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FAU Climate Change Initiative Priority Theme: Research, Engineering, and Adaption to a Change Climate
Title
FAU Climate Change Initiative Priority Theme: Research, Engineering, and Adaption to a Change Climate.
Creator
Berry, Leonard, Koch, Marguerite, Center for Environmental Studies, Benscoter, Brian, Comas, Xavier, Devlin, Donna, Fadiman, Maria, Gerstein, E., Herzing, Denise L., Hindle, Tobin, Milton, Sarah L., Oleinik, Anton E., Proffitt, C. Edward, Restrepo, Jorge I., Root, Tara L., Wyneken, Jeanette, Xie, Zhixiao, Zhang, Xing-Hai, Esnard, Ann-Margaret, Mitsova, Diana, Murley, J., Vos, J., Escaleras, Monica, Mehallis, M., Shaw, Eric H., Hardman, Guillermo [John], Lambert, Julie, Thomas, G., Arockiasamy, Madasamy, Bloetscher, Frederick, Carvalho, G., Dhanak, Manhar R., Frisk, George V., Kaisar, Evangelos I., Kalva, Hari, Meeroff, Daniel E., Rodriguez, Jarice, Scarlatos, Panagiotis (Pete) D., Shankar, Ravi, Teegavarapu, Ramesh, Brown, Clifford T., McAfee, Francis, Widener, Patricia, Dalgleish, Fraser R., Hanisak, M. Dennis, McMulloch, S., O'Corry-Crowe, Gregory, Pomponi, Shirley A., Reed, John K., Scarpa, John, Voss, Joshua, Heimlich, Barry N., Alvarez, R., Jolley, J., Edwards, A., Charles E. Schmidt College of Science, Harbor Branch Oceanographic Institute, College of Business, Dorothy F. Schmidt College of Arts and Letters, College of Education, College of Engineering and Computer Science
Date Issued
2010
PURL
http://purl.flvc.org/fau/fd/FA00003457
Format
Citation
New occurrences of Fortipecten hallae (Dall, 1921) (Mollusca, Bivalvia) in the Pliocene of the North Pacific
Title
New occurrences of Fortipecten hallae (Dall, 1921) (Mollusca, Bivalvia) in the Pliocene of the North Pacific.
Creator
Oleinik, Anton E., Barinov, Konstantin B., Marincovich, Louie, Jr.
Abstract/Description
The large North Pacific bivalve mollusk index-fossil Fortipecten hallae (Dall, 1921) is present in a well-dated stratigraphic section of the Milky River Formation, Alaska Peninsula, southwestern Alaska. Co-occurring marine diatoms belong to the upper part of the subzone B of the Neodenticula kamtschatica diatom zone of the North Pacific diatom chronostratigraphy, with an age range of 4.8–5.1 Ma (early Pliocene). Based on coeval occurrences in northeastern Kamchatka, Russia, and synchronous...
Show moreThe large North Pacific bivalve mollusk index-fossil Fortipecten hallae (Dall, 1921) is present in a well-dated stratigraphic section of the Milky River Formation, Alaska Peninsula, southwestern Alaska. Co-occurring marine diatoms belong to the upper part of the subzone B of the Neodenticula kamtschatica diatom zone of the North Pacific diatom chronostratigraphy, with an age range of 4.8–5.1 Ma (early Pliocene). Based on coeval occurrences in northeastern Kamchatka, Russia, and synchronous changes in the two molluscan assemblages, F. hallae is a useful indicator of early Pliocene climatic warming along the high latitude North Pacific margin.
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Date Issued
2005-07-25
PURL
http://purl.flvc.org/fau/165900
Subject Headings
Biogeography--North Pacific Ocean, Geology, Stratigraphic--Paleocene, Geology--North Pacific Ocean, Mollusks, Fosssil--North Pacific Ocean, Paleoclimatology--North Pacific Ocean
Format
Document (PDF)
Eocene gastropods of Western Kamchatka- implications for high-latitude North Pacific biostratigraphy and biogeography.
Title
Eocene gastropods of Western Kamchatka- implications for high-latitude North Pacific biostratigraphy and biogeography.
Creator
Oleinik, Anton E.
