Revision as of 19:19, 22 October 2023 editCommonsDelinker (talk | contribs)Bots, Template editors1,017,947 edits Replacing Greenandorange_pog.svg with File:Green-orange_pog.svg (by CommonsDelinker because: File renamed: Criterion 4 (harmonizing names of file set) · in [[:c::Category:Map pointers, d← Previous edit |
Latest revision as of 12:15, 30 December 2024 edit undoJunsik1223 (talk | contribs)Extended confirmed users6,791 edits →Theropods: the specimens are actually identified as cf. V. iaai and cf. P. gregorii in the study |
(44 intermediate revisions by 21 users not shown) |
Line 10: |
Line 10: |
|
| namedfor = López de Bertodano Bay |
|
| namedfor = López de Bertodano Bay |
|
| namedby = |
|
| namedby = |
|
| region = ], ] |
|
| region = ], ], ] |
|
| country = ] |
|
| country = ] |
|
| coordinates = {{coord|64.0|S|57.4|W|display=inline,title}} |
|
| coordinates = {{coord|64.0|S|57.4|W|display=inline,title}} |
Line 39: |
Line 39: |
|
== Cretaceous-Paleogene boundary == |
|
== Cretaceous-Paleogene boundary == |
|
], ] with the Lopez de Bertodano Formation in light green, the locations where the ] is exposed are indicated]] |
|
], ] with the Lopez de Bertodano Formation in light green, the locations where the ] is exposed are indicated]] |
|
The ] (K–Pg) crops out on ] in the upper levels of the Lopez de Bertodano Formation.<ref name="Zinsmeister">{{cite journal |author1=Zinsmeister, W.J. |title=Discovery of fish mortality horizon at the K-T Boundary on Seymour Island: Re-evaluation of events at the end of the Cretaceous |year=1998 |journal=Journal of Paleontology |volume=72 |issue=3 |pages=556–571 |url=https://www.cambridge.org/core/journals/journal-of-paleontology/article/discovery-of-fish-mortality-horizon-at-the-k-t-boundary-on-seymour-island-re-evaluation-of-events-at-the-end-of-the-cretaceous/C6F72A86DAB664F2E2315A34B3875875|doi=10.1017/S0022336000024331 |s2cid=132206016 }}</ref> A small (but significant) ] anomaly occurs at the boundary on Seymour Island, as at lower latitudes, thought to be fallout from the ] in the ].<ref name="Elliot">{{cite journal |author1=Elliot D.H. |title=Iridium and dinocysts at the Cretaceous-Tertiary boundary on Seymour Island, Antarctica: Implications for the K-T event |year=1994 |journal=Geology |volume=22 |issue=8 |doi=10.1130/0091-7613(1994)022<0675:IADATC>2.3.CO;2 |author2=Askin RA |author3=Kyte FT |author4=Zinsmeister WJ |page=675|bibcode=1994Geo....22..675E }}</ref> Directly above the boundary a layer of disarticulated fish ]s occurs, victims of a disturbed ecosystem immediately following the impact event.<ref name="Zinsmeister"/> Multiple reports have described evidence for climatic changes in ] prior to the ],<ref name="Petersen">{{cite journal |author1=Petersen, S.V. |title=End-Cretaceous extinction in Antarctica linked to both Deccan volcanism and meteorite impact via climate change |year=2016 |journal=Nature Communications |volume=7 |doi=10.1038/ncomms12079|pmid=27377632 |pmc=4935969 |author2=Dutton A |author3=Lohmann KC |page=12079|bibcode=2016NatCo...712079P }}</ref> but the extent to which these affected marine ] is debated. Based on extensive marine fossil collections from Seymour Island, recent work has confirmed that a single and severe ] event occurred at this time in Antarctica just as at lower latitudes.<ref name="Witts">{{cite journal |author1=Witts J.D. |title=Macrofossil evidence for a rapid and severe Cretaceous-Paleogene mass extinction in Antarctica |year=2016 |journal=Nature Communications |volume=7 |doi=10.1038/ncomms11738 |author2=Whittle RJ |author3=Wignall PB |author4=Crame JA |author5=Francis JE |author6=Newton RJ |author7=Bowman VC |pmid=27226414 |pmc=4894978 |page=11738|bibcode=2016NatCo...711738W }}</ref> |
|
The ] (K–Pg) crops out on ] in the upper levels of the Lopez de Bertodano Formation.<ref name="Zinsmeister">{{cite journal |author1=Zinsmeister, W.J. |title=Discovery of fish mortality horizon at the K-T Boundary on Seymour Island: Re-evaluation of events at the end of the Cretaceous |year=1998 |journal=Journal of Paleontology |volume=72 |issue=3 |pages=556–571 |url=https://www.cambridge.org/core/journals/journal-of-paleontology/article/discovery-of-fish-mortality-horizon-at-the-k-t-boundary-on-seymour-island-re-evaluation-of-events-at-the-end-of-the-cretaceous/C6F72A86DAB664F2E2315A34B3875875|doi=10.1017/S0022336000024331 |bibcode=1998JPal...72..556Z |s2cid=132206016 }}</ref> A small (but significant) ] anomaly occurs at the boundary on Seymour Island, as at lower latitudes, thought to be fallout from the ] in the ].<ref name="Elliot">{{cite journal |author1=Elliot D.H. |title=Iridium and dinocysts at the Cretaceous-Tertiary boundary on Seymour Island, Antarctica: Implications for the K-T event |year=1994 |journal=Geology |volume=22 |issue=8 |doi=10.1130/0091-7613(1994)022<0675:IADATC>2.3.CO;2 |author2=Askin RA |author3=Kyte FT |author4=Zinsmeister WJ |page=675|bibcode=1994Geo....22..675E }}</ref> Directly above the boundary a layer of disarticulated fish ]s occurs, victims of a disturbed ecosystem immediately following the impact event.<ref name="Zinsmeister"/> Multiple reports have described evidence for climatic changes in ] prior to the ],<ref name="Petersen">{{cite journal |author1=Petersen, S.V. |title=End-Cretaceous extinction in Antarctica linked to both Deccan volcanism and meteorite impact via climate change |year=2016 |journal=Nature Communications |volume=7 |doi=10.1038/ncomms12079|pmid=27377632 |pmc=4935969 |author2=Dutton A |author3=Lohmann KC |page=12079|bibcode=2016NatCo...712079P }}</ref> but the extent to which these affected marine ] is debated. Based on extensive marine fossil collections from Seymour Island, recent work has confirmed that a single and severe ] event occurred at this time in Antarctica just as at lower latitudes.<ref name="Witts">{{cite journal |author1=Witts J.D. |title=Macrofossil evidence for a rapid and severe Cretaceous-Paleogene mass extinction in Antarctica |year=2016 |journal=Nature Communications |volume=7 |doi=10.1038/ncomms11738 |author2=Whittle RJ |author3=Wignall PB |author4=Crame JA |author5=Francis JE |author6=Newton RJ |author7=Bowman VC |pmid=27226414 |pmc=4894978 |page=11738|bibcode=2016NatCo...711738W }}</ref> |
|
|
|
|
|
{{clearleft}} |
|
{{clear left}} |
|
|
|
|
|
==Climate== |
|
==Climate== |
|
