@misc{barton1936gulf,
    author = "Barton, Donald C. and Sawtelle, George",
    title = "Gulf Coast Oil Fields A Symposium on the Gulf Coast Cenozoic",
    year = "1936",
    url = "https://doi.org/10.1306/sv29337",
    doi = "10.1306/sv29337",
    openalex = "W604470536"
}

@article{murray1947cenozoic,
    author = "Murray, Grover E.",
    title = "Cenozoic Deposits of Central Gulf Coastal Plain",
    year = "1947",
    journal = "AAPG Bulletin",
    abstract = "Twenty thousand feet or more of Tertiary and Quaternary sediments are present in the central Gulf region of southern United States. They comprise a large, seaward-thickening, wedge-shaped sedimentary complex (Gulf Coast geosyncline) composed predominantly of deltaic deposits. Thin, relatively uniform and widespread, marine strata are present between the thick deltaic deposits and on the seaward edges of the deltaic masses. These thin, generally distinctive, marine strata are adaptable on the surface to detailed structural mapping; they also serve as key strata in core drilling, in tracing surface units into the subsurface, and in the preparation of subsurface structural maps. Fossils present in the marine units determine their position in the standard geological time scale and assist in determining the relative geographic position at the time of deposition. The thick, ladle-shaped, deltaic deposits are normally unadaptable to structural mapping; however, they are readily used in the construction of areal, facies, and isopachous maps. Landward, both marine and deltaic deposits are replaced by brackish-water and fluviatile sediments; seaward, the marine deposits are progressively of a deeper-water environment, the deltaic deposits are progressively more marine. The Tertiary is represented by four, perhaps five, epochs of deposition, which are, in ascending order, Paleocene, Eocene, Oligocene, Miocene and Pliocene (?). Each successively younger series of rocks occupies an outcrop position progressively nearer the present coastline. Similarly, each younger rock series has been downwarped less by the thick, geosynclinal sedimentary load and, therefore, has less southwest regional dip. The Midway (Paleocene), Claiborne (middle Eocene), Jackson (upper Eocene), and Vicksburg (Oligocene) groups each contain important marine units. The Wilcox (lower Eocene), Miocene, and Pliocene (?) are primarily deltaic deposits; they constitute the thickest Cenozoic sedimentary accumulations in the eastern Gulf region. The Quaternary is represented by two epochs of deposition, the Pleistocene and Recent. These deposits are characteristically fluviatile gravels, sands, silts, and clays; they border or fill alluvial valleys and were deposited during or subsequent to the Pleistocene glaciation. The outcrop patterns of the major rock divisions of the Central Gulf Coastal Plain are illustrated by areal geologic maps and stratigraphic sections. The thickness and structural configuration of each division is shown by isopachous and structural contour maps. Representative electrical logs illustrate the electrical pattern of each rock division.",
    url = "https://doi.org/10.1306/3d933a5b-16b1-11d7-8645000102c1865d",
    doi = "10.1306/3d933a5b-16b1-11d7-8645000102c1865d",
    number = "10",
    openalex = "W2076988154",
    pages = "1825-1850",
    volume = "31",
    references = "doi101086624603, doi101130gsab541713, doi1013061013063d93370416b111d78645000102c1865d, doi1013061013063d93378a16b111d78645000102c1865d, doi1013063d932bd616b111d78645000102c1865d, doi1013063d932fc216b111d78645000102c1865d, doi1013063d93363816b111d78645000102c1865d, doi1013063d9336b216b111d78645000102c1865d, doi1013063d9336ea16b111d78645000102c1865d, openalexw2602770706"
}

@article{blackman1951harbor,
    author = "Blackman, Berkeley and Lindner, C. P.",
    title = "HARBOR AND COASTAL PROBLEMS ON THE EAST GULF COAST",
    year = "1951",
    journal = "Coastal Engineering Proceedings",
    abstract = {The "East Gulf Coast" discussed herein embraces the coast of the Gulf of Mexico from Cape Sable, Florida, generally northerly and westerly to the Rigolets, Louisiana (See Figure 1). So far as concerns Federal waterway improvements, the section is under the jurisdiction of the South Atlantic Division, Corps of Engineers, U. S. Array, Atlanta, Ga. That section in Florida as far northward as the mouth of the Aucilla River is administered by the District Engineer, Jacksonville, Fla,; thence westerly to the Rigolets, by the District Engineer, Mobile, Ala.},
    url = "https://doi.org/10.9753/icce.v2.20",
    doi = "10.9753/icce.v2.20",
    number = "2",
    openalex = "W2338339787",
    pages = "20"
}

