Venericards

@incollection{gardner1957cenozoic,
    author = "Gardner, Julia and Ladd, Harry S.",
    title = "Cenozoic Mollusks of the Atlantic and East Gulf Coastal Plains",
    year = "1957",
    booktitle = "Geological Society of America Memoirs",
    url = "https://doi.org/10.1130/mem67v2-p885",
    doi = "10.1130/mem67v2-p885",
    pages = "885-886"
}

@misc{heaslip1968cenozoic1,
    author = "Heaslip, W. G",
    title = "Cenozoic evolution of the alticostate venericards in the Gulf and East Coastal North America",
    year = "1968",
    howpublished = "Palaeontographica Americana, v. 6, p. 55-135",
    note = "talkorigins\_source = {true}; raw\_reference = {Heaslip, W. G., 1968, Cenozoic evolution of the alticostate venericards in the Gulf and East Coastal North America: Palaeontographica Americana, v. 6, p. 55-135.}"
}

@article{funnell1980the,
    author = "Funnell, Brian",
    title = "The evolution of coastal East Anglia",
    year = "1980",
    journal = "Nature",
    url = "https://doi.org/10.1038/287260a0",
    doi = "10.1038/287260a0",
    number = "5779",
    pages = "260-260",
    volume = "287"
}

@article{doi1079079wjy2a97,
    author = "Weldon, R.",
    title = "The Late Cenozoic Geology of Cajon Pass; Implications for Tectonics and Sedimentation along the San Andreas Fault",
    year = "1986",
    url = "https://www.semanticscholar.org/paper/ed74ac3368d6d50d8c0f2a31e5b4abc47795d6a6",
    doi = "10.7907/9WJY-2A97.",
    is_oa = "true",
    semanticscholar_citation_count = "105",
    semanticscholar_id = "ed74ac3368d6d50d8c0f2a31e5b4abc47795d6a6"
}

@article{pindell1993mesozoiccenozoic,
    author = "{PINDELL, JAMES, Dartmouth College,}",
    title = "Mesozoic-Cenozoic Paleogeographic Evolution of Northern South America",
    year = "1993",
    journal = "AAPG Bulletin",
    url = "https://doi.org/10.1306/d9cb6f47-1715-11d7-8645000102c1865d",
    doi = "10.1306/d9cb6f47-1715-11d7-8645000102c1865d",
    volume = "77"
}

@article{doi101130b254541,
    author = "Gómez, E. and Jordan, T. and Allmendinger, R. and Hegarty, K. and Kelley, S.",
    title = "Syntectonic Cenozoic sedimentation in the northern middle Magdalena Valley Basin of Colombia and implications for exhumation of the Northern Andes",
    year = "2005",
    journal = "Geological Society of America Bulletin",
    url = "https://www.semanticscholar.org/paper/ad46d6cf733930d2caf2314c6980a5e516034dd2",
    doi = "10.1130/B25454.1",
    is_oa = "true",
    number = "5",
    pages = "547",
    semanticscholar_citation_count = "127",
    semanticscholar_id = "ad46d6cf733930d2caf2314c6980a5e516034dd2",
    volume = "117"
}

@article{ortizjaureguizar2006paleoenvironmental,
    author = "Ortiz-Jaureguizar, E. and Cladera, G.A.",
    title = "Paleoenvironmental evolution of southern South America during the Cenozoic",
    year = "2006",
    journal = "Journal of Arid Environments",
    url = "https://doi.org/10.1016/j.jaridenv.2006.01.007",
    doi = "10.1016/j.jaridenv.2006.01.007",
    number = "3",
    pages = "498-532",
    volume = "66"
}

A series of Cenozoic basins fringes the Vietnamese coastal margin, often characterised by more than 10 km of sedimentary infill (Fig. 1). Greater parts of the margin are still in an early explorational state, although significant petroleum production has taken place in all but the southern Song Hong and the Phu Khanh Basins. This has increased the need for a fundamental understanding of the processes behind the formation of the basins, including analyses of potential source rocks. The basins fringing the Indochina Block provide excellent evidence of the geological evolution of the region, and the basin geometries reflect the collision of India and Eurasia and the late Cenozoic uplift of south Indochina (Rangin et al. 1995a; Fyhn et al. in press). In addition, the basins provide evidence of regional Palaeogene rifting and subsequent Late Palaeogene through Early Neogene sea-floor spreading in the South China Sea. Apart from the regional Cenozoic tectonic record, the basins contain a high-resolution climatic record of South-East Asia due to the high depositional rates, changing depositional styles and large hinterland of the basin (Clift et al. 2004).