During the Maastrichtian, Seymour Island was located within the Antarctic ] at around ~65°S latitude.<ref name=Kempetal>{{cite journal|author1=David B. Kemp|author2=Stuart A. Robinson|author3=J. Alistair Crame|author4=Jane E. Francis|author5=Jon Ineson|author6=Rowan J. Whittle|author7=Vanessa Bowman|author8=Charlotte O'Brien|title=A cool temperate climate on the Antarctic Peninsula through the latest Cretaceous to early Paleogene|year=2014|journal=Geology|volume=42|issue=7|pages=583–586|doi=10.1130/g35512.1|bibcode=2014Geo....42..583K|doi-access=free}}</ref> Chemical studies on ] isotopes found in shells and benthic ] have calculated intermediate-depth and deep-sea ocean temperatures at a mean average of {{convert|6|C|F|sp=us}} with fluctuations of {{convert|4–12|C|F|sp=us}} throughout the Maastrichtian; one of the same studies has also suggested that sea surface temperatures may have been colder, possibly dropping below freezing and forming sea ice at times.<ref name=Bowmanetal>{{cite journal|author1=Vanessa C. Bowman|author2=Jane E. Francis|author3=James B. Riding|title=Late Cretaceous winter sea ice in Antarctica?|journal=Geology|year=2013|volume=41|issue=12|pages=1227–1230|doi=10.1130/G34891.1|bibcode=2013Geo....41.1227B|s2cid=128885087 |url=http://nora.nerc.ac.uk/id/eprint/504369/1/sea%20ice%20%20revised%20Jim%20edit.pdf}}</ref><ref name=Tobinetal>{{cite journal|author1=Thomas S. Tobin|author2=Peter D. Ward|author3=Eric J. Steig|author4=Eduardo B. Olivero|author5=Isaac A. Hilburn|author6=Ross N. Mitchell|author7=Matthew R. Diamond|author8=Timothy D. Raub|author9=Joseph L. Kirschvink|title=Extinction patterns, δ18 O trends, and magnetostratigraphy from a southern high-latitude Cretaceous–Paleogene section: Links with Deccan volcanism|journal=Palaeogeography, Palaeoclimatology, Palaeoecology|year=2012|volume=350–352|issue=2012|pages=180–188|doi=10.1016/j.palaeo.2012.06.029|bibcode=2012PPP...350..180T|url=https://authors.library.caltech.edu/35186/2/mmc1.doc}}</ref> Alternatively, a study using data acquired from ancient bacterial membrane lipids yielded a slightly warmer temperature of {{convert|12|±|5|C}} around 66 Ma. Nevertheless, these estimated climates characterize primarily cool temperate environments with possible subpolar and warm episodes.<ref name=Kempetal /> |
|
During the Maastrichtian, Seymour Island was located within the Antarctic ] at around ~65°S latitude.<ref name=Kempetal>{{cite journal|author1=David B. Kemp|author2=Stuart A. Robinson|author3=J. Alistair Crame|author4=Jane E. Francis|author5=Jon Ineson|author6=Rowan J. Whittle|author7=Vanessa Bowman|author8=Charlotte O'Brien|title=A cool temperate climate on the Antarctic Peninsula through the latest Cretaceous to early Paleogene|year=2014|journal=Geology|volume=42|issue=7|pages=583–586|doi=10.1130/g35512.1|bibcode=2014Geo....42..583K|doi-access=free|hdl=2164/4380|hdl-access=free}}</ref> Chemical studies on ] isotopes found in shells and benthic ] have calculated intermediate-depth and deep-sea ocean temperatures at a mean average of {{convert|6|C|F|sp=us}} with fluctuations of {{convert|4–12|C|F|sp=us}} throughout the Maastrichtian; one of the same studies has also suggested that sea surface temperatures may have been colder, possibly dropping below freezing and forming sea ice at times.<ref name=Bowmanetal>{{cite journal|author1=Vanessa C. Bowman|author2=Jane E. Francis|author3=James B. Riding|title=Late Cretaceous winter sea ice in Antarctica?|journal=Geology|year=2013|volume=41|issue=12|pages=1227–1230|doi=10.1130/G34891.1|bibcode=2013Geo....41.1227B|s2cid=128885087 |url=http://nora.nerc.ac.uk/id/eprint/504369/1/sea%20ice%20%20revised%20Jim%20edit.pdf}}</ref><ref name=Tobinetal>{{cite journal|author1=Thomas S. Tobin|author2=Peter D. Ward|author3=Eric J. Steig|author4=Eduardo B. Olivero|author5=Isaac A. Hilburn|author6=Ross N. Mitchell|author7=Matthew R. Diamond|author8=Timothy D. Raub|author9=Joseph L. Kirschvink|title=Extinction patterns, δ18 O trends, and magnetostratigraphy from a southern high-latitude Cretaceous–Paleogene section: Links with Deccan volcanism|journal=Palaeogeography, Palaeoclimatology, Palaeoecology|year=2012|volume=350–352|issue=2012|pages=180–188|doi=10.1016/j.palaeo.2012.06.029|bibcode=2012PPP...350..180T|url=https://authors.library.caltech.edu/35186/2/mmc1.doc}}</ref> Alternatively, a study using data acquired from ancient bacterial membrane lipids yielded a slightly warmer temperature of {{convert|12|±|5|C}} around 66 Ma. Nevertheless, these estimated climates characterize primarily cool temperate environments with possible subpolar and warm episodes.<ref name=Kempetal /> |
|
|
|
|
|
== Fossil content == |
|
== Fossil content == |
|
The Lopez de Bertodano Formation has provided many fossils of ], ]s and ]s.<ref name=FWLdB1> at ].org</ref><ref name=FWLdB2> at ].org</ref><ref name=FWLdB3> at ].org</ref> Also the first fossil egg from Antarctica, '']'', was found in the formation.<ref name=Legendre2020>Legendre et al., 2020</ref> |
|
The Lopez de Bertodano Formation has provided many fossils of ], ]s and ]s.<ref name=FWLdB1> at ].org</ref><ref name=FWLdB2> at ].org</ref><ref name=FWLdB3> at ].org</ref> Also the first fossil egg from Antarctica, '']'', was found in the formation.<ref name=Legendre2020>Legendre et al., 2020</ref> |
|
|
|
|
|
Dinosaur remains are among the fossils that have been recovered from the formation<ref name="cretaceousdistribution">Weishampel, David B; et al. (2004). "Dinosaur distribution (Late Cretaceous, Antarctica)." In: Weishampel, David B.; Dodson, Peter; and Osmólska, Halszka (eds.): The Dinosauria, 2nd, Berkeley: University of California Press. p. 606. {{ISBN|0-520-24209-2}}.</ref> and include at least two and probably as much as six lineages of indisputably ]: one related to ], a primitive ] or related form, 1 to 2 species of possible ]s, a large and possibly ] belonging to a lineage extinct today<!-- need to determine whether this was not a Pelagornithidae --> as well as a partial ] that might belong to either of the smaller species or represent yet another one. The formation also contains a rich fossil ] fauna, including ]s, ]s,<ref name="Crame">{{cite journal |author1=Crame, J.A. |title=The Early Origin of the Antarctic Marine Fauna and Its Evolutionary Implications |year=2014 |journal=PLOS ONE |volume=7 |issue=12 |doi=10.1371/journal.pone.0114743 |pmid=25493546 |pmc=4262473 |author2=Beu, A.G. |author3=Ineson J.R. |author4=Francis J.A. |author5=Whittle R.J. |author6=Bowman V.C. |page=e114743|bibcode=2014PLoSO...9k4743C |doi-access=free }}</ref> and ]s (]s and ]s).<ref name="Witts15">{{cite journal |author1=Witts, J.D. |title=Evolution and extinction of Maastrichtian (Late Cretaceous) cephalopods from the López de Bertodano Formation, Seymour Island, Antarctica |year=2015 |journal=Palaeogeography, Palaeoclimatology, Palaeoecology |volume=418 |pages=193–212 |doi=10.1016/j.palaeo.2014.11.002 |author2=Bowman V.C. |author3=Wignall P.B. |author4=Crame J.A. |author5=Francis, J.E. |author6=Newont, R.J.|bibcode=2015PPP...418..193W |url=http://nora.nerc.ac.uk/id/eprint/507013/1/Evolution%20and%20extinction%20of%20Maastrichtian%20%28Late%20Cretaceous%29%20cephalopods%20AAM.pdf }}</ref> |
|