Abstract/Description
Fossiliferous rocks of the Snatolskaya and Kovachinskaya formations comprise a Middle and Late Eocene shallow-marine record of the central part of western Kamchatka. Gastropod assemblages of these formations contain taxa that are conspecific with those in Paleogene strata of western North America and Japan, as well as a large percentage of endemic species. Analysis of the latitudinal ranges and worldwide occurrences of gastropod genera from these formations show the presence of three...
Show moreFossiliferous rocks of the Snatolskaya and Kovachinskaya formations comprise a Middle and Late Eocene shallow-marine record of the central part of western Kamchatka. Gastropod assemblages of these formations contain taxa that are conspecific with those in Paleogene strata of western North America and Japan, as well as a large percentage of endemic species. Analysis of the latitudinal ranges and worldwide occurrences of gastropod genera from these formations show the presence of three biogeographic components: cosmopolitan, North Pacific, and endemic. No Tethyan, or circumtropical genera are present in these Kamchatkan Middle and Late Eocene gastropod faunas. Changes in the geographic distribution of North Pacific gastropod assemblages through the Middle and Late Eocene indicate that only eastern Pacific Tethyan taxa were subjected to latitudinal range reduction. The distribution of cosmopolitan and North Pacific elements did not significantly change from the Middle to Late Eocene, which suggests a relatively stable environment and climate stability during that time. High-latitude Eocene gastropod assemblages from Western Kamchatka demonstrate a high level of endemism at the species level and a low-level of endemism on the genus level. This pattern is thought to be a result of the unrestricted migration of cosmopolitan taxa northward along the shallow-marine margin of the Pacific rim.
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Date Issued
2001-02-01
PURL
http://purl.flvc.org/fau/165898
Subject Headings
Geology, Stratigraphic--Paleogene, Paleontology--Paleogene, Geology--North Pacific Ocean, Gastropoda--North Pacific Ocean--Classification, Paleobiology, Biogeography
Format
Document (PDF)
A revision of the recent species of Exilia, formerly Benthovoluta (Gastropoda: Turbinellidae)
Title
A revision of the recent species of Exilia, formerly Benthovoluta (Gastropoda: Turbinellidae).
Creator
Oleinik, Anton E., Kantor, Yuri I., Bouchet, Philippe
Abstract/Description
The range of shell characters (overall shape, sculpture, columellar plaits, protoconchs) exhibited by fossil and Recent species placed in Exilia Conrad, 1860, Mitraefusus Bellardi, 1873, Mesorhytis Meek, 1876, Surculina Dall, 1908, Phenacoptygma Dall, 1918, Palaeorhaphis Stewart, 1927, Zexilia Finlay, 1926, Graphidula Stephenson, 1941, Benthovoluta Kuroda et Habe, 1950, and Chathamidia Dell, 1956 and the anatomy of the Recent species precludes separation of more than one genus. Consequently...
Show moreThe range of shell characters (overall shape, sculpture, columellar plaits, protoconchs) exhibited by fossil and Recent species placed in Exilia Conrad, 1860, Mitraefusus Bellardi, 1873, Mesorhytis Meek, 1876, Surculina Dall, 1908, Phenacoptygma Dall, 1918, Palaeorhaphis Stewart, 1927, Zexilia Finlay, 1926, Graphidula Stephenson, 1941, Benthovoluta Kuroda et Habe, 1950, and Chathamidia Dell, 1956 and the anatomy of the Recent species precludes separation of more than one genus. Consequently all of these nominal genera are synonymised with Exilia, with a stratigraphical range from Late Cretaceous to Recent.
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Date Issued
2001
PURL
http://purl.flvc.org/fcla/dt/210412
Subject Headings
Mollusks, Fossil--Type specimens, Gastropoda--Classification, Exilia. [from old catalog], Fossils--Classification, Paleontology--Neocene
Format
Document (PDF)
The Genus Fulgoraria (Gastropoda: Volutidae) of the northeastern Kamchatka Peninsula and Sakhalin Island, with notes on the paleoecology and distribution of the subfamily Fulgorariinae in the Oligocene of the northern Pacific
Title
The Genus Fulgoraria (Gastropoda: Volutidae) of the northeastern Kamchatka Peninsula and Sakhalin Island, with notes on the paleoecology and distribution of the subfamily Fulgorariinae in the Oligocene of the northern Pacific.
Creator
Oleinik, Anton E.
