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Sirenians

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Journal Article
Journal: Paleobiology
Published: 01 January 2004
Paleobiology (2004) 30 (2): 297–324.
...Bruce J. MacFadden; Pennilyn Higgins; Mark T. Clementz; Douglas S. Jones Abstract Cenozoic sediments of Florida contain one of the most highly fossiliferous sequences of extinct sirenians in the world. Sirenians first occur in Florida during the Eocene (ca. 40 Ma), have their peak diversity during...
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First thumbnail for: Diets, habitat preferences, and niche differentiat...
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Journal Article
Journal: AAPG Bulletin
Published: 01 February 1973
AAPG Bulletin (1973) 57 (2): 432.
...Daryl P. Domning Abstract Sirenians are fairly common as fossils in many late Tertiary nearshore marine deposits of the West Coast. The general pattern of their evolution in the North Pacific from early Miocene to recent times is now known. With the exception of the early Miocene forms, all...
Journal Article
Published: 01 November 1964
Journal of Paleontology (1964) 38 (6): 1108–1109.
Image
Figure 4. Plot of δ13C versus δ18O for all modern sirenians sampled in this study. All measurements were made from tooth enamel carbonate. Different ecologies grade between modeled end-members of ecological variation. Modern Dugong (white diamonds) is known to be a strictly marine, seagrass feeder, and captive Trichechus (black diamonds) are strictly freshwater, C3 feeders. Wild Trichechus (gray diamonds) is known to live in either habitat, i.e., ranging between the two end-members
Published: 01 January 2004
Figure 4. Plot of δ 13 C versus δ 18 O for all modern sirenians sampled in this study. All measurements were made from tooth enamel carbonate. Different ecologies grade between modeled end-members of ecological variation. Modern Dugong (white diamonds) is known to be a strictly marine, seagrass
Journal Article
Published: 08 February 2017
Journal of Paleontology (2017) 91 (2): 337–367.
...Manja Voss; Oliver Hampe Abstract The early Oligocene (Rupelian) sirenian Halitherium schinzii Kaup, 1838, which represents the type species of the genus Halitherium Kaup, 1838, is revised herein based on a morphological re-evaluation of skeletal material originally assigned to this taxon...
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First thumbnail for: Evidence for two sympatric <span class="search-hig...
Second thumbnail for: Evidence for two sympatric <span class="search-hig...
Third thumbnail for: Evidence for two sympatric <span class="search-hig...
Journal Article
Journal: Geology
Published: 01 April 2009
Geology (2009) 37 (4): 307–310.
...Mark T. Clementz; Silvia Sorbi; Daryl P. Domning Abstract Sirenians (sea cows: manatees and dugongs) have been primary consumers in tropical and subtropical shallow-water marine ecosystems for more than 50 m.y. Though fossils of the earliest sirenians have been recovered from the Caribbean...
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First thumbnail for: Evidence of Cenozoic environmental and ecological ...
Second thumbnail for: Evidence of Cenozoic environmental and ecological ...
Journal Article
Published: 18 February 2010
Geological Magazine (2010) 147 (5): 665–673.
... of two partial atlas vertebrae, one humerus and several dorsal ribs (from Arrasate, Urbasa plateau), and partial dorsal ribs (from Lezaun, Andia plateau). The morphology of the fossils is consistent with referral to Dugongidae, the only sirenian clade known so far in the Middle Eocene of Europe. Moreover...
Journal Article
Published: 01 January 2014
Journal of Paleontology (2014) 88 (1): 109–129.
... specialization consistent with life in water. Protocetid specimens distinctly smaller and larger than those of Togocetus traversei indicate the presence of at least three protocetids at Kpogamé. Sirenian vertebral and rib pieces indicate the presence of a protosirenid and a dugongid. Finally, a vertebral centrum...
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First thumbnail for: A New Archaeocete and Other Marine Mammals (Cetace...
Second thumbnail for: A New Archaeocete and Other Marine Mammals (Cetace...
Third thumbnail for: A New Archaeocete and Other Marine Mammals (Cetace...
Book Chapter

Published: 01 December 1957
DOI: 10.1130/MEM67V1-p1223
... Members of three orders of mammals—the Sirenia, the Carnivora, and the Cetacea—are adapted in varying degrees to life in fresh, brackish and salt water. Of these the sirenians, or sea-cows are probably the most retiring, the least aggressive, and the most local in their distribution. At least...