@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{waller1969the,
    author = "Waller, Thomas R.",
    title = "The Evolution of the Argopecten Gibbus Stock (Mollusca: Bivalvia), with Emphasis on the Tertiary and Quaternary Species of Eastern North America",
    year = "1969",
    journal = "Journal of Paleontology",
    abstract = "The living members of the Argopecten gibbus stock include the bay and calico scallops, Argopecten irradians (Lamarck) and A. gibbus (Linné), both common in the western Atlantic and Gulf of Mexico; the less common A. nucleus (Born) of the Caribbean, southern Gulf of Mexico, Antilles, and southeastern Florida; and the common A. circularis (Sowerby) and A. purpuratus (Lamarck) of the eastern Pacific. The fossil members of the stock include the ancestors of these living species together with Argopecten eboreus (Conrad), an extinct species or species-group not ancestral to any of the later taxa. This study seeks to determine evolutionary relationships within the Argopecten gibbus stock by working back through the fossil record from a model of the morphological and ecological relationships of living species and subspecies. Biologically, the study is limited to an analysis of the morphology and ecology of the living taxa deduced from population samples. Paleontologically, it is limited to an analysis of morphological variation among samples of fossil populations collected from upper Cenozoic strata (Alum Bluff Group of the middle Miocene through the Pleistocene) exposed on the Atlantic and Gulf Coastal Plains of the United States. The time span investigated is about 18 million years, according to the latest published scale of absolute time. Differences between samples were studied and evaluated by means of morphometric data consisting of 70 measurements and form ratios of the outline, ligamenture, and musculature of each valve. Using an electronic digital computer, data were subjected to univariate and bivariate analyses, and samples were compared using machine-plotted, bivariate scatter diagrams, reduced major axes, and other graphical techniques. Data from right and left valves were treated separately, except that they were recombined in the study of characters that differ between valves, thereby furnishing new information on intervalve features. The postulated phylogeny shows a poorly known species, Argopecten species b, in the early middle Miocene (Oak Grove Sand), that is apparently very near the origin of the stock. This species evolved phyletically through A. nicholsi (Gardner) of the Shoal River Formation and A. choctawhatcheensis (Mansfield) of the Arca Faunizone into A. comparilis (Tuomey \& Holmes) of the upper Miocene (Tamiami, Pinecrest, Duplin, and Yorktown Formations). A. comparilis was apparently broadly adapted and widely distributed, living in bays, sounds, and open marine waters in the western Atlantic, Gulf of Mexico, and Caribbean and probably extending through seaway passages to the Pacific, where it gave rise phyletically to A. circularis. By the end of the Miocene, on the eastern side of the Americas, this variable species had split, giving rise to a primitive bay scallop, A. anteamplicostatus (Mansfield), that, like the living bay scallop (its phyletic descendant), was probably ecologically restricted to the semienclosed waters of bays and sounds, and to another species, A. vicenarius (Conrad), probably restricted to open marine waters like the living calico scallop. The primitive bay scallop was apparently unable to reach the Pacific, but the open-marine species seems to have given rise to both the Pacific A. purpuratus and the Atlantic calico scallop, A. gibbus. The living Pacific A. circularis is morphologically primitive in that it resembles the Miocene species A. comparilis more than it does any of the later species on the eastern side of the Americas and is ecologically primitive in that it is broadly adapted and able to live both in bays and sounds and in open marine waters. During the Pleistocene, A. nucleus, a tropical bay scallop, is inferred to have split from A. gibbus and to have become morphologically convergent on the true bay scallop, A. irradians. A. eboreus, a common scallop on the eastern side of the Americas in the Miocene and Pliocene, represents a highly variable yet morphologically persistent lineage that neither split nor gave rise phyletically to other species and that became extinct during the early Pleistocene. In certain features of morphology, the A. gibbus lineage is convergent on the A. eboreus lineage, indicating that the extinct species may also have been restricted to open marine waters. On the basis of the materials analyzed thus far, the evolution (both phyletic change and splitting) of the stock has been faster on the Atlantic side of the Americas than on the Pacific side, with the living Pacific species resembling late Miocene and early Pliocene Atlantic species. Because barrier islands seem to have played a key role in speciation within the stock, it would appear that evolutionary differences may have been caused by the active coastal tectonism of the Pacific side destroying such island barriers before genetic differences between inshore and offshore scallop populations could arise. With regard to nomenclature, the name Argopecten is shown to be a senior synonym of Plagioctenium; the generic name Aequipecten is rejected for American species related to Argopecten gibbus; and it is concluded that the generic name Chlamys, sensu lato, is better applied as the subfamily name Chlamydinae. The species name Argopecten vicenarius (Conrad), unused since 1898, is reinstated as the only available name for an important taxon occurring in the Caloosahatchee Marl of Florida and the Waccamaw Formation of the Carolinas.",
    url = "https://doi.org/10.1017/s0022336000062466",
    doi = "10.1017/s0022336000062466",
    number = "S3",
    openalex = "W2728810968",
    pages = "1-125",
    volume = "43",
    references = "doi101017cbo9781139567411, doi101086404940, doi101130001676061967781125bif20co2, doi101130gsab541713, doi101139f68189, doi1023071539297, doi104159harvard9780674865327, doi107312simp92414, openalexw1513990972, openalexw2133981135, openalexw2264583994"
}

@incollection{kinsman1976chapter,
    author = "Kinsman, David J.J. and Park, Robert K.",
    title = "Chapter 8.4 Algal Belt and Coastal Sabkha Evolution, Trucial Coast, Persian Gulf",
    year = "1976",
    booktitle = "Developments in Sedimentology",
    url = "https://doi.org/10.1016/s0070-4571(08)71149-x",
    doi = "10.1016/s0070-4571(08)71149-x",
    openalex = "W1732205489",
    pages = "421-433"
}

@incollection{galloway1981depositional,
    author = "GALLOWAY, WILLIAM E.",
    title = "DEPOSITIONAL ARCHITECTURE OF CENOZOIC GULF COASTAL PLAIN FLUVIAL SYSTEMS",
    year = "1981",
    booktitle = "Recent and Ancient Nonmarine Depositional Environments",
    url = "https://doi.org/10.2110/pec.81.31.0127",
    doi = "10.2110/pec.81.31.0127",
    openalex = "W1566657324",
    pages = "127-155",
    references = "doi1010079783642814983, doi1010160037073878900027, doi101029wr003i002p00623, doi101086625561, doi101306212f6ff52b2411d78648000102c1865d, doi1023071795984, doi104324978020337108412, openalexw121949292, openalexw1539070761, openalexw1912927042"
}

@article{doi101029tc001i002p00179,
    author = "Pindell, James and Dewey, John",
    title = "Permo‐Triassic reconstruction of western Pangea and the evolution of the Gulf of Mexico\/Caribbean region",
    year = "1982",
    journal = "Tectonics",
    abstract = "A Permo‐Triassic reconstruction of western Pangea (North America, South America, Africa) is proposed that is characterized by (1) definition of the North Atlantic fit by matching of marginal offsets (fracture zones) along the opposing margins, (2) a South Atlantic fit that is tighter than the BuIlard fit and that is achieved by treating Africa as two plates astride the Benue Trough and related structures during the Cretaceous, (3) complete closure of the Proto‐Atlantic Ocean between North and South America, accomplished by placing the Yucatan block between the Ouachita Mountains and Venezuela, (4) a proposed Hercynian suture zone that separates zones of foreland thrusting from zones of arc‐related magmatic activity; to the northwest of this suture lie the Chortis block and Mexico and most of North America, and to the southeast lie South America, the Yucatan Block, Florida and Africa, and (5) satisfaction of paleomagmatic data from North America, South America, and Africa. Beginning with the proposed reconstruction, the relative motion history of South America with respect of North America is defined by using the finite difference method. Within the framework provided by the proposed relative motion history, an evolutionary model for the development of the Gulf of Mexico and Caribbean region is outlined in a series of 13 plate boundary reconstructions at time intervals from the Jurassic to the present. The model includes (1) formation of the Gulf of Mexico by 140 Ma, (2) Pacific provenance of the Caribbean plate through the North America‐South America gap during Cretaceous time, (3) Paleocene‐Early Eocene back arc spreading origin for the Yucatan Basin, whereby Cuba is the frontal arc and the Nicaragua Rise‐Jamaica‐Southern Hispaniola is the remnant arc, and (4) 1200 km of post‐Eocene cumulative offset along both the Northern and Southern Caribbean Plate Boundary Zones, allowing large‐scale eastward migration of the Caribbean plate with respect to the North and South American Plates.",
    url = "https://doi.org/10.1029/tc001i002p00179",
    doi = "10.1029/tc001i002p00179",
    openalex = "W2154463579",
    references = "doi1010160012821x78900717, doi101029jb084ib11p05973, doi101038211676a0, doi101038224125a0, doi101038249313a0, doi101086628336, doi101098rsta19650020, doi10113000167606197485273geotsn20co2, doi10113000167606197586273hmffdi20co2, doi1011300091761319797563ttitcs20co2, doi101130009176131981910ptotar20co2, doi10130683d923ed16c711d78645000102c1865d"
}

