke ,&nbsp;Oliver Friedrich ,&nbsp;Stylianos Iliakis ,&nbsp;Mirko Alessandro Uy ,&nbsp;Ross Williams ,&nbsp;Geoffrey Bailey ,&nbsp;Dimitris Sakellariou","doi":"10.1016/j.quascirev.2025.109310","DOIUrl":"10.1016/j.quascirev.2025.109310","url":null,"abstract":"<div><div>Sedimentation in the Red Sea basin is governed by the complex interplay between regional atmospheric circulation, precipitation patterns, and sea level fluctuations, which altogether exert a profound control on the detrital and biogenic components of the sedimentary record. To gain a comprehensive understanding of these controls on the southern Red Sea sedimentation over the past 30 ka, we here combine high-resolution bulk geochemical and mineralogical data with detrital grain-size distributions and plant-wax biomarkers at a sub-centennial average temporal resolution. Our proxies reveal that the sedimentary record is characterised by two distinct depositional regimes of detrital and marine origin. The pronounced shift from the detrital-dominated (ca. 30–14.6 kyr) to the marine-dominated phase (ca. 14.6–0.8 kyr) coincides with the end of Heinrich Event 1 and the rapid sea-level rise associated with Meltwater Pulse 1a. Flooding of the shelf during deglacial sea-level rise increased the distance between the core site and the respective shoreline, and partially controlled the delivery of detrital material to the site. Shifts in detrital grain-size distribution and mineralogical composition indicate a reduction in regional continental aridity and potentially weaker wind circulation with the onset of Greenland Interstadial-1, while the reestablishment of water-mass exchange with the Gulf of Aden from ca. 15 ka onwards led to a marine productivity surge at our study area. An increase of fine-grained fluvial material and terrestrial <em>n</em>-alkanes between ca. 16 and 8 ka points to the establishment of more pluvial conditions and the activation of local wadi runoff during the African Humid Period. Finally, the subtle but steady increase of detrital input from ca. 5 ka onwards suggests the re-establishment of continental aridity during the late Holocene.</div></div>","PeriodicalId":20926,"journal":{"name":"Quaternary Science Reviews","volume":"357 ","pages":"Article 109310"},"PeriodicalIF":3.2,"publicationDate":"2025-04-08","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"143791486","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":1,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"OA","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

{"title":"Uplift, tilting, and underlying structures of coastal northwestern Luzon, Philippines, deduced from marine terraces","authors":"Yiran Wang ,&nbsp;Aron J. Meltzner ,&nbsp;Jennifer Quye-Sawyer ,&nbsp;Huili Yang ,&nbsp;Yichen Pu ,&nbsp;Jintang Qin ,&nbsp;Lin Thu Aung ,&nbsp;Zihan Aw ,&nbsp;Andrea Denise A. Pamintuan ,&nbsp;Noelynna T. Ramos","doi":"10.1016/j.quascirev.2025.109347","DOIUrl":"10.1016/j.quascirev.2025.109347","url":null,"abstract":"<div><div>Northern Luzon Island of the Philippines, located between the converging Sunda and Philippine Sea Plates, is a seismically active region within a complex tectonic setting. Remnants of Pleistocene marine terraces along the coast of northwestern Luzon have been deformed and provide clues to the active underlying structures. Through remote sensing and field surveys, we mapped and surveyed multiple generations of uplifted Pleistocene marine terraces between the municipalities of Pasuquin and Santo Domingo along the northwestern Luzon coast. We found that wave-cut platforms are the most common type of marine terrace in the area, each consisting of a sedimentary basement (Laoag Formation) and a fluvial or alluvial deposit cover. The uplift of these terraces shows that the area north of Laoag City has experienced westward tilting while the area farther south has been uniformly uplifted. With K-feldspar infrared stimulated luminescence (IRSL) dating of sand samples collected above the abrasion surface of the wave-cut platforms, we infer that the most prominent marine terrace, with a seaward edge 40–50 m above mean sea level, was formed during marine isotope stage (MIS) 5a. This suggests a long-term uplift rate of ∼1 m/kyr along the coast and up to 1.6 m/kyr farther inland. Combining evidence from field surveys and bathymetric and focal mechanism data, we suggest that the large-scale uplift of the coastal area is the result of slip along an east-dipping thrust with a surface trace ∼12 km off the west coast, while a west-dipping branch of the Vigan-Aggao Fault Zone has contributed to tilting, horizontal (sinistral) movement, and localized folding of the coastal area. Through elastic dislocation modeling, we suggest the offshore fault likely has a dip angle lower than 45°, and the difference in uplift patterns between north and south can be attributed to different slip-rate distributions between the two faults. Overall, we estimate west-northwest directed shortening at 1–2 m/kyr across the nearshore and coastal area of northwestern Luzon.</div></div>","PeriodicalId":20926,"journal":{"name":"Quaternary Science Reviews","volume":"358 ","pages":"Article 109347"},"PeriodicalIF":3.2,"publicationDate":"2025-04-08","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"143792556","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":1,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"OA","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}