@article{fyhn2007cenozoic,
    author = "Fyhn, Michael B.W. and Nielsen, Lars Henrik and Boldreel, Lars Ole",
    title = "Cenozoic evolution of the Vietnamese coastal margin",
    year = "2007",
    journal = "Geological Survey of Denmark and Greenland Bulletin",
    abstract = "A series of Cenozoic basins fringes the Vietnamese coastal margin, often characterised by more than 10 km of sedimentary infill (Fig. 1). Greater parts of the margin are still in an early explorational state, although significant petroleum production has taken place in all but the southern Song Hong and the Phu Khanh Basins. This has increased the need for a fundamental understanding of the processes behind the formation of the basins, including analyses of potential source rocks. The basins fringing the Indochina Block provide excellent evidence of the geological evolution of the region, and the basin geometries reflect the collision of India and Eurasia and the late Cenozoic uplift of south Indochina (Rangin et al. 1995a; Fyhn et al. in press). In addition, the basins provide evidence of regional Palaeogene rifting and subsequent Late Palaeogene through Early Neogene sea-floor spreading in the South China Sea. Apart from the regional Cenozoic tectonic record, the basins contain a high-resolution climatic record of South-East Asia due to the high depositional rates, changing depositional styles and large hinterland of the basin (Clift et al. 2004).",
    url = "https://doi.org/10.34194/geusb.v13.4983",
    doi = "10.34194/geusb.v13.4983",
    pages = "73-76",
    volume = "13"
}

We apply adjoint models of mantle convection to North America since the Late Cretaceous. The present‐day mantle structure is constrained by seismic tomography and the time‐dependent evolution by plate motions and stratigraphic data (paleoshorelines, borehole tectonic subsidence, and sediment isopachs). We infer values of average upper and lower mantle viscosities, provide a synthesis of North American vertical motions (relative sea level) from the Late Cretaceous to the present, and reconstruct the geometry of the Farallon slab back to the Late Cretaceous. In order to fit Late Cretaceous marine inundation and borehole subsidence, the adjoint model requires a viscosity ratio across 660 km discontinuity of 15:1 (reference viscosity of 10 21 Pa s), which is consistent with values previously inferred by postglacial rebound studies. The dynamic topography associated with subduction of the Farallon slab is localized in western North America over Late Cretaceous, representing the primary factor controlling the widespread flooding. The east coast of the United States is not stable; rather, it has been experiencing continuous dynamic subsidence over the Cenozoic, coincident with an overall eustatic fall, explaining a discrepancy between sea level derived from the New Jersey coastal plain and global curves. The east coast subsidence further constrains the mantle viscosity structure and requires an uppermost mantle viscosity of 10 20 Pa s. Imposed constraints require that the Farallon slab was flat lying during Late Cretaceous, with an extensive zone of shallow dipping Farallon subduction extending beyond the flat‐lying slab farther east and north by up to 1000 km than previously suggested.

@article{doi1010292008gc002345,
    author = "Spasojević, S. and Liu, Lijun and Gurnis, M.",
    title = "Adjoint models of mantle convection with seismic, plate motion, and stratigraphic constraints: North America since the Late Cretaceous",
    year = "2009",
    journal = "Geochemistry",
    abstract = "We apply adjoint models of mantle convection to North America since the Late Cretaceous. The present‐day mantle structure is constrained by seismic tomography and the time‐dependent evolution by plate motions and stratigraphic data (paleoshorelines, borehole tectonic subsidence, and sediment isopachs). We infer values of average upper and lower mantle viscosities, provide a synthesis of North American vertical motions (relative sea level) from the Late Cretaceous to the present, and reconstruct the geometry of the Farallon slab back to the Late Cretaceous. In order to fit Late Cretaceous marine inundation and borehole subsidence, the adjoint model requires a viscosity ratio across 660 km discontinuity of 15:1 (reference viscosity of 10 21 Pa s), which is consistent with values previously inferred by postglacial rebound studies. The dynamic topography associated with subduction of the Farallon slab is localized in western North America over Late Cretaceous, representing the primary factor controlling the widespread flooding. The east coast of the United States is not stable; rather, it has been experiencing continuous dynamic subsidence over the Cenozoic, coincident with an overall eustatic fall, explaining a discrepancy between sea level derived from the New Jersey coastal plain and global curves. The east coast subsidence further constrains the mantle viscosity structure and requires an uppermost mantle viscosity of 10 20 Pa s. Imposed constraints require that the Farallon slab was flat lying during Late Cretaceous, with an extensive zone of shallow dipping Farallon subduction extending beyond the flat‐lying slab farther east and north by up to 1000 km than previously suggested.",
    url = "https://onlinelibrary.wiley.com/doi/pdfdirect/10.1029/2008GC002345",
    doi = "10.1029/2008GC002345",
    is_oa = "true",
    number = "5",
    semanticscholar_citation_count = "111",
    semanticscholar_id = "d8f65aef5b549c1ed7189645d29e964a78a5de98",
    volume = "10"
}