@article{doi101029tc004i001p00001,
    author = "Pindell, James",
    title = "Alleghenian reconstruction and subsequent evolution of the Gulf of Mexico, Bahamas, and Proto‐Caribbean",
    year = "1985",
    journal = "Tectonics",
    abstract = "A detailed model for the evolution of the Gulf of Mexico, the Bahamas and the Proto‐Caribbean is built within the framework provided by a detailed initial Alleghenian (western Pangean) reconstruction and an accurate subsequent relative‐motion history between North America and Gondwana (northern Africa and South America). The Alleghenian reconstruction closes all pre‐Jurassic oceans; accounts for Jurassic attenuation of continental crust by restoring that attenuation to original prerift continental thicknesses; incorporates an improved Equatorial Atlantic fit between northern Brazil and the Guinea margin of Africa; quantitatively removes changes in shape of northern South America due to Late Cretaceous and Cenozoic accretion and internal deformation; includes pre‐Mesozoic continental crust presently underlying the western Bahamas and southern Florida; and correlates Late Paleozoic geology of Yucatan with its neighboring continental masses. Extension occurred within the Gulf of Mexico from Late Triassic to earliest Cretaceous time, but seafloor spreading was delayed until the Late Callovian. This divided a single Gulf‐wide salt basin into the Louann and Campeche salt provinces. The Yucatan block progressively rotated about 43 degrees counterclockwise away from the Texas‐Louisiana margin around a pole in northern Florida. The Tamaulipas‐Golden Lane‐Chiapas fault zone of eastern Mexico is interpreted as the remains of an initially intracontinental transform system along which Yucatan migrated. Attenuated continental crust beneath southern Florida and the western Bahamas, termed here the Florida Straits block, migrated approximately 300 km out of the eastern Gulf, approximately along Central Atlantic flow lines. These rotations are consistent with recently suggested magnetic anomaly trends in the Gulf of Mexico (Shepherd et al., 1982; S. Hall, personal communication, 1984). The Proto‐Caribbean formed synchronously by a fan‐like rotation of Yucatan away from Venezuela.",
    url = "https://doi.org/10.1029/tc004i001p00001",
    doi = "10.1029/tc004i001p00001",
    openalex = "W2062024970",
    references = "doi10113000167606198394941teomaa20co2"
}

@article{curtis1989source,
    author = "Curtis, Doris M.",
    title = "Source of Oils in Gulf Coast Cenozoic Reservoirs: ABSTRACT",
    year = "1989",
    journal = "AAPG Bulletin",
    url = "https://doi.org/10.1306/44b4a8ed-170a-11d7-8645000102c1865d",
    doi = "10.1306/44b4a8ed-170a-11d7-8645000102c1865d",
    openalex = "W2036358704",
    volume = "73"
}

@article{doi10108008912968909386518,
    author = "Allmon, Warren D.",
    title = "Paleontological completeness of the record of lower tertiary mollusks, U.S. Gulf and Atlantic coastal plains: Implications for phylogenetic studies",
    year = "1989",
    journal = "Historical Biology",
    abstract = "Choice of method in phylogenetic analysis should involve some consideration of the quality or completeness of the available fossil record. If it is poor, cladistic methods are preferable; if it is good, stratophenetic methods may be valid. A concept of paleontological completeness, defined herein, is useful for judging the quality of a given fossil record. This paper considers eight possible measures of paleontological completeness, and evaluates their value as phylogenetically useful estimates of the quality of the fossil record. Of the eight measures, Sadler‐Schindel type analysis of stratigraphic completeness and analysis of geographic ranges appear to be the most useful and reliable. The remaining six are useful only as rough approximations of the quality of the record, or as supporting evidence for conclusions based on other methods. Use of these eight measures on the lower Tertiary molluscan record of the U.S. Gulf and Atlantic coastal plains indicates that this record is approximately 30–50\% complete. This is probably not complete enough to trust purely stratophenetic approaches to phylogenetic analysis, but is too complete to ignore the record in favor of a purely atemporal, cladistic approach. The concept of paleontological completeness may be useful in estimating the quality of this and other fossil records for non‐phylogenetic purposes, such as studies of evolutionary rates and diversity and extinction patterns.",
    url = "https://doi.org/10.1080/08912968909386518",
    doi = "10.1080/08912968909386518",
    openalex = "W2000907561",
    references = "doi1010160031018284900981, doi105724gcs84050109"
}