Dinosaur remains are among the fossils that have been recovered from the formation<ref name="cretaceousdistribution">Weishampel, David B; et al. (2004). "Dinosaur distribution (Late Cretaceous, Antarctica)." In: Weishampel, David B.; Dodson, Peter; and Osmólska, Halszka (eds.): The Dinosauria, 2nd, Berkeley: University of California Press. p. 606. {{ISBN|0-520-24209-2}}.</ref> and include at least two and probably as much as six lineages of indisputably ]: one related to ], a primitive ] or related form, 1 to 2 species of possible ]s, a large and possibly ] belonging to a lineage extinct today<!-- need to determine whether this was not a Pelagornithidae --> as well as a partial ] that might belong to either of the smaller species or represent yet another one. The formation also contains a rich fossil ] fauna, including ]s, ]s,<ref name="Crame">{{cite journal |author1=Crame, J.A. |title=The Early Origin of the Antarctic Marine Fauna and Its Evolutionary Implications |year=2014 |journal=PLOS ONE |volume=7 |issue=12 |doi=10.1371/journal.pone.0114743 |pmid=25493546 |pmc=4262473 |author2=Beu, A.G. |author3=Ineson J.R. |author4=Francis J.A. |author5=Whittle R.J. |author6=Bowman V.C. |page=e114743|bibcode=2014PLoSO...9k4743C |doi-access=free }}</ref> and ]s (]s and ]s).<ref name="Witts15">{{cite journal |author1=Witts, J.D. |title=Evolution and extinction of Maastrichtian (Late Cretaceous) cephalopods from the López de Bertodano Formation, Seymour Island, Antarctica |year=2015 |journal=Palaeogeography, Palaeoclimatology, Palaeoecology |volume=418 |pages=193–212 |doi=10.1016/j.palaeo.2014.11.002 |author2=Bowman V.C. |author3=Wignall P.B. |author4=Crame J.A. |author5=Francis, J.E. |author6=Newont, R.J.|bibcode=2015PPP...418..193W |url=http://nora.nerc.ac.uk/id/eprint/507013/1/Evolution%20and%20extinction%20of%20Maastrichtian%20%28Late%20Cretaceous%29%20cephalopods%20AAM.pdf }}</ref> |
|
|
|
|
|
The fish assemblage of the López de Bertodano Formation was dominated by ''Enchodus'' and ichthyodectiformes, accounting for 21.95% and 45.6% of local fish diversity respectively. Of the remaining percentages, sand sharks made up 10.5%, the cow shark '']'' 6.8%, ]s 3.9%, ]s 2.7%, various other ] 2.4%, and the remaining 6% were shared between other sharks like '']'', ], '']'', and ''Cretalamna''.<ref name=Cioneetal2018>{{cite journal|author1=Alberto L. Cione|author2=Sergio Santillana|author3=Soledad Gouiric-Cavalli|author4=Carolina Acosta Hospitaleche|author5=Javier N. Gelfo|author6=Guillermo M. Lopez|author7=Marcelo Reguero|title=Before and after the K/Pg extinction in West Antarctica: New marine fish records from Marambio (Seymour) Island|year=2018|journal=Cretaceous Research|volume=85|pages=250–265|doi=10.1016/j.cretres.2018.01.004|url=http://sedici.unlp.edu.ar/handle/10915/147537 }}</ref> |
|
The fish assemblage of the López de Bertodano Formation was dominated by ''Enchodus'' and ichthyodectiformes, accounting for 21.95% and 45.6% of local fish diversity respectively. Of the remaining percentages, sand sharks made up 10.5%, the cow shark '']'' 6.8%, ]s 3.9%, ]s 2.7%, various other ] 2.4%, and the remaining 6% were shared between other sharks like '']'', ], '']'', and ''Cretalamna''.<ref name=Cioneetal2018>{{cite journal|author1=Alberto L. Cione|author2=Sergio Santillana|author3=Soledad Gouiric-Cavalli|author4=Carolina Acosta Hospitaleche|author5=Javier N. Gelfo|author6=Guillermo M. Lopez|author7=Marcelo Reguero|title=Before and after the K/Pg extinction in West Antarctica: New marine fish records from Marambio (Seymour) Island|year=2018|journal=Cretaceous Research|volume=85|pages=250–265|doi=10.1016/j.cretres.2018.01.004|bibcode=2018CrRes..85..250C |url=http://sedici.unlp.edu.ar/handle/10915/147537 |hdl=11336/99687|hdl-access=free}}</ref> |
|
|
|
|
=== Dinosaurs === |
|
|
|
=== Vertebrates === |
|
|
==== Dinosaurs ==== |
|
|
|
|
|
{{paleobiota-key-compact}} |
|
|
===== Ornithischians ===== |
|
|
|
|
{| class="wikitable" align="center" |
|
{| class="wikitable" align="center" |
|
|- |
|
|- |
|
! colspan="6" align="center" | ''']s''' recorded from Lopez de Bertodano Formation |
|
! colspan="6" align="center" | ''']s''' recorded from Lopez de Bertodano Formation |
|
|- |
|
|- |
|
! Genus |
|
! Genus |
|
! Species |
|
! Species |
|
! Member |
|
! Member/Location |
|
! Material |
|
! Material |
|
! Description |
|
! Description |
|
! Image |
|
! Image |
|
|- |
|
|- |
|
| rowspan="2" | '']'' |
|
| rowspan="2" |] |
|
|
|Indeterminate |
|
|
|Sandwich Bluff Member |
|
|
|CM 93790, right prox. Metatarsal II; Rt. Prox. Metatarsal IV; left. Prox. Fibula <ref name=":0" /> |
|
|
| |
|
|
| |
|
|
|- |
|
|
|Indeterminate |
|
|
|Sandwich Bluff Member |
|
|
|MLP 98-I-10-70, pedal ungual<ref name=":0" /> |
|
|
|Also considered Ornithischia Indet |
|
|
| |
|
|
|- |
|
|
| rowspan="2" | ] |
|
|
| Indeterminate |
|
|
| Sandwich Bluff, Vega Island |
|
|
| Isolated cheek tooth, MLP 98-I-10-1.<ref>{{Cite journal |last=Case |first=Judd A. |last2=Martin |first2=James E. |last3=Chaney |first3=Dan S. |last4=Reguero |first4=Marcelo |last5=Marenssi |first5=Sergio A. |last6=Santillana |first6=Sergio M. |last7=Woodburne |first7=Michael O. |date=2000-09-25 |title=The first duck-billed dinosaur (Family Hadrosauridae) from Antarctica |url=http://dx.doi.org/10.1671/0272-4634(2000)0202.0.co;2 |journal=Journal of Vertebrate Paleontology |volume=20 |issue=3 |pages=612–614 |doi=10.1671/0272-4634(2000)0202.0.co;2 |issn=0272-4634|hdl=11336/105444 |hdl-access=free }}</ref> |
|
|
| rowspan="2" |The 1st Hadrosaur remains of Antarctica |
|
|
| rowspan="2" | |
|
|
|- |
|
|
|Indeterminate |
|
|
|Seymour Island |
|
|
|MLP 96-1-6-2, Distal end of metatarsal<ref>{{Cite journal |last=Rich |first=T. H. |last2=Vickers-Rich |first2=P. |last3=Fernandez |first3=M. |last4=Santillana |first4=S. |date=1999 |title=A probable hadrosaur from Seymour Island, Antarctic Peninsula. |url=https://www.researchgate.net/publication/274780002_A_PROBABLE_HADROSAUR_FROM_SEYMOUR_ISLAND_ANT_ARCTIC_PENINSULA |journal=Proceedings of the Second Gondwanan Dinosaur Symposium, National Science Museum Monographs |volume=15 |pages=219-222}}</ref> |
|
|
|- |
|
|
|] |
|
|
|Indeterminate |
|
|
|Sandwich Bluff Member |
|
|
|Right pedal ungual IV, CM93791, and osteoderm<ref name=":0" /> |
|
|
| |
|
|
| |
|
|
|} |
|
|
|
|
|
===== Theropods ===== |
|
|
{| class="wikitable" align="center" |
|
|
|- |
|
|
! colspan="6" align="center" | ''']s''' recorded from Lopez de Bertodano Formation |
|
|
|- |
|
|
! Genus |
|
|
! Species |
|
|
! Member/Location |
|
|
! Material |
|
|
! Description |
|
|
! Image |
|
|
|- |
|
|
| ]<ref>{{cite journal | last1 = Cordes | year = 2002 | title = A new charadriiform avian specimen from the Early Maastrichtian of Cape Lamb, Vega Island, Antarctic Peninsula | journal = Journal of Vertebrate Paleontology | volume = 22 | issue = 3| page = 46A }}</ref> |
|
|
| Indeterminate |
|
|
| Cape Lamb |
|
|
| Partial skeleton |
|
|
| |
|
|
| align=center | <!--Image--> |
|
|
|- |
|
|
| '']''<ref>{{Cite journal |last=Tambussi |first=Claudia P |last2=Degrange |first2=Federico J |last3=De Mendoza |first3=Ricardo S |last4=Sferco |first4=Emilia |last5=Santillana |first5=Sergrio |date=2019-01-09 |title=A stem anseriform from the early Palaeocene of Antarctica provides new key evidence in the early evolution of waterfowl |url=http://dx.doi.org/10.1093/zoolinnean/zly085 |journal=Zoological Journal of the Linnean Society |volume=186 |issue=3 |pages=673–700 |doi=10.1093/zoolinnean/zly085 |issn=0024-4082}}</ref> |
|
|
| ''C. antarcticus'' |
|
|
| Seymour Island |
|
|
| MLP 07-III-1-1, a three-dimensionally preserved, partly complete skeleton |
|
|
| An ] |
|
|
| align=center | ] |
|
|
|- |
|
|
|] |
|
|
|Indeterminate |
|
|
|VEG IAA 2/98, Isla Vega |
|
|