We have produced common conversion point (CCP) stacked Ps and Sp receiver function image volumes of the Moho and lithosphere‐asthenosphere boundary (LAB) beneath the western United States using Transportable Array data. The large image volumes and the diversity of tectonic environments they encompass allow us to investigate evolution of these structural discontinuities. The Moho is a nearly continuous topographic surface, whereas the LAB is not and the seismic images show a more complex expression. The first order change in LAB depth in the western U.S. occurs along the Cordilleran hingeline, the former Laurasian passive margin along the southwestern Precambrian North American terranes. The LAB is about 50% deeper to the east of the hingeline than to the west, with most of the increase in LAB thickness being in the mantle lithosphere. We infer that the Moho and the LAB are Late Mesozoic or Cenozoic everywhere west of the hingeline, modified during Farallon subduction and its aftermath. Between the hingeline and the Rocky Mountain Front, the LAB, and to a lesser extent the Moho, have been partially reset during the Cenozoic by processes that continue today. Seismicity and recent volcanism in the interior of the western U.S. are concentrated along gradients in crustal and/or lithospheric thickness, for example the hingeline, and the eastern edge of the coastal volcanic‐magmatic terranes. To us this suggests that lateral gradients in integrated lithospheric strength focus deformation. Similarly, areas conjectured to be the sites of convective downwellings and associated volcanism are located along gradients in regional lithosphere thickness.

@article{doi1010292012gc004056,
    author = "Levander, A. and Miller, M.",
    title = "Evolutionary aspects of lithosphere discontinuity structure in the western U.S.",
    year = "2012",
    journal = "Geochemistry",
    abstract = "We have produced common conversion point (CCP) stacked Ps and Sp receiver function image volumes of the Moho and lithosphere‐asthenosphere boundary (LAB) beneath the western United States using Transportable Array data. The large image volumes and the diversity of tectonic environments they encompass allow us to investigate evolution of these structural discontinuities. The Moho is a nearly continuous topographic surface, whereas the LAB is not and the seismic images show a more complex expression. The first order change in LAB depth in the western U.S. occurs along the Cordilleran hingeline, the former Laurasian passive margin along the southwestern Precambrian North American terranes. The LAB is about 50\% deeper to the east of the hingeline than to the west, with most of the increase in LAB thickness being in the mantle lithosphere. We infer that the Moho and the LAB are Late Mesozoic or Cenozoic everywhere west of the hingeline, modified during Farallon subduction and its aftermath. Between the hingeline and the Rocky Mountain Front, the LAB, and to a lesser extent the Moho, have been partially reset during the Cenozoic by processes that continue today. Seismicity and recent volcanism in the interior of the western U.S. are concentrated along gradients in crustal and/or lithospheric thickness, for example the hingeline, and the eastern edge of the coastal volcanic‐magmatic terranes. To us this suggests that lateral gradients in integrated lithospheric strength focus deformation. Similarly, areas conjectured to be the sites of convective downwellings and associated volcanism are located along gradients in regional lithosphere thickness.",
    url = "https://openresearch-repository.anu.edu.au/bitstream/1885/153117/2/01\_Levander\_Evolutionary\_aspects\_of\_2012.pdf",
    doi = "10.1029/2012GC004056",
    is_oa = "true",
    number = "7",
    semanticscholar_citation_count = "144",
    semanticscholar_id = "41b4df67956ae28bd384450f575b3d636a26843a",
    volume = "13"
}