@incollection{doi101130dnaggnaa97,
    author = "Worrall, Dan M. and Snelson, S.",
    title = "Evolution of the northern Gulf of Mexico, with emphasis on Cenozoic growth faulting and the role of salt",
    year = "1989",
    booktitle = "Geological Society of America eBooks",
    abstract = "Abstract The northern Gulf of Mexico Basin, although one of the most intensely studied and explored regions in North America, is also one of the most structurally complex (Figs. 1 and 2). Cenozoic depocenters contain abundant growth faults of a variety of shapes, orientations, sizes, and complexities. In addition, salt domes, flows, and massifs combine to form a complex near-surface pattern that tends to mask the origins of many structures. Not surprisingly, a number of contrasting hypotheses have been proposed to explain the growth faults of this region, among them theories invoking shale diapirism, shale compaction, gravity gliding, salt diapirism, and salt flow. Clearly, the best way to understand the various origins of these features is to observe their structural underpinnings at depth; unfortunately, most of the large growth fault systems of the Texas and Louisiana shelf project below the bottoms of seismic lines of 6- or 7-sec record length. However, as will be discussed in this chapter, deep seismic data now available from the Louisiana slope greatly illuminate the spectacular structural development of this province. In addition, palinspastic reconstructions are useful for analyzing the structural development of these features, and for constraining hypotheses on their origins. Prior to discussing the Cenozoic tectonic development of the northern Gulf of Mexico—the main focus of this chapter—we will briefly review the pre-Cenozoic framework and basic Cenozoic depositional patterns of the Gulf of Mexico Basin, both of which influenced Cenozoic structural styles. The Gulf of Mexico Basin (Fig. 1) was initiated in the late Middle to early Late Jurassic as a result of crustal attenuation and sea-floor spreading associated with the breakup of the supercontinent Pangea.",
    url = "https://doi.org/10.1130/dnag-gna-a.97",
    doi = "10.1130/dnag-gna-a.97",
    openalex = "W2488817644",
    references = "doi1010800072139519759989753, doi10113000167606198394941teomaa20co2, doi10130603b5a2f516d111d78645000102c1865d, doi1013060bda5a8316bd11d78645000102c1865d"
}

@incollection{crossref1995cenozoic,
    title = "Cenozoic Structural Evolution and Tectono-Stratigraphic Framework of the Northern Gulf Coast Continental Margin",
    year = "1995",
    booktitle = "Salt Tectonics",
    url = "https://doi.org/10.1306/m65604c6",
    doi = "10.1306/m65604c6",
    openalex = "W2151332720",
    pages = "109-151"
}

@article{doi101306522b49a1172711d78645000102c1865d,
    author = "Liangqing, Xue",
    title = "Depositional Cycles and Evolution of the Paleogene Wilcox Strata, Gulf of Mexico Basin, Texas",
    year = "1997",
    journal = "AAPG Bulletin",
    abstract = "ABSTRACT The Wilcox Group is one of the major thick clastic successions of the Tertiary Gulf Coast. The Wilcox is conventionally subdivided into lower, middle, and upper parts. Detailed correlation of more than 700 well logs has identified two depositional cycles of the Wilcox strata, each of which is represented by four parasequence sets or high-frequency genetic stratigraphic sequences. Two depositional cycles bounded by maximum flooding events were characterized by depocenter shifting, shelf-margin progradation, and deposi-tional system evolution, and lasted several million years. The sedimentary record of two depositional cycles documents two aspects of these cycles. One aspect is that the shelf margin alternated between periods of active outbuilding and periods of relative stability or minor retrogradation. Another aspect of the cycle is that depositional system evolution displays a progression from progradation to aggradation to retrogressive transgression. The time spans of these two cycles are 3.6 m.y. and 7.5 m.y., respectively, based on the Haq time scale. Each of the two depositional cycles generally corresponds to a pulse of Laramide tectonism. Deposition of two cycles may also reflect a eustatic sea level overprint.",
    url = "https://doi.org/10.1306/522b49a1-1727-11d7-8645000102c1865d",
    doi = "10.1306/522b49a1-1727-11d7-8645000102c1865d",
    openalex = "W2170624036",
    references = "doi1013063d933e2d16b111d78645000102c1865d, doi1013065ceae1c616bb11d78645000102c1865d"
}

@article{doi101016s1367912001000694,
    author = "Hall, Robert",
    title = "Cenozoic geological and plate tectonic evolution of SE Asia and the SW Pacific: computer-based reconstructions, model and animations",
    year = "2002",
    journal = "Journal of Asian Earth Sciences",
    url = "https://doi.org/10.1016/s1367-9120(01)00069-4",
    doi = "10.1016/s1367-9120(01)00069-4",
    openalex = "W2068365898",
    references = "doi1010079781461323518, doi101016s0012821x98001988, doi101016s0012821x99001314, doi101017cbo9780511524936, doi10102994gl02118, doi10102994jb03098, doi101029gm027p0023, doi101029jb075i014p02625, doi101029jb077i023p04432, doi101029jb091ib03p03664, doi101029jb093ib12p15085, doi101029me001, doi101111j1365246x1990tb06579x, doi101111j155856461960tb03057x, doi101126science1483671754, doi101126science23547931156, doi101126science25550521663, doi101126science29054981910, doi10113000917613198210611petian20co2, doi101130dnaggnam351, doi101130spe206, doi101144gslsp19981430117, doi1023072399464, doi1023073515620, doi102973odpprocsr1271281992, openalexw2989049194, openalexw3126336940, openalexw641398428"
}

@article{openalexw2271539750,
    author = "McClure, Kate J.",
    title = "Phylogenetic relationships and morphological changes in Venericardia on the Gulf Coastal Plain during the Paleogene",
    year = "2009",
    journal = "W\&M Publish (College of William \& Mary)",
    abstract = "The bivalve genus Venericardia is abundant and exceptionally well-preserved on the U.S. Gulf Coastal Plain during the Paleogene. The climate was extremely variable during the Paleogene, allowing the system to serve as a proxy for modern climate change. The primary goal of this research was to quantitatively reconstruct the phylogenetic relationships among venericard species and to explore patterns in venericard morphology. A phylogeny was produced from 70 qualitative multi-state characters applied to over 37 species and analyzed using a parsimony-based approach. This phylogeny identified the major clades of venericards that occur in Paleogene units along the Gulf Coastal Plain, as well as their relationships to European venericards. The phylogenetic framework was applied to investigate the evolution of external ornamentation and the validity of proposed subgenera. Landmark data were collected via digital images of the internal and cross-sectional orientations of right venericard valves and used to explore the morphometric relationships among hypothesized groups. Finally, the timing of phylogenetic events and morphometric changes were compared with climate shifts. \n \nThe phylogeny demonstrates that alticostate venericards form a monophyletic group within the venericard genus. None of the proposed venericard subgenera are monophyletic, although European and North American venericard species are closely related. The interior and cross-sectional morphospaces indicate that alticostate and planicostate venericards are morphometrically separate and that the proposed subgenera are all morphometrically distinct. Venericard diversity increased after the Paleocene-Eocene Thermal Maximum, although there is no significant morphological change across the climate shift. After the Eocene-Oligocene Transition, venericards suffered an \nextinction and became more globose in shape. These patterns could suggest that venericard morphology responds more strongly to temperature decreases than to increases.",
    url = "https://openalex.org/W2271539750",
    openalex = "W2271539750"
}