Abstract/Description
A review of the Oligocene biogeography of northern fulgorariines along the northern Pacific margin, including the western coast of North America, indicates that this subfamily had a much broader distribution during late Paleogene time than today. These data point to more favorable climatic conditions (including lower water temperatures) for dispersal of fulgorariine volutes during the Oligocene.
Date Issued
1993
PURL
http://purl.flvc.org/fau/165935
Subject Headings
Biogeography--North Pacific Ocean, Gastropoda--North Pacific--Classification, Mollusks, Fossil--Pacific Area, Geology, Stratigraphic--Oligocene, Mollusks--Geographical distribution, Paleoecology
Format
Document (PDF)
A refined age for the earliest opening of Bering Strait
Title
A refined age for the earliest opening of Bering Strait.
Creator
Oleinik, Anton E., Gladenkov, Andrey Yu, Marincovich, Louie, Jr., Barinov, Konstantin B.
Abstract/Description
Biostratigraphically and chronostratigraphically important diatoms from the Milky River Formation, Alaska Peninsula, southwestern Alaska, imply an age range of 5.4-5.5 Ma for the oldest North Pacific Cenozoic occurrence of the marine bivalve mollusk Astarte, which migrated from the Arctic Ocean into the North Pacific when Bering Strait first flooded. The data presented here are a refinement of the age range of 4.8-5.5 Ma reported earlier and imply that Bering Strait first opened very near the...
Show moreBiostratigraphically and chronostratigraphically important diatoms from the Milky River Formation, Alaska Peninsula, southwestern Alaska, imply an age range of 5.4-5.5 Ma for the oldest North Pacific Cenozoic occurrence of the marine bivalve mollusk Astarte, which migrated from the Arctic Ocean into the North Pacific when Bering Strait first flooded. The data presented here are a refinement of the age range of 4.8-5.5 Ma reported earlier and imply that Bering Strait first opened very near the end of the Miocene at 5.32 Ma.
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PURL
http://purl.flvc.org/fau/165902
Subject Headings
Paleoecology--Bering Sea Region, Diatoms, Fossil--North Pacific Region, Geology, Stratigraphic--Miocene, Paleoceanography--North Pacific Region, Mollusks, Fossil--Arctic Ocean
Format
Document (PDF)
Magnitude of Middle Miocene warming in North Pacific high latitudes: stable isotope evidence from Kaneharaia (Bivalvia, Dosiniinae)
Title
Magnitude of Middle Miocene warming in North Pacific high latitudes: stable isotope evidence from Kaneharaia (Bivalvia, Dosiniinae).
Creator
Oleinik, Anton E., Marincovich, Louie, Jr., Barinov, Konstantin B., Swart, Peter K.
Abstract/Description
The Middle Miocene Climatic Optimum (MMCO) at ~ 16 Ma was the warmest interval during the Neogene. The peak of the MMCO in the North Pacific is marked by the appearance of the bivalve genus Kaneharaia (Bivalvia, Dosiniinae) in the high-latitude regions of Kamchatka and Alaska (55 –65°N). Specimens of Kaneharaia sp. were collected from two early middle Miocene high-latitude localities in the North Pacific – the Sea urchin Horizon of northwestern Kamchatka and the Narrow Cape Formation of...
Show moreThe Middle Miocene Climatic Optimum (MMCO) at ~ 16 Ma was the warmest interval during the Neogene. The peak of the MMCO in the North Pacific is marked by the appearance of the bivalve genus Kaneharaia (Bivalvia, Dosiniinae) in the high-latitude regions of Kamchatka and Alaska (55 –65°N). Specimens of Kaneharaia sp. were collected from two early middle Miocene high-latitude localities in the North Pacific – the Sea urchin Horizon of northwestern Kamchatka and the Narrow Cape Formation of Alaska. Middle Miocene Kaneharaia specimens were incrementally sampled for oxygen and carbon stable isotope records of seasonality. Results were compared with stable isotope profiles constructed for two Recent species of Dosinia from subtropical waters.
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PURL
http://purl.flvc.org/fcla/dt/210410
Subject Headings
Biogeography--North Pacific Ocean, Mollusks, Fossils--North Pacific Ocean, Sediments (Geology)--North Pacific Ocean, Paleoclimatology--Miocene, Climatic changes--North Pacific Ocean
Format
Document (PDF)