@incollection{ebinger2012evolution,
    author = "Ebinger, Cynthia",
    title = "Evolution of the Cenozoic East African rift system",
    year = "2012",
    booktitle = "Regional Geology and Tectonics: Phanerozoic Rift Systems and Sedimentary Basins",
    url = "https://doi.org/10.1016/b978-0-444-56356-9.00006-7",
    doi = "10.1016/b978-0-444-56356-9.00006-7",
    pages = "132-162"
}

Based on the structural style and physiographic criteria, the Central Andes of Peru can be divided into segments running parallel to the Pacific coast. The westernmost segment, the Coastal Belt, consists of a Late Jurassic–Cretaceous volcanic arc sequence that was accreted to the South American craton in Cretaceous times. The Mesozoic strata of the adjacent Western Cordillera represent an ENE-vergent fold-and-thrust belt that formed in Eocene times. Tight upright folds developed above a shallow detachment horizon in the West, while more open folds formed above a deeper detachment horizon towards the East and in the neighboring Central Highlands. A completely different style with steeply dipping reverse faults and open folds affecting the Neoproterozoic crystalline basement is typical for the Eastern Cordillera. The Subandean Zone is characterized by mainly NE-vergent imbricate thrusting which occurred in Neogene times. A quantitative estimate of the shortening of the orogen obtained from balanced cross-sections indicates a total shortening of 120–150 km (24%–27%). This shortening was coevel with the Neogene westward drift of South America, occurred at rates between 3 and 4.7 mm/year and was responsible for the high elevation of the Peruvian Andes.

@article{doi103390geosciences3020262,
    author = "Pfiffner, O. and Gonzalez, L.",
    title = "Mesozoic–Cenozoic Evolution of the Western Margin of South America: Case Study of the Peruvian Andes",
    year = "2013",
    journal = "Geosciences",
    abstract = "Based on the structural style and physiographic criteria, the Central Andes of Peru can be divided into segments running parallel to the Pacific coast. The westernmost segment, the Coastal Belt, consists of a Late Jurassic–Cretaceous volcanic arc sequence that was accreted to the South American craton in Cretaceous times. The Mesozoic strata of the adjacent Western Cordillera represent an ENE-vergent fold-and-thrust belt that formed in Eocene times. Tight upright folds developed above a shallow detachment horizon in the West, while more open folds formed above a deeper detachment horizon towards the East and in the neighboring Central Highlands. A completely different style with steeply dipping reverse faults and open folds affecting the Neoproterozoic crystalline basement is typical for the Eastern Cordillera. The Subandean Zone is characterized by mainly NE-vergent imbricate thrusting which occurred in Neogene times. A quantitative estimate of the shortening of the orogen obtained from balanced cross-sections indicates a total shortening of 120–150 km (24\%–27\%). This shortening was coevel with the Neogene westward drift of South America, occurred at rates between 3 and 4.7 mm/year and was responsible for the high elevation of the Peruvian Andes.",
    url = "https://www.mdpi.com/2076-3263/3/2/262/pdf?version=1370341005",
    doi = "10.3390/GEOSCIENCES3020262",
    is_oa = "true",
    number = "2",
    pages = "262-310",
    semanticscholar_citation_count = "71",
    semanticscholar_id = "1cba1156f8931653eb79f222a6a68b56fd7dd5ab",
    volume = "3"
}

@article{s2e77a6cfadaf4211754d0910fb4e6da561970c92b,
    author = "Montecinos, R. and Pía, M.",
    title = "Cenozoic uplift and exhumation above the southern part of the flat slab subduction segment of Chile (28.5-32°S)",
    year = "2013",
    url = "https://www.semanticscholar.org/paper/e77a6cfadaf4211754d0910fb4e6da561970c92b",
    is_oa = "true",
    semanticscholar_citation_count = "8",
    semanticscholar_id = "e77a6cfadaf4211754d0910fb4e6da561970c92b"
}

@article{doi101016jsedgeo201404001,
    author = "Xie, Xiangyang and Mann, P.",
    title = "U-Pb detrital zircon age patterns of Cenozoic clastic sedimentary rocks in Trinidad and its implications",
    year = "2014",
    journal = "Sedimentary Geology",
    url = "https://www.semanticscholar.org/paper/a697ed88565f3180b4f5e6126842eb894ae78b11",
    doi = "10.1016/J.SEDGEO.2014.04.001",
    is_oa = "true",
    pages = "7-16",
    semanticscholar_citation_count = "8",
    semanticscholar_id = "a697ed88565f3180b4f5e6126842eb894ae78b11",
    volume = "307"
}

