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Left saccular otoliths from two Recent specimens of Apogon townsendi (Breder, 1927) from off Mona Island, Lesser Antilles (Coll. IRSNB). Dorsal view of first specimen (A). Inner face of first specimen (B). Inner face of second specimen (C). Figure modified from Nolf and Bajpai (1992).
Source publication
A matched pair of otoliths (right and left saccular otoliths) and associated skeletal remains (n = 107) of Apogon townsendi (belted cardinalfish) were obtained in unconsolidated sediment from inside the valves of an articulated scallop Carolinapecten eboreus. The scallop specimen was collected in Hendry County, Florida, from the lower Pleistocene C...
Context in source publication
Context 1
... and associated skeletal remains perfectly preserved and allowed for identification. The Caloosahatchee Formation otoliths were compared with the otoliths of Recent apogonids that occur in southern Florida and the Caribbean from the IRSNB collection. They agree best with those of Apogon townsendi, which was illustrated by Nolf and Bajpai (1992) (Fig. 3). Stringer (1992) reported a similar apogonid from a late Pleistocene mudlump island in the Gulf of Mexico. Higher level taxonomy follows Nelson et al. ...
Citations
... Thompson "formations" have been combined into the Okeechobee Fm. by Scott[71], but this name is not in wide use. Based on faunal differences these have been treated as separate units in the recent paleontological literature[22,66,72,73]. ...
The Plio-Pleistocene turnover event in the western Atlantic following the closure of the Central American Seaway involved high rates of extinction for both gastropod and bivalve molluscs. This extinction was associated with declining nutrient conditions and has been presumed to be associated with a decrease in molluscan body size. Previous work which has been concordant with this expectation, however, has either focused on bivalves or not considered the effects of the recovery post extinction. In three phylogenetically diverse clades, we found that body-size evolution in gastropods across the turnover event is likely tied to ecology. One clade increased in size, one decreased, and another exhibited no substantial change. Individual species lineages exhibit a mixture of microevolutionary changes from the Pliocene to today. This study indicates that gastropod body-size evolution may be more complex than in bivalves, with ecology and other functional traits playing a significant role. Macroevolutionary processes, especially whether a clade re-radiated post extinction, were found to be important. Indeed, a low portion of extant diversity consists of survivors from clades that increased in size or have similar size distributions among their species relative to the Pliocene.
... Scott (1992) suggested grouping the latest Pliocene through Late Pleistocene Caloosahatchee, Bermont, and Fort Thompson "formations" into a single lithostratigraphic unit, the Okeechobee Fm. This proposal has not been widely adopted, however, and the traditional units continue to be treated as separate formal or informal stratigraphic units in recent literature (e.g., Harper, 2002;Dietl et al., 2004;Knowles et al., 2009;Portell and Kittle, 2010;Tao and Grossman, 2010;Scott, 2011;Stringer et al., 2017;Johnson et al., 2019) (Text- fig. 1). ...
Turritellid gastropods are among the most widespread, abundant, and diverse mollusks in Plio-Pleistocene deposits of the Atlantic coastal plain and Florida, with at least 46 species and subspecies described over almost two centuries. Yet the systematic status of these common fossil species and their phylogenetic relationships—to each other and to turritellids living today in the western Atlantic—have never been investigated in detail. We make use of recent molecular phylogenetic work on living turritellids and new analyses of shell characters to review the group from this time interval to the present in a comprehensive phylogenetic analysis and assessment of their evolutionary history in the region. We conclude that 20 fossil and two Recent species are valid. Four of these species are placed in the genus Torcula Gray, 1847; five in Caviturritella new genus, and eleven in “Turritella” sensu lato. We identify Torcula perattenuata as the likely direct ancestor of one of the two turritellid species living today off the southeastern U.S. coast, Torcula exoleta, and we elucidate the fossil record of the other extant species, “Turritella” perexilis (senior synonym of Turritella acropora). We show that Caviturritella was extirpated from the United States Gulf and Atlantic coastal plains in the Early Pleistocene but is still represented in the western Atlantic by the living species C. variegata in the southern Caribbean. We also present the first detailed treatment of Plio-Pleistocene turritellid fossils from Georgia. Our analysis shows that the PlioPleistocene Pinecrest beds of Florida contain 18 co-occurring turritellid species, which is the highest turritellid species diversity in one formation known in the fossil record.