|MLP 98-I-10-47, MLP 98-I-10-50, MLP 98-I-10-52, MLP 98-I-10-76: tarsometatarsus;MLP 98-I-10-59: diaphysis of left tibiotarsus; MLP 98-I-10-51: proximal end of left femur; MLP 98-I-10-48: distal end of left tibiotarsus; MLP 98-I-10-60 and MLP 98-I-10-61: distal end and partial corpus of pedal phalanges.<ref name=":1">{{Cite journal |last=Acosta Hospitaleche |first=Carolina |last2=Gelfo |first2=Javier N. |date=2015 |title=New Antarctic findings of Upper Cretaceous and lower Eocene loons (Aves: Gaviiformes) |url=http://dx.doi.org/10.1016/j.annpal.2015.10.002 |journal=Annales de Paléontologie |volume=101 |issue=4 |pages=315–324 |doi=10.1016/j.annpal.2015.10.002 |issn=0753-3969|hdl=11336/53690 |hdl-access=free }}</ref> |
|
|
|Very similar to that of '']'' |
|
|
| |
|
|
|- |
|
|
|cf. ] |
|
|
|Indeterminate |
|
|
|VEG IAA 2/98, Isla Vega |
|
|
|MLP 98-I-10-54, MLP 98-I-10-27: tarsometatarsus; MLP 98-I-10-53: distal end of left tibiotarsus; MLP 98-I-10-49 distal end of right tibiotarsus<ref name=":1" /> |
|
|
|Very similar to that of '']'' |
|
|
| |
|
|
|- |
|
|
| rowspan="2" |]<ref name=":0">{{Cite journal |last=Broxson |first=Ian |date=2023 |title=Reconstructing the ecological relationships of the latest Cretaceous Antarctic dinosaurs and how functional tooth Cretaceous Antarctic dinosaurs and how functional tooth morphology influenced diet and ecological niche among basal Ornithopod dinosaurs |url=https://dc.ewu.edu/cgi/viewcontent.cgi?article=1839&context=theses |journal=EWU Masters Thesis Collection}}</ref> |
|
|
|Indeterminate |
|
|
|Sandwich Bluff, Cape Lamb |
|
|
|SDSM 159537, maxilla |
|
|
|rowspan="2" |Has oblong and narrow tooth alveoli, seen in Megaraptorans |
|
|
|rowspan="2" | |
|
|
|- |
|
|
|Indeterminate |
|
|
|Sandwich Bluff, Cape Lamb |
|
|
|SDSM 9918, left maxillary |
|
|
|- |
|
|
| ] |
|
|
| Indeterminate |
|
|
| Sandwich Bluff, Cape Lamb |
|
|
| Partial skull |
|
|
| Relationships undetermined, ] some {{convert|5|–|6|cm}} long |
|
|
| align="center" |<!--Image--> |
|
|
|- |
|
|
| rowspan="4" | '']'' |
|
| ''P. gregorii'' |
|
| ''P. gregorii'' |
|
| Lower Sandwich Bluff |
|
| Sandwich Bluff, Seymour Island |
|
| Partial ] and ], ] |
|
| Partial ] and ], ] |
|
| A ]?<ref name="cretaceousdistribution"/> |
|
| rowspan = "4"|A ] of uncertain relative. Possibly a more primitive form with strong flight ability and lighter bones<ref name="cretaceousdistribution" /> |
|
| rowspan=2 | <!--Image--> |
|
| rowspan="4" |<!--Image--> |
|
|- |
|
|- |
|
| ''P.''? sp. |
|
| ''P.''? sp. |
|
| Lower Sandwich Bluff |
|
| Sandwich Bluff, Cape Lamb |
|
| Partial skeleton including wing and hindlimbs |
|
| Partial skeleton including wing and hindlimbs |
|
| Possibly a more primitive form with strong flight ability and lighter bones |
|
|
|- |
|
|- |
|
|
|cf. ''P. gregorii''<ref name=":2">{{Cite journal |last=SOUZA |first=GEOVANE A. DE |last2=BULAK |first2=BRUNO A. |last3=SOARES |first3=MARINA B. |last4=SAYÃO |first4=JULIANA M. |last5=WEINSCHÜTZ |first5=LUIZ CARLOS |last6=BATEZELLI |first6=ALESSANDRO |last7=KELLNER |first7=ALEXANDER W.A. |date=2023 |title=The Cretaceous Neornithine record and new Vegaviidae specimens from the López de Bertodano Formation (Upper Maastrichthian) of Vega Island, Antarctic Peninsula |url=http://dx.doi.org/10.1590/0001-3765202320230802 |journal=Anais da Academia Brasileira de Ciências |volume=95 |issue=suppl 3 |doi=10.1590/0001-3765202320230802 |issn=1678-2690|doi-access=free }}</ref> |
|
| rowspan="2" | '']'' |
|
|
|
|Sandwich Bluff, Cape Lamb |
|
|
|MN 7833-V, distal portion of a tarsometatarsus |
|
|
|- |
|
|
|''P. sp.'' |
|
|
|IAA 10/13, Marambio Island |
|
|
|MLP 96-I-6-2, incomplete skeleton<ref name=":1" /> |
|
|
|- |
|
|
| rowspan="3" | '']''<ref>{{Cite journal |last=Marsà |first=Jordi Alexis Garcia |last2=Agnolín |first2=Federico L. |last3=Novas |first3=Fernando |date=2017-07-11 |title=Bone microstructure of ''Vegavis iaai'' (Aves, Anseriformes) from the Upper Cretaceous of Vega Island, Antarctic Peninsula |url=http://dx.doi.org/10.1080/08912963.2017.1348503 |journal=Historical Biology |volume=31 |issue=2 |pages=163–167 |doi=10.1080/08912963.2017.1348503 |issn=0891-2963}}</ref> |
|
| ''V. iaai''<ref name="clarkeetal2005">{{cite journal | last1 = Clarke | first1 = J.A. | last2 = Tambussi | first2 = C.P. | last3 = Noriega | first3 = J.I. | last4 = Erickson | first4 = G.M. | last5 = Ketcham | first5 = R.A. | year = 2005 | title = Definitive fossil evidence for the extant avian radiation in the Cretaceous | url = http://www.digimorph.org/specimens/Vegavis_iaai/nature03150.pdf | journal = Nature | volume = 433 | issue = 7023| pages = 305–308 | doi = 10.1038/nature03150 | pmid = 15662422 | bibcode = 2005Natur.433..305C | s2cid = 4354309 }} </ref> |
|
| ''V. iaai''<ref name="clarkeetal2005">{{cite journal | last1 = Clarke | first1 = J.A. | last2 = Tambussi | first2 = C.P. | last3 = Noriega | first3 = J.I. | last4 = Erickson | first4 = G.M. | last5 = Ketcham | first5 = R.A. | year = 2005 | title = Definitive fossil evidence for the extant avian radiation in the Cretaceous | url = http://www.digimorph.org/specimens/Vegavis_iaai/nature03150.pdf | journal = Nature | volume = 433 | issue = 7023| pages = 305–308 | doi = 10.1038/nature03150 | pmid = 15662422 | bibcode = 2005Natur.433..305C | s2cid = 4354309 }} </ref> |
|
| Lower Sandwich Bluff |
|
| Lower Sandwich Bluff |
|
| Partial skeleton, holotype |
|
| Partial skeleton, holotype |
|
| An ] |
|
| An ] |
|
| rowspan=2 | ] |
|
| rowspan="3" | ] |
|
|- |
|
|- |
|
| ''V.'' sp. |
|
| ''V.'' sp. |
|
| Cape Lamb |
|
| Plesiosaur Papoose, Cape Lamb |
|
| Isolated femur |
|
| Isolated femur |
|
| Initially identified as a fossil of a member of ],<ref>{{cite journal | last1 = Case | first1 = J. | last2 = Reguero | first2 = M. | last3 = Martin | first3 = J. | last4 = Cordes-Person | first4 = A. | year = 2006 | title = A cursorial bird from the Maastrictian of Antarctica | doi = 10.1080/02724634.2006.10010069| journal = Journal of Vertebrate Paleontology | volume = 26 | issue = 3| page = 48A | s2cid = 220413406 }}</ref> but subsequently reinterpreted as a fossil of an unnamed large-bodied member of the genus ''Vegavis''.<ref>{{cite journal |author1=Abagael R. West |author2=Christopher R. Torres |author3=Judd A. Case |author4=Julia A. Clarke |author5=Patrick M. O'Connor |author6=Matthew C. Lamanna |year=2019 |title=An avian femur from the Late Cretaceous of Vega Island, Antarctic Peninsula: removing the record of cursorial landbirds from the Mesozoic of Antarctica |journal=PeerJ |volume=7 |pages=e7231 |doi=10.7717/peerj.7231 |pmid=31333904 |pmc=6626523 }}</ref> |
|
| Initially identified as a fossil of a member of ],<ref>{{cite journal | last1 = Case | first1 = J. | last2 = Reguero | first2 = M. | last3 = Martin | first3 = J. | last4 = Cordes-Person | first4 = A. | year = 2006 | title = A cursorial bird from the Maastrictian of Antarctica | doi = 10.1080/02724634.2006.10010069| journal = Journal of Vertebrate Paleontology | volume = 26 | issue = 3| page = 48A | s2cid = 220413406 }}</ref> but subsequently reinterpreted as a fossil of an unnamed large-bodied member of the genus ''Vegavis''.<ref>{{cite journal |author1=Abagael R. West |author2=Christopher R. Torres |author3=Judd A. Case |author4=Julia A. Clarke |author5=Patrick M. O'Connor |author6=Matthew C. Lamanna |year=2019 |title=An avian femur from the Late Cretaceous of Vega Island, Antarctic Peninsula: removing the record of cursorial landbirds from the Mesozoic of Antarctica |journal=PeerJ |volume=7 |pages=e7231 |doi=10.7717/peerj.7231 |pmid=31333904 |pmc=6626523 |doi-access=free }}</ref> |