@article{doi101130ges006471,
    author = "Galloway, William E. and Whiteaker, T. and Ganey-Curry, Patricia",
    title = "History of Cenozoic North American drainage basin evolution, sediment yield, and accumulation in the Gulf of Mexico basin",
    year = "2011",
    journal = "Geosphere",
    abstract = "The Cenozoic fi ll of the Gulf of Mexico basin contains a continuous record of sediment supply from the North American continental interior for the past 65 million years.",
    url = "https://doi.org/10.1130/ges00647.1",
    doi = "10.1130/ges00647.1",
    openalex = "W2021800930",
    references = "doi101016b9780444594259000287, doi101016b9780444594259000299, doi101016jearscirev200810003, doi101038nature06588, doi101086509246, doi101111j13652117200900397x, doi101126science1059412, doi1011300016760619881001023papsol23co2, doi101130b262311, doi101130dnaggnag3261, doi101130mem144p45, doi101146annurevearth32091003143456, doi101306703c9af5170711d78645000102c1865d, doi1013068626c37f173b11d78645000102c1865d, galloway1981depositional"
}

@article{doi10130604011312073,
    author = "Hudec, Michael R. and Norton, Ian O. and Jackson, Martin P. A. and Peel, Frank J.",
    title = "Jurassic evolution of the Gulf of Mexico salt basin",
    year = "2013",
    journal = "AAPG Bulletin",
    abstract = "Abstract We present a new hypothesis for the Jurassic plate-tectonic evolution of the Gulf of Mexico basin and discuss how this evolution influenced Jurassic salt tectonics. Four interpretations, some based on new data, constrain the hypothesis. First, the limit of normal oceanic crust coincides with a landward-dipping basement ramp near the seaward end of the salt basin, which has been mapped on seismic data. Second, the deep salt in the deep-water Gulf of Mexico can be separated into provinces on the basis of position with respect to this ramp. Third, paleodepths in the postsalt sequence indicate that salt filled the Gulf of Mexico salt basin to near sea level. Fourth, seismic data show that postsalt sediments in the central Louann and the Yucatan salt basins exhibit large magnitudes of Late Jurassic salt-detached extension not balanced by equivalent salt-detached shortening. In our hypothesis, Callovian salt was deposited in preexisting crustal depressions on hyperextended continental and transitional crust. After salt deposition ended, rifting continued for another 7 to 12 m.y. before sea-floor spreading began. During this phase of postsalt crustal stretching, the salt and its overburden were extended by 100 to 250 km (62–155 mi), depending on location. Sea-floor spreading divided the northern Gulf of Mexico into two segments, separated by the northwest-trending Brazos transform. The eastern segment opened from east to west, leaving the Walker Ridge salient in the center of the basin as the final area to break apart. In some areas, salt flowed seaward onto new oceanic crust, first concordantly over the basement as a parautochthonous province, then climbing up over stratigraphically younger strata as an allochthonous province.",
    url = "https://doi.org/10.1306/04011312073",
    doi = "10.1306/04011312073",
    openalex = "W2134109970",
    references = "crossref1995cenozoic, doi1010073540323449, doi10102996jb03223, doi101029tc001i002p00179, doi101029tc004i001p00001, doi10103823231, doi101038242240a0, doi101038316033a0, doi101038nature09988, doi101126science27753341956, doi1011300091761319960240363aiotms23co2, doi101130dnaggnaj389, doi10130606210404017"
}

@article{doi10130604011312074,
    author = "Hudec, Michael R. and Jackson, Martin P. A. and Peel, Frank",
    title = "Influence of deep Louann structure on the evolution of the northern Gulf of Mexico",
    year = "2013",
    journal = "AAPG Bulletin",
    abstract = "Abstract Three aspects of basement structure and rift-related salt distribution have especially influenced the evolution of the deep-water northern Gulf of Mexico: (1) creation of a basement high (Toledo Bend flexure), separating a chain of interior basins from the central Louann salt basin, (2) segmentation of the central Louann salt basin by the Brazos transfer fault into eastern and central domains, and (3) salt provinces formed during basin opening. The Toledo Bend flexure was reactivated as a hinge during the Cenozoic uplift of the North American craton. This uplift triggered gravity gliding, forming fold belts in the seaward parts of the continental margin. The geometry of the Toledo Bend flexure influenced the position of these fold belts. The Brazos transfer fault separates the west sector of the study area from the central and east sectors. Most of the salt in the deep-water northern Gulf of Mexico lay in the central sector, which sourced most of the Sigsbee salt canopy. The western sector was narrower and was subdivided by the East Breaks basement high. Splitting the Callovian salt basin in two as the gulf opened created a southward-thinning wedge of salt at the seaward end of the northern Gulf of Mexico. We divide this wedge into a series of provinces on the basis of the geometry of the base of the deep salt. Original salt thickness influenced diapir location, the geometry of the Sigsbee canopy, the geometry and style of later compressional fold belts, and petroleum systems.",
    url = "https://doi.org/10.1306/04011312074",
    doi = "10.1306/04011312074",
    openalex = "W2161849672",
    references = "doi101130dnaggnaj245, doi10130604011312073"
}