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Published: 01 January 2004
Table 3. Stable isotopic values indicating intra-tooth variation in teeth of fossil and extant Florida sirenians
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Figure 1
Published: 08 February 2017
Figure 1 Geographic setting of sirenian sites and paleogeography during the early Oligocene of Central Europe (modified after Meulenkamp and Sissingh, 2003 ; Gürs and Janssen, 2004 ). Open asterisks indicate estimated find localities of the sympatric species
Image
A: Plot of taxonomic ranges for sirenian clades from Tethys-Mediterranean (tree). B: Plot of mean enamel δ13C values. VPDB—Vienna Peedee belemnite; FW—freshwater. C: Plot of mean enamel δ18O values. VSMOW—Vienna standard mean ocean water. D: Plot of skull measurements (width across occipital condyles) as estimate of body size for specimens of Metaxytherium spp. versus age from Tethys-Mediterranean (from Bianucci et al., 2008). In A, thick black bars show temporal ranges for groups in Tethys-Mediterranean, whereas thin black lines show temporal range for groups worldwide. Dashed lines show possible relationships between lineages. Symbols as in Figure 1 for sirenian groups. In B and C, symbols represent mean stable isotope values for each species of given age, and error bars represent ±1σ from mean values (horizontal) and age range (vertical). In B, long vertical dashed line and shaded field represent mean (±1σ) for δ13C values from all specimens. In C, solid black line and gray shaded field represent expected mean enamel δ18O values (±2 σ) for sirenians following calculations described in text. Horizontal bars at bottom of figure represent expected range in enamel δ13C values for different aquatic diets (B) and enamel δ18O values for different salinities (C) (Eocene [marine]—light gray; Neogene [marine]—dark gray). In D, gray curve is our subjective interpretation of trend in body size. Scale bar is 5 cm. Dashed horizontal lines define Messinian Age (7.24–5.33 Ma), and solid horizontal gray bar marks Messinian salinity crisis (MSC).
Published: 01 April 2009
Figure 2. A: Plot of taxonomic ranges for sirenian clades from Tethys-Mediterranean (tree). B: Plot of mean enamel δ 13 C values. VPDB—Vienna Peedee belemnite; FW—freshwater. C: Plot of mean enamel δ 18 O values. VSMOW—Vienna standard mean ocean water. D: Plot of skull measurements (width across
Journal Article
Published: 01 December 1978
Jour. Geol. Soc. India (1978) 19 (12): 571–576.
.... Sirenian rib bones have also been collected from the Eocene beds. The earliest record of fossil Sirenia from Kutch is by Grant (1840) who collected 'Some rib bones from Nummulitic limestone and marl beds. These were considered by Cleft and Owen (in Grant, 1840) to be similar to the Sirenian genus Mana/us...
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Figure 3. Simple box model of potential δ13C and δ18O end-member values of tooth enamel used to interpret, respectively, the diets and habitats of extinct Florida sirenians
Published: 01 January 2004
Figure 3. Simple box model of potential δ 13 C and δ 18 O end-member values of tooth enamel used to interpret, respectively, the diets and habitats of extinct Florida sirenians
Image
Published: 01 January 2004
Table 4. Univariate statistical data ( n , mean, standard deviation, range) for different subsets of bulk sample stable carbon and oxygen isotopic data (as discussed in the text) for the fossil and extant sirenians from Florida. See Appendix for raw data
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Figure 5. Plot of δ13C against δ18O for all teeth of Protosiren sampled in this study. Data from recent sirenians are also plotted for comparison. All measurements were made from tooth enamel carbonate
Published: 01 January 2004
Figure 5. Plot of δ 13 C against δ 18 O for all teeth of Protosiren sampled in this study. Data from recent sirenians are also plotted for comparison. All measurements were made from tooth enamel carbonate
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Figure 6. Plot of δ13C against δ18O for all teeth of Metaxytherium sampled in this study. Metaxytherium data are separated according to locality and/or age of the fossils. Data from recent sirenians are also plotted for comparison. All measurements were made from tooth enamel carbonate.
Published: 01 January 2004
Figure 6. Plot of δ 13 C against δ 18 O for all teeth of Metaxytherium sampled in this study. Metaxytherium data are separated according to locality and/or age of the fossils. Data from recent sirenians are also plotted for comparison. All measurements were made from tooth enamel carbonate.
Journal Article
Published: 26 October 2017
Geological Magazine (2019) 156 (1): 117–132.
.... The palaeomagnetic data from the samples are very unstable, except for eight from three similar sandstone levels which show a normal polarity. Matched with biostratigraphic data on rodents, primates, the selachian, sirenian and cetacean faunas, the new carbon isotope chemostratigraphy on organics (1) refines the age...
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First thumbnail for: Geology, biostratigraphy and carbon isotope chemos...
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Journal Article
Published: 26 September 2017
Geological Magazine (2018) 155 (7): 1596–1620.
... and terrestrial vertebrate fauna. Abundant and diversified chondrichthyans and archaeocete whales have been found, as well as the remains of sirenians and proboscideans. Here we describe the rest of this fossil assemblage which includes actinopterygians, turtles, palaeophiid snakes, crocodiles and pelagornithid...
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First thumbnail for: Marine vertebrate fauna from the late Eocene Samla...
Second thumbnail for: Marine vertebrate fauna from the late Eocene Samla...
Third thumbnail for: Marine vertebrate fauna from the late Eocene Samla...
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Figure 7. Plot of δ13C versus δ18O for all fossil teeth of Trichechus sampled in this study. Fossil Trichechus are separated according to the locality from which the fossil was collected. Data from recent sirenians are also plotted for comparison. All measurements were made from tooth enamel carbonate
Published: 01 January 2004
Figure 7. Plot of δ 13 C versus δ 18 O for all fossil teeth of Trichechus sampled in this study. Fossil Trichechus are separated according to the locality from which the fossil was collected. Data from recent sirenians are also plotted for comparison. All measurements were made from tooth