|
|- |
|
|- |
|
|
|cf. ''V. iaai''<ref name=":2" /> |
|
| '']'' |
|
|
|
|Sandwich Bluff, Cape Lamb |
|
| ''C. antarcticus'' |
|
|
|
|MN 7832-V, synsacrum |
|
| |
|
|
|
| |
|
| Partial skeleton |
|
|
| An ] |
|
|
| align=center | ] |
|
|
|- |
|
|- |
|
|
|] |
|
| '']''<ref name=Morrosaurus>{{cite journal | last1 = Rozadilla | first1 = Sebastián | last2 = Agnolin | first2 = Federico L. | last3 = Novas | first3 = Fernando E. | last4 = Aranciaga Rolando | first4 = Alexis M. | last5 = Motta | first5 = Matías J. | last6 = Lirio | first6 = Juan M. | last7 = Isasi | first7 = Marcelo P. | year = 2016 | title = A new ornithopod (Dinosauria, Ornithischia) from the Upper Cretaceous of Antarctica and its palaeobiogeographical implications | journal = Cretaceous Research | volume = 57| pages = 311–324| doi = 10.1016/j.cretres.2015.09.009 }}</ref> |
|
|
|
|Indeterminate |
|
| ''M. antarcticus'' |
|
|
|
|Seymour Island |
|
| |
|
|
|
|<ref name=":1" /> |
|
| |
|
|
|
| |
|
| An ]n ornithopod |
|
|
|
| |
|
| ] |
|
|
|- |
|
|- |
|
|
| ] |
|
| Undescribed ]<ref>{{cite journal | last1 = Cordes | year = 2002 | title = A new charadriiform avian specimen from the Early Maastrichtian of Cape Lamb, Vega Island, Antarctic Peninsula | journal = Journal of Vertebrate Paleontology | volume = 22 | issue = 3| page = 46A }}</ref> |
|
|
|
| Indeterminate |
|
| Unnamed species |
|
|
| Cape Lamb |
|
| Sandwich Bluff, Cape Lamb |
|
|
| Fragments<ref name="deposition" /> |
|
| Partial skeleton |
|
|
| |
|
| |
|
| align=center | <!--Image--> |
|
| align="center" |<!--Image--> |
|
|
|} |
|
|
|
|
|
==== Fish ==== |
|
|
===== Bony Fishes ===== |
|
|
{| class="wikitable" align="center" |
|
|- |
|
|- |
|
|
! colspan="6" align="center" | ] recorded from Lopez de Bertodano Formation |
|
| Unidentified ] |
|
|
| Unnamed species |
|
|
| |
|
|
| Partial skull |
|
|
| Relationships undetermined, ] some {{convert|5|–|6|cm}} long |
|
|
| align=center | <!--Image--> |
|
|
|- |
|
|- |
|
|
! Genus |
|
| Undescribed ] |
|
|
|
! Species |
|
| Unnamed species |
|
|
|
! Member/Location |
|
| |
|
|
|
! Material |
|
| Isolated tooth<ref name=deposition/> |
|
|
|
! Description |
|
|
! Image |
|
|
|- |
|
|
|'']''<ref name=":11" /> |
|
|
|''A. seymouri'' |
|
|
|Seymour Island |
|
|
|TTU P9210. A poorly preserved anterior skull section with partial dentary attached |
|
|
|A member of ] |
|
| |
|
| |
|
| align=center | <!--Image--> |
|
|
|- |
|
|- |
|
|
|'']'' |
|
| Undescribed non-avian ] |
|
|
|
|''E. sp.'' |
|
| Unnamed species |
|
|
|
|Seymour Island |
|
| |
|
|
|
|One palatine tooth, MLP 12-XI-29-43; five teeth, MLP 12-XI-29-25 to 28; one tooth, MLP 12-XI-29-53; thirty-five teeth, MLP 12-XI-29-55; fifty-three teeth, MLP 12-XI-29-56<ref name="Cioneetal2018" /> |
|
| Fragments<ref name=deposition/> |
|
|
|
|A member of ] |
|
| |
|
|
|
|] |
|
| align=center | <!--Image--> |
|
|
|- |
|
|- |
|
|
|] |
|
|
|Indeterminate |
|
|
|Seymour Island |
|
|
|One tooth, MLP 12-XI-29-21; ninety-four teeth, MLP 12-XI-29-38; thirteen teeth, MLP 12-XI-29-51; seventy-eight teeth, MLP 12-XI-29-52; one tooth, MLP 12-XI-29-54.<ref name="Cioneetal2018" /> |
|
|
| |
|
|
| |
|
|
|- |
|
|
|] |
|
|
|Indeterminate |
|
|
|Seymour Island |
|
|
|Isolated and fragmentary caudal fin-rays, MLP 13XI-29-57.<ref name="Cioneetal2018" /> |
|
|
| |
|
|
| |
|
|} |
|
|} |
|
|
|
|
|
=== Reptiles === |
|
=====Chondrichthyes===== |
|
{| class="wikitable" align="center" |
|
{| class="wikitable" align="center" |
|
|- |
|
|- |
|
! colspan="6" align="center" | ''']s''' recorded from Lopez de Bertodano Formation |
|
! colspan="6" align="center" | ] recorded from Lopez de Bertodano Formation |
|
|- |
|
|- |
|
! Genus |
|
! Genus |
|
! Species |
|
! Species |
|
! Member |
|
! Member/Location |
|
! Material |
|
! Material |
|
! Description |
|
! Description |
|
! Image |
|
! Image |
|
|- |
|
|- |
|
|
|'']'' |
|
|'']''<ref>O'Gorman, J. P., Gasparini, Z., & Salgado, L. (2012). Postcranial morphology of Aristonectes (Plesiosauria, Elasmosauridae) from the Upper Cretaceous of Patagonia and Antarctica. Antarctic Science, 25(1), 71–82. https://doi.org/10.1017/S0954102012000673</ref> |
|
|
|
|''C. sp.'' <ref name=":10">{{Cite journal |last=Gouiric-Cavalli |first=S. |last2=Acosta-Burllaile |first2=L. |last3=Iglesias |first3=A. |last4=Moly |first4=J. J. |last5=O’Gorman |first5=J. P. |last6=Reguero |first6=M. |last7=Santillana |first7=S. |last8=Talevi... |first8=M. |date=2017 |title=Late Mesozoic marine Antarctic fishes: future perspectives based on the newly collections recovered in the Ameghino and López de Bertodano Formations. |url=http://sedici.unlp.edu.ar/handle/10915/81187 |journal=Research and Knowledge |volume=3 |issue=1 |pages=16-21}}</ref> |
|
|''A. cf. parvidens'' |
|
|
|
|Seymour Island |
|
|
|Teeth |
|
|
|A ] |
|
|
|] |
|
|
|- |
|
|
|'']'' |
|
|
|''cf. C. sp.'' |
|
|
|Seymour Island |
|
|
|Two left upper lateral teeth preserving one root branch and lateral denticle, MLP 13-XI-29-35, MLP 13-XI-29-37; one right upper lateral tooth preserving one root branch and lateral denticle, MLP 13-XI-29-36; several fragmentary teeth, MLP 13-XI29-4, MLP13-XI-29-44 to46, MLP13-XI-29-16, MLP 13-XI-29-13 to 14.<ref name="Cioneetal2018" /> |
|
|
|A ] Shark |
|
| |
|
| |
|
|Partial postcranial skeleton, MLP 89-III-3-1. |
|
|
| A giant ] |
|
|
|] |
|
|
|- |
|
|- |
|
|'']'' |
|
|"'']''" |
|
|''K. hervei'' |
|
|''“C. appendiculata”'' |
|
|
|Seymour Island |
|
|
|One lateral lower tooth which lacks crown tip, distal lateral cusplet, and distal root branch, MLP 13XI-29-47; one anterior upper tooth lacking the distal root branch, distal lateral cusplet, and crown tip, MLP 13-XI-29-2<ref name="Cioneetal2018" /> |
|
|
|A ] Shark |
|
| |
|
| |
|
|Several incomplete parts of a skull, jawbone, 30 isolated teeth, and a partial left humerus. |
|
|
|A ]. |
|
|
|] |
|
|
|- |
|
|- |
|
|'']'' |
|
|] |
|
|
|Indeterminate |
|
|''M. seymourensis'' |
|
|
|
|Seymour Island |
|
|
|Four crowns, MLP 13-XI-29-30.<ref name="Cioneetal2018" /> |
|
| |
|
| |
|
|
| |
|
|several cervical vertebrae, a right humerus, a nearly complete left forelimb missing the proximal end of the humerus, and a left femur (TTU P9217). |
|
|
|
|- |
|
|
| rowspan="2" |'']''<ref name=":11">{{Cite journal |last=Grande |first=L. |last2=Chatterjee |first2=S. |date=1987 |title=New Cretaceous fish fossils from Seymour Island, Antarctic Peninsula. |url=https://www.palass.org/sites/default/files/media/publications/palaeontology/volume_30/vol30_part4_pp829-837.pdf |journal=Palaeontology |volume=30 |pages=829-837}}</ref> |
|
|
|''N. sp.'' |
|
|
|Seymour Island |
|
|
|Teeth |
|
|
|A ] Shark |
|
|
| |
|
|
|- |
|
|
|''?N. sp.''<ref name=":10" /> |
|
|
|Seymour Island |
|
|
|Teeth |
|
|
|A ] Shark |
|
|
| |
|
|
|- |
|
|
|'']'' |
|
|
|''P. sp.'' |
|
|
|Seymour Island |
|
|
|Four fragmentary teeth, MLP 13-XI-29-8, MLP 13XI-29-18, MLP 13-XI-29-31, and MLP 13-XI-29-32.<ref name="Cioneetal2018" /> |