@article{doi1010022014jb011311,
    author = "Eddy, Drew and Avendonk, Harm J. A. Van and Christeson, Gail and Norton, Ian O. and Karner, Garry D. and Johnson, Christopher and Snedden, John W.",
    title = "Deep crustal structure of the northeastern Gulf of Mexico: Implications for rift evolution and seafloor spreading",
    year = "2014",
    journal = "Journal of Geophysical Research Solid Earth",
    abstract = "Abstract We image deep crustal structure using marine seismic refraction data recorded by a linear array of ocean‐bottom seismometers in the Gulf of Mexico Basin Opening project (GUMBO Line 3) in order to provide new constraints on the nature of continental and oceanic crust in the northeastern Gulf of Mexico. GUMBO Line 3 extends \textasciitilde 524 km from the continental shelf offshore Pensacola, Florida, across the De Soto Canyon and into the central Gulf basin. Travel times from long offset, wide angle reflections and refractions resolve compressional seismic velocities and layer boundaries for sediment, crystalline crust, and upper mantle. We compare our results with coincident multichannel seismic reflection data. Our velocity model recovers shallow seismic velocities (\textasciitilde 2.0–4.5 km/s) that we interpret as evaporites and clastic sediments. A Cretaceous carbonate platform is interpreted beneath the De Soto Canyon with seismic velocities >5.0 km/s. Crystalline continental crust thins seaward along GUMBO Line 3 from 23–10 km across the De Soto Canyon. High seismic velocity lower crust (>7.2 km/s) is interpreted as extensive syn‐rift magmatism and possibly mafic underplating, common features at volcanic rift margins with high mantle potential temperatures. In the central Gulf basin we interpret thick oceanic crust (>8 km) emplaced at a slow full‐spreading rate (\textasciitilde 24 mm/yr). We suggest a sustained thermal anomaly during slow seafloor‐spreading conditions led to voluminous basalt flows from a spreading ridge that overprinted seafloor magnetic anomalies in the northeastern Gulf of Mexico.",
    url = "https://doi.org/10.1002/2014jb011311",
    doi = "10.1002/2014jb011311",
    openalex = "W2139421241",
    references = "doi10130604011312073, doi10130606210404017"
}

@article{doi101017jpa201523,
    author = "McClure, Kate J. and Lockwood, Rowan",
    title = "Relationships among Venericardia (Bivalvia: Carditidae) on the U.S. Coastal Plain during the Paleogene",
    year = "2015",
    journal = "Journal of Paleontology",
    abstract = "Abstract Despite the abundance and diversity of Venericardia bivalves on the U.S. Coastal Plain during the Paleogene, the evolutionary relationships within the genus remain unresolved. The primary objectives of this study were to reconstruct a phylogeny of Venericardia species, identify major clades within the genus, and determine whether groupings within traditional venericard classifications constitute monophyletic taxa. Fifty-one conchological characters were applied to 18 venericard and two outgroup species. Parsimony analysis produced three equally parsimonious trees and robustness was assessed through Bremer support and bootstrap values. The resultant trees indicate that the smooth-ribbed planicostate venericards are monophyletic, whereas the sharp-ribbed alticostate venericards are paraphyletic. Additionally, the original planicostate subtaxon, Venericor, is monophyletic whereas the original alticostate subtaxa, Claibornicardia, Glyptoactis, and Rotundicardia, are nonmonophyletic.",
    url = "https://doi.org/10.1017/jpa.2015.23",
    doi = "10.1017/jpa.2015.23",
    openalex = "W2187444455"
}

@article{doi1010022015jb012615,
    author = "Sanford, Jason C. and Snedden, John W. and Gulick, S. P. S.",
    title = "The Cretaceous‐Paleogene boundary deposit in the Gulf of Mexico: Large‐scale oceanic basin response to the Chicxulub impact",
    year = "2016",
    journal = "Journal of Geophysical Research Solid Earth",
    abstract = "Abstract Hydrocarbon exploration in the last decade has yielded sufficient data to evaluate the Gulf of Mexico basin response to the Chicxulub asteroid impact. Given its passive marine setting and proximity to the impact structure on the Yucatán Peninsula, the gulf is the premier locale in which to study the near‐field geologic effect of a bolide impact. We mapped a thick (decimeter‐ to hectometer‐scale) deposit of carbonate debris at the Cretaceous‐Paleogene boundary that is ubiquitous in the gulf and readily identifiable on borehole and seismic data. We interpret deposits seen in seismic and borehole data in the deepwater gulf to be predominately muddy debrites with minor turbidites based on cores in the southeastern gulf. Mapping of the deposit in the northern Gulf of Mexico reveals that the impact redistributed roughly 1.05 × 10 5 km 3 of sediment therein and over 1.98 × 10 5 km 3 gulfwide. Deposit distribution suggests that the majority of sediment derived from coastal and shallow‐water environments throughout the gulf via seismic and megatsunamic processes initiated by the impact. The Texas shelf and northern margin of the Florida Platform were significant sources of sediment, while the central and southern Florida Platform underwent more localized platform collapse. The crustal structure of the ancestral gulf influenced postimpact deposition both directly and indirectly through its control on salt distribution in the Louann Salt Basin. Nevertheless, impact‐generated deposition overwhelmed virtually all topography and depositional systems at the start of the Cenozoic, blanketing the gulf with carbonate debris within days.",
    url = "https://doi.org/10.1002/2015jb012615",
    doi = "10.1002/2015jb012615",
    openalex = "W2342207590",
    references = "doi10130604011312073"
}

@article{doi101130g387651,
    author = "Sharman, Glenn R. and Covault, Jacob A. and Stöckli, Daniel F. and Wroblewski, Anton and Bush, Meredith A.",
    title = "Early Cenozoic drainage reorganization of the United States Western Interior–Gulf of Mexico sediment routing system",
    year = "2016",
    journal = "Geology",
    abstract = "Abstract Continental-scale drainages host the world’s largest rivers and offshore sediment accumulations, many of which contain significant petroleum reserves. Rate of sediment supply in these settings may be a signal of external controls (e.g., tectonics) on landscape evolution, yet deciphering these controls remains a major challenge in interpreting the ancient stratigraphic record. Integration of new and published detrital zircon U-Pb ages from the United States Rocky Mountain region and Gulf of Mexico (GOM) sedimentary basin demonstrates profound changes in the U.S. continental drainage divide that controlled the rate of sediment delivery to the northern GOM during Paleocene–Eocene time. Sedimentation rate increased dramatically during deposition of the lower Wilcox Group, reaching approximately three times the Cenozoic average, accompanied by pronounced shoreline regression and delivery of a large volume of sand to the basin floor. We hypothesize that this increase in sediment delivery to the GOM resulted from drainage capture of a significant portion of the Sevier-Laramide structural province (∼900,000 km2) that included the headwaters of the California and Idaho Rivers. Capture of the California River drainage may have occurred in the vicinity of the Hanna Basin of eastern Wyoming that previously emptied northward into a shallow seaway, but was subsequently diverted southward to the Rockdale delta, which accumulated within the Houston embayment during the time of deposition of the lower Wilcox Group. Detrital zircon U-Pb ages from Wilcox samples within the Rockdale delta show a remarkable similarity with contemporaneous Laramide synorogenic units, including enrichment in detritus derived from the Cordilleran arc and basement terranes of western North America relative to older and younger units in the Houston embayment. A subsequent order of magnitude decline in sedimentation rate to the GOM can be partly attributed to well-documented drainage closure (∼800,000 km2) that accompanied lake formation in interior Laramide basins (ca. 53–51.8 Ma). Our results demonstrate that tectonically induced drainage migration in the high-relief segments of continental-scale drainages can have a pronounced effect on the rate of sediment transfer to continental margins.",
    url = "https://doi.org/10.1130/g38765.1",
    doi = "10.1130/g38765.1",
    openalex = "W2567603126",
    references = "doi101130ges009171"
}