The Douala Basin is one of three units of the Cameroonian coastal basin in the Gulf of Guinea, formed from the east-west extension between African and South American plates generated during the opening of South Atlantic in the Early Cretaceous. This basin contains sediments from Lower Cretaceous to present. The Cretaceous depositional environments are well understood whereas there is very little information concerning Cenozoic depositional environments. Facies and their stratigraphical distribution analyses were conducted on Cenozoic formations exposed at the E-W central part of the Douala Basin in the Missole II, Piti, Missole I and Dibamba localities, with an objective to provide details on the depositional environments and to reconstruct the depositional model and their evolution over time. Seventeen (17) lithofacies were identified on the basis of lithology, grain size and sedimentary structures. The facies constitute three (3) main facies associations; the gravelly dominated, the sandy dominated and the fine grained dominated. These facies and facies associations were interpreted and five depositional environments successions were recognized; the fluvial-braided and meandered channel, the delta plain, the continental shelf and the marginal-littoral. The facies distribution shows a progradational succession from a fluvial to delta plain at the axial part of the basin and a storm dominated continental shelf to marginal-littoral at the central part of the basin. The facies stacking patterns depict sedimentation mainly controlled by sag subsidence and probably by climate.

@article{doi103844ajgsp2014823,
    author = "Chavom, Bachirou Mfayakouo and Ngaha, P. and Bitom, D.",
    title = "SEDIMENTARY FACIES AND DEPOSITIONAL ENVIRONMENTS OF CENOZOIC SEDIMENTARY FORMATIONS CROPPING OUT AT THE CENTRAL PART OF THE DOUALA BASIN",
    year = "2014",
    journal = "American Journal of Geoscience",
    abstract = "The Douala Basin is one of three units of the Cameroonian coastal basin in the Gulf of Guinea, formed from the east-west extension between African and South American plates generated during the opening of South Atlantic in the Early Cretaceous. This basin contains sediments from Lower Cretaceous to present. The Cretaceous depositional environments are well understood whereas there is very little information concerning Cenozoic depositional environments. Facies and their stratigraphical distribution analyses were conducted on Cenozoic formations exposed at the E-W central part of the Douala Basin in the Missole II, Piti, Missole I and Dibamba localities, with an objective to provide details on the depositional environments and to reconstruct the depositional model and their evolution over time. Seventeen (17) lithofacies were identified on the basis of lithology, grain size and sedimentary structures. The facies constitute three (3) main facies associations; the gravelly dominated, the sandy dominated and the fine grained dominated. These facies and facies associations were interpreted and five depositional environments successions were recognized; the fluvial-braided and meandered channel, the delta plain, the continental shelf and the marginal-littoral. The facies distribution shows a progradational succession from a fluvial to delta plain at the axial part of the basin and a storm dominated continental shelf to marginal-littoral at the central part of the basin. The facies stacking patterns depict sedimentation mainly controlled by sag subsidence and probably by climate.",
    url = "https://doi.org/10.3844/ajgsp.2014.8.23",
    doi = "10.3844/AJGSP.2014.8.23",
    is_oa = "true",
    number = "1",
    pages = "8-23",
    semanticscholar_citation_count = "15",
    semanticscholar_id = "bdcb453297bd90c34cdd89dca8a75f0837662b34",
    volume = "4"
}

Abstract The California Borderland is a region of topographic and geologic diversity along the densely populated coast of southern California and offshore > 200 km. The Borderland includes complex basin-and-range topography defined by a regional structural transition from west-east-striking reverse and thrust faults in the north to northwest-southeast-striking, dextral strike-slip faults and transpressional oblique-slip faults in the south. The Miocene-Quaternary strata within the inner (i.e., onshore and nearshore) Borderland basins host important natural resources, including petroleum and drinking water for the coastal population. The present physiography of the California Borderland basins took shape during the Cenozoic evolution of the San Andreas transform continental margin. The transform margin developed after the East Pacific Rise spreading center came into contact with the North American plate