|
|
|A ] Shark |
|
|
| |
|
|
|- |
|
|
|'']'' |
|
|
|''aff. P. sp.'' |
|
|
|Seymour Island |
|
|
|Three fragmentary rostral spines, MLP 13-XI-2939, MLP 13-XI-29-40, and MLP 13-XI-29-41.<ref name="Cioneetal2018" /> |
|
|
|A ] Shark |
|
|
| |
|
|
|- |
|
|
|'']'' |
|
|
|''P. sp.'' |
|
|
|Seymour Island |
|
|
|Two lateral, almost complete teeth, MLP 13-XI29-9, MLP 13-XI-29-33; one latero-posterior, complete tooth, MLP 13-XI-29-10<ref name="Cioneetal2018" /> |
|
|
|A ] Shark |
|
|
| |
|
|
|- |
|
|
| rowspan="2" |'']''<ref name=":11" /> |
|
|
|''S. sp.'' |
|
|
|Seymour Island |
|
|
|Teeth |
|
|
|A ] Shark |
|
|
| |
|
|
|- |
|
|
|''S. sp.'' |
|
|
|Seymour Island |
|
|
|Two fragmentary teeth, MLP 13-XI-29-20, MLP 13-XI-29-11<ref name="Cioneetal2018" /> |
|
|
|A ] Shark |
|
|
| |
|
|
|- |
|
|
| '']''<ref name=":9" /> |
|
|
| ''X. diastemacron'' |
|
|
| Filo Negro Section, Klb 9 |
|
|
|MN 7825-V (holotype),incomplete posterolateral tooth of the lower jaw, with only its anterior portion still preserved |
|
|
| A ] Shark |
|
|
| |
|
|
|} |
|
|
|
|
|
==== Reptiles ==== |
|
|
===== Elasmosaurs ===== |
|
|
{| class="wikitable" align="center" |
|
|
|- |
|
|
! colspan="6" align="center" | ''']s''' recorded from Lopez de Bertodano Formation |
|
|
|- |
|
|
! Genus |
|
|
! Species |
|
|
! Member/Location |
|
|
! Material |
|
|
! Description |
|
|
! Image |
|
|
|- |
|
|
| rowspan="3" |'']''<ref>O'Gorman, J. P., Gasparini, Z., & Salgado, L. (2012). Postcranial morphology of Aristonectes (Plesiosauria, Elasmosauridae) from the Upper Cretaceous of Patagonia and Antarctica. Antarctic Science, 25(1), 71–82. https://doi.org/10.1017/S0954102012000673</ref> |
|
|
|''A. parvidens'' |
|
|
| Seymour Island |
|
|
|Partial postcranial skeleton (MLP 89-III-3-1) |
|
|
| rowspan="3" | A giant ] |
|
|
| rowspan="3" |] |
|
|
|- |
|
|
|''A. sp''<ref name=":3">{{Cite journal |last=Miller |first=Case V. |last2=O'Gorman |first2=José P |last3=Salisbury |first3=Steven W. |last4=Coria |first4=Rodolfo A. |last5=Roberts |first5=Eric M. |last6=O'Connor |first6=Patrick M |last7=Reguero |first7=Marcelo A. |last8=Lamanna |first8=Matthew C. |date=2020-07-31 |title=A New Plesiosaur (Reptilia: Sauropterygia) Specimen from the Upper Cretaceous of West Antarctica, with Comments on the Ontogeny and Morphological Diversity of the Elasmosaurid Pelvic Girdle |url=http://dx.doi.org/10.2992/007.086.0201 |journal=Annals of Carnegie Museum |volume=86 |issue=2 |pages=93 |doi=10.2992/007.086.0201 |issn=0097-4463}}</ref> |
|
|
|Sandwich Bluff, Cape Lamb |
|
|
|MLP 11-I-1-15, caudal vertebra |
|
|
|- |
|
|
|''A. sp''<ref name="Chatterjee1989" /><ref>{{Cite journal |last=Otero |first=Rodrigo A. |last2=Soto-Acuña |first2=Sergio |last3=O'Keefe |first3=Frank Robin |last4=O’Gorman |first4=José P. |last5=Stinnesbeck |first5=Wolfgang |last6=Suárez |first6=Mario E. |last7=Rubilar-Rogers |first7=David |last8=Salazar |first8=Christian |last9=Quinzio-Sinn |first9=Luis Arturo |date=2014 |title=''Aristonectes quiriquinensis'', sp. nov., a new highly derived elasmosaurid from the upper Maastrichtian of central Chile |url=http://dx.doi.org/10.1080/02724634.2013.780953 |journal=Journal of Vertebrate Paleontology |volume=34 |issue=1 |pages=100–125 |doi=10.1080/02724634.2013.780953 |issn=0272-4634|hdl=11336/79718 |hdl-access=free }}</ref> |
|
|
|Seymour Island |
|
|
|TTU.P.9219 (holotype skull and cervical vertebrae) |
|
|
|- |
|
|
| rowspan="7" |]<ref>{{Cite journal |last=Gasparini |first=Z. |last2=Del Valle |first2=F. |last3=Goñi |first3=R. |date=1984 |title=An elasmosaur (Reptilia, Plesiosauria) of the Upper Cretaceous in the Antarctic |journal=Contribuciones del Instituto Antártico Argentino |volume=305 |pages=1-24}}</ref> |
|
|
|Indeterminate |
|
|
|SW corner, Seymour Island |
|
|
|MLP 82-I-28-1, an incomplete skeleton comprising 15 cervical, three pectorals, 21 dorsal, three sacral, and 22 caudal vertebrae, an almost complete left hind limb, some dorsal ribs, incomplete coracoids and fragments of the scapulae |
|
|
|rowspan="7" | |
|
|
|rowspan="7" | |
|
|
|- |
|
|
|Indeterminate<ref>{{Cite journal |last=Fostowicz-Frelik |first=L. |last2=Gazdzicki |first2=A. |date=2001 |title=Anatomy and histology of plesiosaur bones from the Late Cretaceous of Seymour Island, Antarctic Paninsula. |url=https://www.researchgate.net/publication/301287045_Anatomy_and_histology_of_plesiosaur_bones_from_the_Late_Cretaceous_of_Seymour_Island_Antarctic_Peninsula |journal=Palaeontologica Polonica |volume=60 |pages=7-32}}</ref> |
|
|
|SW corner, Seymour Island |
|
|
|ZPAL R.8, pectoral, dorsal, and caudal vertebral centra, femur, tibia, and fragments of the humerus, scapula, and ischia |
|
|
|- |
|
|
|Indeterminate<ref name=":4">{{Cite journal |last=Chatterjee |first=Sankar |last2=Small |first2=Bryan J. |date=1989 |title=New plesiosaurs from the Upper Cretaceous of Antarctica |url=http://dx.doi.org/10.1144/gsl.sp.1989.047.01.15 |journal=Geological Society, London, Special Publications |volume=47 |issue=1 |pages=197–215 |doi=10.1144/gsl.sp.1989.047.01.15 |issn=0305-8719}}</ref> |
|
|
|Seymour Island |
|
|
|TTU P 9240; dorsal, sacral and caudal vertebrae, limbs and paddle fragments |
|
|
|- |
|
|
|Indeterminate<ref>{{Cite journal |last=Otero |first=Rodrigo A. |last2=Soto-Acuña |first2=Sergio |last3=Vargas |first3=Alexander O. |last4=Rubilar-Rogers |first4=David |last5=Yury-Yáñez |first5=Roberto E. |last6=Gutstein |first6=Carolina S. |date=2014 |title=Additions to the diversity of elasmosaurid plesiosaurs from the Upper Cretaceous of Antarctica |url=http://dx.doi.org/10.1016/j.gr.2013.07.016 |journal=Gondwana Research |volume=26 |issue=2 |pages=772–784 |doi=10.1016/j.gr.2013.07.016 |issn=1342-937X}}</ref> |
|
|
|Seymour Island |
|
|
|SGO.PV.6523, postcranial remains of a single adult individual, including remains of 9 mid-to-posterior cervical vertebrae (6 of them preserving parts of their centra), the right scapula, several fragments of ribs and gastralia, and one phalanx. |
|
|
|- |
|
|
|Indeterminate<ref name=":4" /> |
|
|
|Seymour Island |
|
|
|TTU P 9238; part of cervicals, rib fragments, isolated paddles, and gastroliths |
|
|
|- |
|
|
|Indeterminate<ref name="Chatterjee1989" /> |
|
|
|Seymour Island |
|
|
|TTU P 9239; isolated vertebrae, limb bones, paddle elements, and ribs |
|
|
|- |
|
|
|Indeterminate |
|
|
|Seymour Island |
|
|
|IAA Pv 443, an incomplete skeleton comprising the mandibular symphysis and part of right and left mandibular rami, cervical and dorsal centra, an incomplete humerus, radius, ulna, ulnare, intermedium, radiale and distal carpal 1, 2 þ 3 and 4, other fragmentary postcranial bones and associated gastroliths<ref>{{Cite journal |last=O’Gorman |first=José Patricio |last2=Bona |first2=Paula |last3=de los Reyes |first3=Martín |last4=Raffi |first4=Maria Eugenia |last5=Reguero |first5=Marcelo |date=2020-10-01 |title=A non-aristonectine plesiosaur from Antarctica reveals new data on the mandibular symphysis of elasmosaurids |url=http://dx.doi.org/10.1080/03115518.2020.1824261 |journal=Alcheringa: An Australasian Journal of Palaeontology |volume=44 |issue=4 |pages=565–576 |doi=10.1080/03115518.2020.1824261 |issn=0311-5518}}</ref> |
|
|
|- |