@article{doi101190int201500861,
    author = "Umbarger, K. and Snedden, John W.",
    title = "Delineation of post-KPg carbonate slope deposits as a sedimentary record of the Paleogene linkage of De Soto Canyon and Suwannee Strait, northern Gulf of Mexico",
    year = "2016",
    journal = "Interpretation",
    abstract = "Abstract Seismicity generated from the Chicxulub impact has been postulated as the cause for the dramatic alteration of basin margin morphology and catastrophic movement of sediments in the Gulf of Mexico (GOM). Immediately following the impact, the formation of the Cretaceous-Paleogene boundary deposit (KPBD) was widespread and caused considerable erosion as portions of the Florida Escarpment collapsed, inducing sediment failure on the northern Florida Platform and formation of the ancestral De Soto Canyon. Overlying the more prominent KPBD existed a distinct, younger, post-Cretaceous/Paleogene carbonate slope deposit (CSD) confined within the De Soto Canyon bathymetric feature. Presence of this discrete unit provided insight into the post-impact history of De Soto Canyon and its long-duration connection to the Suwannee Strait, which linked the GOM with the Atlantic Ocean for almost 40 ma. We have postulated that the bathymetric low of the De Soto Canyon acted as a conduit for west to east sediment movement from nearby carbonate-dominated shorelines into the canyon in episodic sediment transport events from the Danian to the earliest Miocene. Closure of the Suwannee Strait, due to sediment infilling, terminated deposition of the De Soto Canyon CSD. This was followed by major siliciclastic influx as the paleo-Tennessee drainage system began to enter the Mississippi Canyon area.",
    url = "https://doi.org/10.1190/int-2015-0086.1",
    doi = "10.1190/int-2015-0086.1",
    openalex = "W2273860324",
    references = "doi101126science22346411135, doi1013061013063d93370416b111d78645000102c1865d"
}

@article{doi1011646zootaxa433813,
    author = "Pérez, Damián E. and del Río, Claudia J.",
    title = "Systematics of the family Carditidae (Bivalvia: Archiheterodonta) in the Cenozoic of Argentina",
    year = "2017",
    journal = "Zootaxa",
    abstract = "The systematics of the Family Carditidae is currently poorly elucidated. This paper reviews the Eocene to Pleistocene carditids from Patagonia and Entre Ríos Province (Argentina). Twelve species are described and illustrated and the presence of the genera Cyclocardia Conrad, Pleuromeris Conrad, Scalaricardita Sacco, Fasciculicardia Maxwell and Purpurocardia Maxwell in southern South America is discussed. The genus Scalaricardita is documented for the first time in South America. Two new genera, Darwinicardia gen. nov. and Kolmeris n. gen. are proposed for the species 'Venericardia' patagonica (Sowerby) and 'V.' tehuelchana (Ihering), respectively, and one new species, Cyclocardia dalek sp. nov., is described.",
    url = "https://doi.org/10.11646/zootaxa.4338.1.3",
    doi = "10.11646/zootaxa.4338.1.3",
    openalex = "W2766699549",
    references = "doi101016jjsames200505006"
}

@article{doi101111jbi13471,
    author = "Vermeij, Geerat J. and Banker, Roxanne and Capece, Lena R. and Hernandez, Emilia S. and Salley, Sydney O. and Vriesman, Veronica Padilla and Wortham, Barbara E.",
    title = "The coastal North Pacific: Origins and history of a dominant marine biota",
    year = "2018",
    journal = "Journal of Biogeography",
    abstract = "Abstract Aims Some biogeographical regions act primarily as donors of colonists to other regions, while others act predominantly as recipient areas. How some biotas become dominant while others do not is a largely historical question that has received surprisingly little attention from biogeographers. Here, we seek to answer this question for the cold‐water North Pacific biota, which did not exist forty million years ago but which is now the principal donor biota outside the tropics. Location We focus on the cool‐temperate coastal North Pacific Ocean over the last 36.5 million years. Taxon We consider all multicellular taxa for which adequate fossil, phylogenetic and biogeographical data exist. Methods After placing North Pacific geographical events in the broader context of ocean gateways opening and closing elsewhere in the world, we discuss the history and factors affecting the planktonic and benthic productivity in the North Pacific based on a review and critical evaluation of the literature. A synthesis of primary sources was used to evaluate the origins and fates of North Pacific lineages, with special emphasis on movements to, within and from the North Pacific during the Cenozoic era. Results During the Late Eocene to earliest Miocene, the cooling North Pacific received colonists from adjacent warm‐water regions and the cold Southern Hemisphere, where temperate conditions had existed since at least the Cretaceous. From the Miocene onward, the North Pacific biota began to spread to the Southern Hemisphere and through Bering Strait to the Arctic and North Atlantic Oceans. Within the North Pacific, lineages during the early cooling phases spread predominantly from west to east, but in the Early Middle Miocene this pattern reversed, with later expansions going in both directions. An increase in productivity, powered by the evolution of highly productive seaweeds and by consumers with high metabolic rates, accompanied the transformation of the North Pacific from a recipient to donor biota. Main conclusions The North Pacific replaced the Southern Hemisphere temperate biota as the principal donor biota during the Miocene through a combination of increasing productivity, low magnitudes of extinction and intense competition and predation in an ocean basin with a long coastline.",
    url = "https://doi.org/10.1111/jbi.13471",
    doi = "10.1111/jbi.13471",
    openalex = "W2902777991",
    references = "doi1011646zootaxa433813"
}