... There are a few investigations conducted in the Gulf of Mexico and U.S. Atlantic coastal plains that are relevant to the Pliocene otolith assemblage of Alabama, and these include Fitch and Lavenberg (1983) on the Yorktown Formation (Pliocene) otoliths in North Carolina, Stringer (1992) on the Pleistocene-early Holocene teleostean otoliths in Louisiana, and Müller (1999) on the Palaeogene and Neogene elasmobranchs and teleosts (including otoliths) of the U.S. Atlantic Coastal Plain. More recent studies meaningful to the Pliocene otoliths of Alabama include Stringer et al. (2017) on the Caloosahatchee Formation (lower Pleistocene) otoliths in Florida, Stringer and Bell (2018) on seven Plio-Pleistocene sites in coastal Georgia, and Stringer and Shannon (2019) on Pliocene otoliths from southern North Carolina. The study of Stringer and Bell (2018) identified an otolith assemblage of 50 taxa present in the Plio-Pleistocene of Georgia; many of these same taxa are also present in the Dauphin Island otolith assemblage. ...
The first Pliocene teleostean otoliths from the Gulf Coastal Plain are described from Dauphin Island, Mobile County, Alabama, USA. The 250 otolith specimens, mainly sagittae, were obtained from shell hash dredged from an offshore Pliocene unit deposited onshore as part of recent beach nourishment. Analysis of the otoliths revealed 22 species from 11 teleostean families. Sciaenid fishes dominate the assemblage and account for 79.6% of the total specimens, while the other 10 families (including indeterminates) comprise approximately 20% of the total. Comparison to modern biological and ecological requirements for the fishes represented by the otoliths suggest a shallow (0–20 m) neritic environment with some brackish and rare deep-water influence. Several of the most abundant taxa indicate shallow, soft bottom estuarine habitat with upstream oligohaline creeks (0.5 to 5.0 ppt salinity) serving as primary nursery area. However, the percentage of marine-only species may indicate more interaction with open estuary and shallow coastal areas and subtropical waters. The lack of invertebrate settlement on the otoliths likely indicates limited surface residence-time. All 22 taxa recovered from the Dauphin Island site are highly significant since they represent the first Pliocene occurrences of these taxa within the Gulf Coastal Plain of North America.
... These studies are of minimal value for the investigation of Pleistocene otoliths of coastal Georgia. The only Pleistocene otolith studies for the entire Gulf and Atlantic coastal plains are Stringer (1992); Stringer et al. (2017); Stringer and Bell (2018), which is the only published study of Georgia Pleistocene otolith assemblages; and Stringer and Shannon (2019). ...
Investigation of teleostean otoliths (n = 418) recovered from the late Pleistocene (Rancholabrean) Jones Girls Site, Chatham County, Georgia, represents just the second study of Pleistocene otoliths in Georgia and only the fifth study of Pleistocene otoliths for the Atlantic and Gulf coastal plains. Geochronologic analysis suggests an age from 80 Ka to 130 Ka for the site. Otoliths indicate 18 extant taxa (10 families) with sciaenids
dominant. Otoliths provide seven additional fish taxa (six families) for the Georgia late Pleistocene. Otoliths point to a neritic coastal environment (< 20 m) with strong evidence for soft bottom, estuarine creeks, and bays with no large freshwater input. The fish represented by otoliths indicate temperatures and conditions similar to present-day coastal Georgia.
... However, the examination of Pliocene otoliths in the United States, especially the Atlantic and Gulf coastal plains, is extremely limited. Atlantic and Gulf coast studies of Pliocene otoliths consist of only five studies: Fitch and Lavenberg (1983), Stringer (1992), Müller (1999), Stringer et al. (2017), Stringer and Bell (2018). Of these, only two major investigations involving Pliocene otoliths in North Carolina have been conducted (Fitch and Lavenberg 1983;Müller 1999). ...
Bulk sampling of Pliocene (2.5–3.1 Ma, Piacenzian) beds at the Elizabethtown locality (Bladen County, North Carolina) produced 745 teleostean otoliths (17 taxa, representing extant fish off the U.S. Atlantic coast). Sciaenids dominate the assemblage (8 taxa; 44.4% of the total) and account for an extremely large percentage of total specimens (93.2%). The number of species (richness) at Elizabethtown is relatively small, and percentage abundance indicates a very large unevenness with Micropogonias undulatus and Leiostomus aff. L. xanthurus (91.4% of the specimens). Otolith assemblages from Elizabethtown and Lee Creek Mine, one of the most extensively studied North Carolina Pliocene sites, were compared. Assemblages were extremely dissimilar (percentage similarity measurement of 3.3%). Modern distributions of M.undulatus and L. aff. L.xanthurus are very strong indicators of shallow, soft bottom estuarine creeks and bays. The preponderance of juvenile M.undulatus (99.5% represent 1-year-old or less) is a strong indicator for a primary nursery area. This specialised habitat explains the dominance of juvenile Atlantic croakers and spots, the high percentage of fishes distributed in freshwater, brackish, and marine environments, and the paucity of marine-only species. The specialised habitat indicated at Elizabethtown would also account for the pronounced difference between the Elizabethtown and Lee Creek otolith assemblages.