|
|
|]<ref name=":3" /> |
|
|
|Indeterminate |
|
|
|Sandwich Bluff, Cape Lamb |
|
|
|CM 93780; left and right pubes and ischia: MLP 15-I-7-8, left ilium and indeterminate fragments |
|
|
| |
|
|
| |
|
|
|- |
|
|
|'']''<ref name="Marambionectes">{{Cite journal |last1=O'Gorman |first1=Jose P. |last2=Canale |first2=Juan I. |last3=Bona |first3=Paula |last4=Tineo |first4=David E. |last5=Reguero |first5=Marcelo |last6=Cárdenas |first6=Magalí |date=2024-12-31 |title=A new elasmosaurid (Plesiosauria: Sauropterygia) from the López de Bertodano Formation: new data on the evolution of the aristonectine morphology |journal=] |language=en |volume=22 |issue=1 |doi=10.1080/14772019.2024.2312302 |bibcode=2024JSPal..2212302O |issn=1477-2019}}</ref> |
|
|
|''M. molinai'' |
|
|
|Seymour Island |
|
|
|Partially articulated incomplete skeleton including cranial material, many vertebrae, ribs, an ilium, limb bones (right humerus and ulna, a femur), and ]s (]-Pv 752) |
|
|
|A ]n elasmosaur |
|
|
| |
|
|
] |
|
|
|- |
|
|
|'']''<ref name="Chatterjee1989">{{cite journal|last1=Chatterjee|first1=S.|last2=Small|first2=B. J.|year=1989|title=New plesiosaurs from the Upper Cretaceous of Antarctica|journal=Geological Society Special Publications|volume=47|issue=1|pages=197–215|doi=10.1144/GSL.SP.1989.047.01.15|bibcode=1989GSLSP..47..197C|s2cid=140639013|url=https://www.researchgate.net/publication/249548928}}</ref> |
|
|
|''M. seymourensis'' |
|
|
| Seymour Island |
|
|
|several cervical vertebrae, a right humerus, a nearly complete left forelimb missing the proximal end of the humerus, and a left femur (TTU P9217) |
|
|An elasmosaur |
|
|An elasmosaur |
|
|] |
|
|] |
|
|
|- |
|
|
| rowspan="2" |]<ref name=":5">{{Cite journal |last=O’Gorman |first=José P. |last2=Coria |first2=Rodolfo A. |date=2016-09-21 |title=A new elasmosaurid specimen from the upper Maastrichtian of Antarctica: new evidence of a monophyletic group of Weddellian elasmosaurids |url=http://dx.doi.org/10.1080/03115518.2016.1224318 |journal=Alcheringa: An Australasian Journal of Palaeontology |volume=41 |issue=2 |pages=240–249 |doi=10.1080/03115518.2016.1224318 |issn=0311-5518|hdl=11336/79006 |hdl-access=free }}</ref> |
|
|
|Indeterminate |
|
|
|Sandwich Bluff, Cape Lamb |
|
|
|MLP 15-I-7-48, right humerus, ulna, ulnare, intermedium, distal carpal I, distal carpal II+III, pisiform, phalanges and one rib |
|
|
| rowspan = "2"| |
|
|
| rowspan = "2"| |
|
|
|- |
|
|
|Indeterminate |
|
|
|Seymour Island |
|
|
|MLP 14-I-20-16, 12 cervical vertebrae, three pectoral vertebrae, 11 dorsal vertebrae, one sacral vertebra, 11 caudal vertebrae, right femur, tibia, fibula and mesopodial elements, fragments of pectoral and pelvic girdles and gastroliths<ref name=":5" /> |
|
|} |
|
|} |
|
|
|
|
|
=== Other fossils === |
|
===== Mosasaurs ===== |
|
|
{| class="wikitable" align="center" |
|
Among others, the following fossils have been found in the formation: |
|
|
|
|- |
|
|
! colspan="6" align="center" | ''']s''' recorded from Lopez de Bertodano Formation |
|
|
|- |
|
|
! Genus |
|
|
! Species |
|
|
! Member/Location |
|
|
! Material |
|
|
! Description |
|
|
! Image |
|
|
|- style="background:#E3F5FF;" |
|
|
|'']'' |
|
|
|''A. bradyi'' |
|
|
| Seymour Island. |
|
|
| A fossilized eggshell. |
|
|
| A ]. |
|
|
| |
|
|
|- |
|
|
|'']''<ref name="Oteroetal2017">{{cite journal|author1=Rodrigo A. Otero|author2= Sergio Soto-Acuña|author3=David Rubilar-Rogers|author4=Carolina S. Gutstein| title = ''Kaikaifilu hervei'' gen. et sp. nov., a new large mosasaur (Squamata, Mosasauridae) from the upper Maastrichtian of Antarctica | journal = ] |year= 2017| volume = 70 | pages = 209–225 | doi = 10.1016/j.cretres.2016.11.002 |bibcode= 2017CrRes..70..209O| s2cid = 133320233}}</ref> |
|
|
|''K. hervei'' |
|
|
| Seymour Island |
|
|
|Several incomplete parts of a skull, jawbone, 30 isolated teeth, and a partial left humerus (SGO.PV.6509) |
|
|
|A ] ] |
|
|
|] |
|
|
|- |
|
|
| rowspan="2" |'']''<ref name=":6">{{Cite journal |last=Martin |first=James E. |last2=Crame |first2=J. Alistair |date=2006 |title=Palaeobiological significance of high-latitude Late Cretaceous vertebrate fossils from the James Ross Basin, Antarctica |url=http://dx.doi.org/10.1144/gsl.sp.2006.258.01.08 |journal=Geological Society, London, Special Publications |volume=258 |issue=1 |pages=109–124 |doi=10.1144/gsl.sp.2006.258.01.08 |issn=0305-8719}}</ref> |
|
|
|''L sp.'' |
|
|
|Vega Island Sandwich Bluff |
|
|
|MLP 98-I-10-1 is a fragment of a maxilla; MLP 98-I-10-12/15/23 are a teeth<ref name=":6" /> |
|
|
| rowspan = 2| A ] mosasaur |
|
|
| rowspan = 2| |
|
|
|- |
|
|
|''L sp.'' |
|
|
|Seymour Island |
|
|
|DJ.952.266, a tooth<ref name=":7">{{Cite journal |last=Mulder |first=E. W. A. |date=1999 |title=Transatlantic latest Cretaceous mosasaurs (Reptilia, Lacertilia) from the Maastrichtian type area and New Jersey |url=https://www.researchgate.net/publication/262901771_Transatlantic_latest_Cretaceous_Mosasaurs_Reptilia_Lacertilia_from_the_Maastrichtian_type_area_and_New_Jersey |journal=Geologie en Mijnbouw |issue=78 |pages=281-300}}</ref> |
|
|
|- |
|
|
| rowspan="5" |] |
|
|
|Indeterminate |
|
|
|Bahía Fósiles |
|
|
|MLP 80-I-1-1, a cervical vertebra; MLP 80-I-1-2, a mandibular fragment; MLP 80-I-1-3, a cranial fragment; MLP 82-I-28-2, a vertebra; MLP 82-I-3-1/4, four caudal centers<ref name=":8">{{Cite journal |last=Fernández |first=Marta S. |last2=Gasparini |first2=Zulma |date=2012 |title=Campanian and Maastrichtian mosasaurs from Antarctic Peninsula and Patagonia, Argentina |url=http://dx.doi.org/10.2113/gssgfbull.183.2.93 |journal=Bulletin de la Société Géologique de France |volume=183 |issue=2 |pages=93–102 |doi=10.2113/gssgfbull.183.2.93 |issn=1777-5817}}</ref> |
|
|
| rowspan = 5| |
|
|
| rowspan = 5| |
|
|
|- |
|
|
|Indeterminate |
|
|
|Seymour Island |
|
|
|DJ.957.133, 18 partially articulated caudal vertebrae, four of which possess transverse process, and DJ.957.505 a caudal vertebra<ref name=":7" /> |
|
|
|- |
|
|
|Indeterminate |
|
|
|Filo Negro Section |
|
|
|MLP 82-I-26-1, a pygal vertebra<ref name=":9">{{Cite journal |last=Otávio dos Santos |first=Rodolfo |last2=Riff |first2=Douglas |last3=Ramos |first3=Renato Rodriguez Cabral |last4=Fernandes Rodrigues |first4=Igor |last5=Scheffler |first5=Sandro Marcelo |last6=Sucerquia |first6=Paula Andrea |last7=de Araújo Carvalho |first7=Marcelo |date=2024-03-06 |title=A new species of cow shark (Hexanchiformes: Hexanchidae) from the Late Cretaceous of Seymour Island, Antarctica |url=http://dx.doi.org/10.1080/08912963.2024.2316047 |journal=Historical Biology |pages=1–12 |doi=10.1080/08912963.2024.2316047 |issn=0891-2963}}</ref> |
|
|
|- |
|
|
|Indeterminate |
|
|
|Seymour Island |
|
|
|IAA-Pv 819, an almost complete right humerus.<ref>{{Cite journal |last=O’Gorman |first=Jose Patricio |last2=Bona |first2=Paula |last3=Canale |first3=Juan Ignacio |last4=Tineo |first4=David Eric |last5=Fernández |first5=Marta Susana |last6=Cárdenas |first6=Magali |last7=Reguero |first7=Marcelo |date=2023-04-03 |title=A new mosasaurine specimen (Squamata, Mosasauridae) from the Upper Cretaceous of Antarctica with comments on the Weddellian diversity of Mosasaurinae |url=http://dx.doi.org/10.1080/03115518.2023.2203739 |journal=Alcheringa: An Australasian Journal of Palaeontology |volume=47 |issue=2 |pages=211–220 |doi=10.1080/03115518.2023.2203739 |issn=0311-5518}}</ref> |