@article{doi101016b9780444638953000127,
    author = "Covault, J. and Sharman, G.",
    title = "Tectonostratigraphic Evolution of the Inner California Borderland: Template for Fill-and-Spill Sedimentation",
    year = "2019",
    journal = "The Sedimentary Basins of the United States and Canada",
    booktitle = "The Sedimentary Basins of the United States and Canada",
    abstract = "Abstract The California Borderland is a region of topographic and geologic diversity along the densely populated coast of southern California and offshore > 200 km. The Borderland includes complex basin-and-range topography defined by a regional structural transition from west-east-striking reverse and thrust faults in the north to northwest-southeast-striking, dextral strike-slip faults and transpressional oblique-slip faults in the south. The Miocene-Quaternary strata within the inner (i.e., onshore and nearshore) Borderland basins host important natural resources, including petroleum and drinking water for the coastal population. The present physiography of the California Borderland basins took shape during the Cenozoic evolution of the San Andreas transform continental margin. The transform margin developed after the East Pacific Rise spreading center came into contact with the North American plate",
    url = "https://www.semanticscholar.org/paper/fb27f217c639cd2631544a38c923b34ffc970e22",
    doi = "10.1016/B978-0-444-63895-3.00012-7",
    is_oa = "true",
    pages = "511-528",
    semanticscholar_citation_count = "3",
    semanticscholar_id = "fb27f217c639cd2631544a38c923b34ffc970e22"
}

@article{doi101016jgloplacha2021103555,
    author = "Vallejo, C. and Romero, Christian W. and Horton, B. and Spikings, R. and Gaibor, J. and Winkler, W. and Estéban, J. J. and Thomsen, T. and Mariño, Elizabeth",
    title = "Jurassic to Early Paleogene sedimentation in the Amazon region of Ecuador: Implications for the paleogeographic evolution of northwestern South America",
    year = "2021",
    journal = "Global and Planetary Change",
    url = "https://www.semanticscholar.org/paper/1c10039b96c04e61aba337d7afbad2c000c9713f",
    doi = "10.1016/J.GLOPLACHA.2021.103555",
    is_oa = "true",
    pages = "103555",
    semanticscholar_citation_count = "32",
    semanticscholar_id = "1c10039b96c04e61aba337d7afbad2c000c9713f",
    volume = "204"
}

@article{gan2023cenozoic,
    author = "Gan, Haonan and Wang, Xiao and Wang, Bo and Wang, Guiling",
    title = "Cenozoic thermal-rheological evolution of the coastal cathaysia block of East Asia: geodynamic implications",
    year = "2023",
    journal = "International Geology Review",
    url = "https://doi.org/10.1080/00206814.2022.2150899",
    doi = "10.1080/00206814.2022.2150899",
    number = "16",
    pages = "2580-2593",
    volume = "65"
}

https://doi.org/10.59350/c48c6-j2e14 Proposed mechanisms for Cenozoic landscape evolution in southwestern North America (SWNA) include crustal isostasy, dynamic topography, or lithosphere tectonics, but their relative contributions remain controversial. Recently our study 'Coupled influence of tectonics, climate, and surface processes on landscape evolution in southwestern North America' published in Nature Communications tried to address that.

@misc{lu2023cenozoic,
    author = "Lu, Neng",
    title = "Cenozoic landscape evolution in southwestern North America",
    year = "2023",
    abstract = "https://doi.org/10.59350/c48c6-j2e14 Proposed mechanisms for Cenozoic landscape evolution in southwestern North America (SWNA) include crustal isostasy, dynamic topography, or lithosphere tectonics, but their relative contributions remain controversial. Recently our study 'Coupled influence of tectonics, climate, and surface processes on landscape evolution in southwestern North America' published in Nature Communications tried to address that.",
    url = "https://doi.org/10.59350/k1e55-2ts32",
    doi = "10.59350/k1e55-2ts32"
}

@article{he2025cenozoic,
    author = "He, Linqiang and Zhou, Tianjun and Guo, Zhun and Ren, Zikun and Chen, Xiaolong and Jiang, Jie and Chen, Fahu and Zhang, Xu and Xiong, Zhongyu and Zuo, Meng and Man, Wenmin and Zhang, Wenxia",
    title = "Cenozoic evolution of spring persistent rainfall in East Asia and North America driven by paleogeography",
    year = "2025",
    journal = "Communications Earth \& Environment",
    url = "https://doi.org/10.1038/s43247-025-02136-0",
    doi = "10.1038/s43247-025-02136-0",
    number = "1",
    volume = "6"
}