... The authors reported unidentified otoliths as present at the Isle of Hope and Jones Girls sites. Most recently, Stringer et al. (2017) described a matched pair of otoliths and associated skeletal remains from Apogon townsendi from the Caloosahatchee Formation (early Pleistocene) of Florida. ...
Extensive bulk sampling at seven Plio-Pleistocene sites spanning approximately 4.5 Ma to 120,000 years ago in age near Brunswick, Glynn County, Georgia, produced 1,803 teleostean otoliths. The otolith assemblage was relatively diverse with 50 taxa (representing 18 families) of Plio-Pleistocene teleosts. The otoliths represented mainly shallow-marine fishes, which were all extant except for four species. The assemblage was dominated by 16 sciaenid taxa that represented 65.8% of the total number of otoliths. The Plio-Pleistocene otoliths indicated fishes that are almost identical to the marine fishes from present-day coastal Georgia. The teleostean otoliths are considered especially important for several reasons. This study represents the first description of fish otoliths from the Plio-Pleistocene of coastal Georgia and describes the bony fishes present from approximately 4.5 Ma (Raysor Marl equivalent) to 120,000 years ago (late Pleistocene). This time interval includes the late Neogene climatic changes as well as the glacial-interglacial climatic cycles in North America. Also, the preservation of aragonitic otoliths is rare in coastal Georgia given the very high water table and the intense and rapid weathering. Furthermore, there is a paucity of Plio-Pleistocene fossils, especially bony fishes, in coastal Georgia related to various geological constraints such as highly erosive transgressive sequences. The Plio-Pleistocene otolith assemblage from coastal Georgia contains 13 families representing 28 taxa not recognized by skeletal fossils in Georgia. Although the Ariidae and Sciaenidae were previously recognized based on skeletal fossil material in Georgia, there are 14 newly reported taxa based on otoliths in these families (1 and 13 respectively) including Protosciaena kirbyorum n. sp., the first fossil species of this genus in the U.S. Otolith data also verified fishes previously indicated by skeletal remains and provided greater specificity in several cases.
Isolated elasmobranch and teleost teeth, jaws, otoliths, scales, vertebrae, and fin spines were recovered from the upper Oligocene (Chattian) Catahoula Formation in Wayne County, Mississippi, USA. A total of 13 551 specimens were examined and 12 340 of these were identified at least to the ordinal level. These remains represent 49 unequivocal fish taxa, viz. 29 elasmobranchs and 20 teleosts. The 3614 elasmobranch remains indicate that Carcharhiniformes is the most diverse group of Elasmobranchii, with 12 taxa belonging to five families. Orectolobiformes and Lamniformes are represented by far fewer taxa (three and four, respectively). Carcharhinus acuarius (Probst, 1879) constitutes 49% of the total number of shark teeth in our sample. Ten batoids have been identified within Myliobatiformes (seven taxa) and Rhinopristiformes (three taxa). Partial teeth of durophagous myliobatids (three genera) are the most abundant batoid remains, constituting 41% of the total number of ray fossils. However, teeth of Dasyatidae and Rhynchobatus cf. pristinus (Probst, 1877) are abundant and represent 36.5% and 15.4%, respectively, of the specimens identified. Herein, we erect five new elasmobranch taxa, including Galeocerdo platycuspidatum sp. nov., Hemipristis intermedia sp. nov., Hypanus? heterodontus sp. nov., “Sphyrna” gracile sp. nov., and “Sphyrna” robustum sp. nov. The Catahoula Formation sample includes over 9935 teleost fossils, which constitutes 73% of the total fish sample. Nine bony fish taxa are represented solely by teeth, jaw elements, or fin spines. Although otoliths are much less common than the other identifiable remains (409 versus roughly 8430, respectively), they allowed us to identify four taxa not known from other skeletal remains. Albulidae, Sciaenidae, and Sparidae are represented by isolated teeth, jaw elements, and otoliths, but we could not ascertain whether the various teeth and jaw elements are conspecific with the otolith-based species we identified. The remains of Sciaenidae (teeth, jaw elements, otoliths) dominate the Catahoula Formation bony fish assemblage, constituting 70% of the teleost specimens identified at least to the ordinal level. Our sample includes the first Oligocene occurrence of Tetraodontidae in the Western Hemisphere. The vertebrate assemblage within the Catahoula Formation at the study site indicates an estuarine depositional environment, which is consistent with previous interpretations based on lithology. At the study site the Catahoula Formation disconformably overlies the Paynes Hammock Limestone, and we believe the disconformable contact locally represents the Rupelian (early Oligocene)/Chattian (late Oligocene) boundary. The fish fauna described herein is therefore of Chattian age.