|
|
|- |
|
|
|Indeterminate |
|
|
|Seymour Island |
|
|
|MLP 82-I-5-1, fragments of vertebrae and ribs<ref name=":8" /> |
|
|
|- |
|
|
| rowspan="3" |'']'' |
|
|
|''aff. M. hoffmanni'' |
|
|
|Seymour Island |
|
|
|DJ.1053.10, a large, fragmentary skull<ref name=":7" /> |
|
|
| rowspan="3" |A ] mosasaur |
|
|
| rowspan="3" |] |
|
|
|- |
|
|
|''M. sp.'' |
|
|
|Seymour Island |
|
|
|DJ.1020.2-A, DJ.1020.2-B and DJ.1053.14- A, teeth; MLP 83-X-12-2, a caudal vertebra; MLP 92-XII-30, skull fragments including one tooth and a relatively short, and medially constricted suprastapedial process of the quadrate<ref name=":7" /> |
|
|
|- |
|
|
|''M. sp.'' |
|
|
|Seymour Island |
|
|
|MLP 15-I-24-41, a partial skull including, partial frontal, right postorbital, parietal, right quadrate, right posterior end of basisphenoid, right coronoid, right angular, splenial and right surangular, a broken marginal tooth and several pterygoid teeth have been associated to this specimen.<ref>{{Cite journal |last=González Ruiz |first=Pablo |last2=Fernández |first2=Marta S. |last3=Talevi |first3=Marianella |last4=Leardi |first4=Juan M. |last5=Reguero |first5=Marcelo A. |date=2019 |title=A new Plotosaurini mosasaur skull from the upper Maastrichtian of Antarctica. Plotosaurini paleogeographic occurrences |url=http://dx.doi.org/10.1016/j.cretres.2019.06.012 |journal=Cretaceous Research |volume=103 |pages=104166 |doi=10.1016/j.cretres.2019.06.012 |issn=0195-6671|hdl=11336/125124 |hdl-access=free }}</ref> |
|
|
|- |
|
|
| rowspan="2" |'']'' |
|
|
|''P. sp.'' |
|
|
|Seymour Island |
|
|
|DJ.1020.2-C, DJ.1020.2-H and DJ.952.266, teeth<ref name=":7" /> |
|
|
| rowspan="2" |A ] mosasaur |
|
|
| rowspan="2" |] |
|
|
|- |
|
|
|''P. sp.'' |
|
|
|Quebrada de la Foca muerta |
|
|
|MLP 79-I-1/20, several vertebrae<ref name=":8" /> |
|
|
|- |
|
|
| rowspan="3" |] |
|
|
|Indeterminate |
|
|
|Bahía Fósiles |
|
|
|MLP 87-II-7-1, a vertebra; MLP 86-X-28-7, an anterior caudal vertebra<ref name=":8" /> |
|
|
| rowspan="3" | |
|
|
| rowspan="3" | |
|
|
|- |
|
|
|Indeterminate |
|
|
|Seymour Island |
|
|
|DJ.956.41, two or three caudal vertebrae<ref name=":7" /> |
|
|
|- |
|
|
|Indeterminate |
|
|
|Filo Negro Section |
|
|
|lam. II, 7-8, a vertebra<ref name=":9" /> |
|
|
|} |
|
|
|
|
|
|
=== Other fossils === |
|
;Ammonites<ref name="Witts15"/> |
|
;Ammonites<ref name="Witts15"/> |
|
{| class="wikitable" align="center" |
|
{| class="wikitable" align="center" |
Line 176: |
Line 551: |
|
! Genus |
|
! Genus |
|
! Species |
|
! Species |
|
! Member |
|
! Member/Location |
|
! Material |
|
! Material |
|
! Description |
|
! Description |
|
! Image |
|
! Image |
|
|- |
|
|- |
|
| ''] |
|
| '']'' |
|
| ''D. cylindraceum'' |
|
| ''D. cylindraceum'' |
|
| |
|
| |
Line 188: |
Line 563: |
|
| |
|
| |
|
|- |
|
|- |
|
| ] |
|
| '']'' |
|
|'' G. seymouriense'' |
|
|'' G. seymouriense'' |
|
| |
|
| |
Line 195: |
Line 570: |
|
| |
|
| |
|
|- |
|
|- |
|
| ] |
|
| '']'' |
|
| ''G. joharae'' |
|
| ''G. joharae'' |
|
| |
|
| |
Line 202: |
Line 577: |
|
| |
|
| |
|
|- |
|
|- |
|
| ] |
|
| '']'' |
|
| ''K. laurae'' |
|
| ''K. laurae'' |
|
| |
|
| |
Line 209: |
Line 584: |
|
| |
|
| |
|
|- |
|
|- |
|
| ] |
|
| '']'' |
|
| ''M. densicostatus'' |
|
| ''M. densicostatus'' |
|
| |
|
| |
Line 216: |
Line 591: |
|
| |
|
| |
|
|- |
|
|- |
|
| ] |
|
| '']'' |
|
| ''P. (Pachydiscus) ultimus'' |
|
| ''P. (Pachydiscus) ultimus'' |
|
| |
|
| |
Line 223: |
Line 598: |
|
| |
|
| |
|
|- |
|
|- |
|
| ] |
|
| '']'' |
|
| ''P. cf. loryi'' |
|
| ''P. cf. loryi'' |
|
| |
|
| |
Line 230: |
Line 605: |
|
| |
|
| |
|
|- |
|
|- |
|
| ] |
|
| '']'' |
|
| ''Z. varuna'' |
|
| ''Z. varuna'' |
|
| |
|
| |
Line 245: |
Line 620: |
|
! Genus |
|
! Genus |
|
! Species |
|
! Species |
|
! Member |
|
! Member/Location |
|
! Material |
|
! Material |
|
! Description |
|
! Description |
|
! Image |
|
! Image |
|
|- |
|
|- |
|
| ] |
|
| '']'' |
|
| ''E. dorbignyanum'' |
|
| ''E. dorbignyanum'' |
|
| |
|
| |
Line 257: |
Line 632: |
|
| |
|
| |
|
|- |
|
|- |
|
| rowspan = "2"| ] |
|
| rowspan = "2"| '']'' |
|
|''C. nordenskjoldi'' |
|
|''C. nordenskjoldi'' |
|
| |
|
| |
Line 270: |
Line 645: |
|
| |
|
| |
|
|- |
|
|- |
|
| ] |
|
| '']'' |
|
| ''R. fallax'' |
|
| ''R. fallax'' |
|
| |
|
| |
Line 291: |
Line 666: |
|
|
|
|
|
=== Bibliography === |
|
=== Bibliography === |
|
* {{cite LSA |first=Lucas J. |last=Legendre |first2=David |last2=Rubilar Rogers |first3=Grace M. |last3=Musser |first4=Sarah N. |last4=Davis |first5=Rodrigo A. |last5=Otero |first6=Alexander O. |last6=Vargas |first7=Julia A. |last7=Clarke |year=2020|title=A giant soft-shelled egg from the Late Cretaceous of Antarctica |url=https://www.nature.com/articles/s41586-020-2377-7 |journal=] |volume=. |pages=. |accessdate=2020-06-17}} |
|
* {{citation |first1=Lucas J. |last1=Legendre |first2=David |last2=Rubilar Rogers |first3=Grace M. |last3=Musser |first4=Sarah N. |last4=Davis |first5=Rodrigo A. |last5=Otero |first6=Alexander O. |last6=Vargas |first7=Julia A. |last7=Clarke |year=2020|title=A giant soft-shelled egg from the Late Cretaceous of Antarctica |url=https://www.nature.com/articles/s41586-020-2377-7 |journal=] |volume= 583|issue=7816 |pages= 411–414|doi=10.1038/s41586-020-2377-7 |pmid=32555453 |bibcode=2020Natur.583..411L |accessdate=2020-06-17}} |
|
|
|
|
|
== Further reading == |
|
== Further reading == |
|
* {{cite journal | last1 = Poole | first1 = I. | last2 = Mennega | first2 = A. M. W. | last3 = Cantrill | first3 = D. J. | year = 2003 | title = Valdivian ecosystems in the Late Cretaceous and Early Tertiary of Antarctica: further evidence from myrtaceous and eucryphiaceous fossil wood | journal = Review of Palaeobotany and Palynology | volume = 124 | issue = 1–2| pages = 9–27 | doi = 10.1016/s0034-6667(02)00244-0 | hdl = 1874/31608 | s2cid = 129281012 | hdl-access = free }} |
|
* {{cite journal | last1 = Poole | first1 = I. | last2 = Mennega | first2 = A. M. W. | last3 = Cantrill | first3 = D. J. | year = 2003 | title = Valdivian ecosystems in the Late Cretaceous and Early Tertiary of Antarctica: further evidence from myrtaceous and eucryphiaceous fossil wood | journal = Review of Palaeobotany and Palynology | volume = 124 | issue = 1–2| pages = 9–27 | doi = 10.1016/s0034-6667(02)00244-0 | bibcode = 2003RPaPa.124....9P | hdl = 1874/31608 | s2cid = 129281012 | hdl-access = free }} |
|
|
|
|
|
] |
|
] |
Dinosaur remains are among the fossils that have been recovered from the formation and include at least two and probably as much as six lineages of indisputably modern birds: one related to waterfowl, a primitive shorebird or related form, 1 to 2 species of possible loons, a large and possibly flightless bird belonging to a lineage extinct today as well as a partial skull that might belong to either of the smaller species or represent yet another one. The formation also contains a rich fossil invertebrate fauna, including bivalves, gastropods, and cephalopods (ammonites and nautiloids).