@article{doi102110jsr201779,
    author = "Cuadrado, Diana G. and Pan, Jerónimo",
    title = "Field Observations On the Evolution of Reticulate Patterns in Microbial Mats in a Modern Siliciclastic Coastal Environment",
    year = "2018",
    journal = "Journal of Sedimentary Research",
    abstract = "Reticulate patterns often found in siliciclastic rocks as wrinkle structures may have been associated with or the product of biological activity. They are also present in modern environments, and laboratory experiments have elucidated the role of filamentous cyanobacteria in their formation, thus considering these microbes putatively as ecosystem engineers. The present study traces the evolution of reticulate structures in situ in a modern siliciclastic coastal sedimentary basin for over a year, under different hydrodynamic conditions. The results give new insights on the parameters involved in the formation and preservation of these microbial structures. Field observations documented the development of millimeter-size microbial reticulate structures with specific geometries. They were found in ephemeral ponds starting from two-dimensional submerged laminated cyanobacterial mats, and ultimately created three-dimensional protruding tufts and pinnacles in junctional positions after their desiccation. Reticulate patterns were formed on top of microbial mats four days after a storm flooding and two days after seawater vacated the area under calm conditions, by virtue of the motility of filamentous cyanobacteria. Through their subsequent consolidation they can be maintained in the form of reticulate structures and tufts for extended periods (months). These structures were found sharing an area with deformation sedimentary structures such as microbial folds, roll-ups, and ripped mats, formed under high energy. Therefore, calm settings such as those created by a shallow-water lamina seem to be a requisite for the formation of reticulate structures in the microbial mats, but once they become established, the microbial mats withstand high-energy hydrodynamic regimes. Our observations of modern structures and the sequential in situ study of their evolution provide linking references to laboratory and rock-record microbial reticulates, aiding in paleoenvironmental reconstruction.",
    url = "https://doi.org/10.2110/jsr.2017.79",
    doi = "10.2110/jsr.2017.79",
    openalex = "W2782536658",
    references = "doi101016jprecamres201308001, doi101111j136530911977tb00135x, doi101111j15746941200800537x"
}

@article{doi101016jgr202204012,
    author = "Dong, Yunpeng and Sun, Shengsi and Santosh, M. and Hui, Bo and Sun, Jiaopeng and Zhang, Feifei and Cheng, Bin and Yang, Zhao and Shi, Xiaohui and He, Dengfeng and Yang, Lei and Cheng, Chao and Liu, Xiaoming and Zhou, Xiaohu and Wang, Wei and Qi, N. D.",
    title = "Cross Orogenic Belts in Central China: Implications for the tectonic and paleogeographic evolution of the East Asian continental collage",
    year = "2022",
    journal = "Gondwana Research",
    url = "https://doi.org/10.1016/j.gr.2022.04.012",
    doi = "10.1016/j.gr.2022.04.012",
    openalex = "W4225262762",
    references = "doi101016jearscirev201009010, doi101144gslmem20060320101, doi10136003yd0085"
}

@article{doi101186s13358023003025,
    author = "Schwarzhans, Werner and Aguilera, Orangel",
    title = "Otoliths of the Gobiidae from the Neogene of tropical America",
    year = "2024",
    journal = "Swiss Journal of Palaeontology",
    abstract = "Abstract Otoliths are common and diverse in the Neogene of tropical America. Following previous studies of Neogene tropical American otoliths of the lanternfishes (Myctophidae), marine catfishes (Ariidae), croakers (Sciaenidae), and cusk-eels (Ophidiiformes), we describe here the otoliths of the gobies (Gobiidae). The Gobiidae represent the richest marine fish family, with more than 2000 species worldwide and about 250 in America. In the fossil record too they are the species richest family in the Neogene of tropical America. We have investigated otoliths sampled from Ecuador, Pacific and Atlantic Panama, Atlantic Costa Rica, Dominican Republic, Venezuela, and Trinidad, ranging in age from late Early Miocene (late Burdigalian) to late Early Pleistocene (Calabrian). Most of the studied material originates from the collection expeditions of the Panama Paleontology Project (PPP). Our study represents the first comprehensive record of fossil gobies from America, and we recognize 107 species, of which 51 are new to science, 35 are in open nomenclature, and 19 represent species that also live in the region today. Previously, only two fossil otolith-based goby species have been described from the Neogene of tropical America. The dominant gobies in the fossil record of the region are from the Gobiosomatini, particularly of genera living over soft bottoms or in deeper water such as Bollmannia, Microgobius, Antilligobius, and Palatogobius. Another purpose of our study is to provide a first comprehensive account of otoliths of the extant Gobiidae of America, which we consider necessary for an adequate identification and interpretation of the Neogene otoliths. We studied otoliths of 130 extant American gobiid species and figured 106 of them for comparison. We also present a morphological analysis and characterization of the extant otoliths as a basis for the identification of fossil otoliths. Problems that commonly arise with the identification of fossil otoliths and specifically of fossil goby otoliths are addressed and discussed. A comparison of the history of the Gobiidae in tropical America reveals a high percentage of shared species between the Pacific and the Atlantic basins during the Late Miocene (Tortonian and Messinian) from at least 11 to 6 Ma. A recording gap on the Pacific side across the Pliocene allows a comparison again only in the late Early Pleistocene (Calabrian, 1.8 to 0.78 Ma), which shows a complete lack of shared species. These observations support the effective closure of the former Central American Seaway and emersion of the Isthmus of Panama in the intervening time. Groups that today only exist in the East Pacific were also identified in the Miocene and Pliocene of the West Atlantic, and there is also at least one instance of a genus now restricted to the West Atlantic having occurred in the East Pacific as late as the Pleistocene. The evolution of gobies in tropical America and the implications thereof are extensively discussed. Furthermore, observations of fossil gobies in the region are discussed in respect to paleoenvironmental indications and paleobiogeographic aspects. ZooBank LSID: urn:lsid:zoobank.org:pub:821F185A-DF6B-4D19-984B-E040A206C45A. https://zoobank.org/CB4D4CB4-FED2-45BF-B164-EB48286E8DB5.",
    url = "https://doi.org/10.1186/s13358-023-00302-5",
    doi = "10.1186/s13358-023-00302-5",
    openalex = "W4392506098",
    references = "doi101016s089598119900005x, doi105852ejt20228141745"
}