Large and diverse Eocene otolith assemblages have been described from the US Gulf and Atlantic coastal plains, various basins in Europe, and New Zealand. Here we described a highly diverse otolith association from the middle Eocene (Lutetian and Bartonian) strata of southern California, San Diego County, which was retrieved
from the heritage of John E. Fitch (1918-1982) in the archives of the Ichthyology Department of the Natural History Museum of Los Angeles County, Los Angeles, Califronia. The collection represents the first Eocene otolith assemblage described from the Northeastern Pacific and stems from two localities: the Ardath Shale at Black’s Beach in the Torrey Pines Park just south of Black’s Canyon Road and north of the Salk Fault on the Pacific shore face, and the MissionValley Formation from the west-facing graded hill just east of the Miramar Water Treatment Plant
near the southern shore of Miramar Reservoir. The Ardath Shale was deposited on the deep shelf and continental slope while the Mission Valley Formation represent an inland, nearshore environment during times of the maximum transgression.
A total of more than15,000 otoliths were found representing 96 species of which 53 are described as new and 12 remain in open nomenclature. The fauna of the Ardath Shale is distinctly richer containing 88 species while the one from the Miramar Reservoir site yielded 38 species. The low diversity at the Miramar Reservoir site is thought to be related to the shallow-water environment in which it was deposited whereas the high diversity at Black’s Beach reflects a mixture of shelf and bathyal fishes. In addition, 24 new otolith-based genera are established, four of which are in the category “incertae sedis”. Furthermore, five new species are described from a comparative otolith collection from the US Gulf Coast Eocene and one new species from a comparative collection from the Lutetian of Balegem in Belgium.
The Eocene otolith-based fish fauna from California is assessed for its paleoecological, paleobiogeographic and evolutionary significance. Particular emphasis is directed towards the elucidation of the evolution of the early
Ophidiiformes, which during the early Paleogene were predominantly adapted to warm, clastic shallow-water environments and there were competing in abundance and diversity with other percomorphs (e.g., perciforms s.l.). A warm Eocene paleobioprovince is proposed for the Californian fish fauna which is not related to today’s endemic Northwest Pacific fish fauna along the regime of the cold-water California Current.
The Oligocene (Rupelian) Byram Formation (Vicksburg Group) in Alabama, USA, is divided into three members, including (in ascending order) the Glendon Limestone, unnamed marl, and the Bucatunna Clay. The Oligocene marine units in Alabama have been historically under-investigated, but bulk samples re-cently obtained from Glendon Limestone Member exposures at site AWa-9 in Washington County yielded 20 unequivocal elasmobranch and teleost taxa. This surprisingly diverse paleofauna, based on isolated teeth, bones and otoliths, includes the new taxon, Gobiosoma? axsmithi sp. nov., as well as “Aetomylaeus” sp., Albula sp., Aplodinotus gemma Koken, 1888, Ariosoma nonsector Nolf and Stringer, 2003, Balistidae indet., Citharichthys sp., Myliobatoidei indet., Diretmus? sp., Hemipristis sp., Negaprion aff. N. gilmorei (Leriche, 1942), Pachyscyllium sp., Paralbula sp., Physogaleus sp., Preophidion meyeri (Koken, 1888), Sciaena pseu-doradians (Dante and Frizzell in Frizzell and Dante, 1965), Sciaenops? sp., Sparus? elegantulus Koken, 1888, Sphyraena sp., and Syacium sp. Additional remains were recovered but could not be identified beyond unde-termined Elasmobranchii or Teleostei. All these taxa represent first occurrences within the Glendon Limestone Member in Alabama, and the “Aetomylaeus” sp., Pachyscyllium sp., Paralbula sp., and Sciaenops? sp. spec-imens represent the first occurrences of each in the Oligocene of the Gulf Coastal Plain of the USA. Wealso report the first record of Oligocene Paralbula Blake, 1940 teeth, and the first occurrence of an Oligocene member of the Balistidae in the Western Hemisphere. This marine vertebrate assemblage indicates that the Glendon Limestone Member at site AWa-9 represented a subtropical to temperate, middle shelf paleoenviron-ment with a paleowater depth interpreted as 30–100 m.
