Bathyal ostracodes from the Florida-Hatteras slope, the Straits of Florida, and the Blake Plateau
References (41)
Preliminary report on the study of abyssal ostracodes
TheBradleya problem, with descriptions of two new psychrospheric ostracode genera,Agrenocythere andPoseidonamicus (Ostracoda: Crustacea)
Smithson. Contrib. Paleobiol.
(1972)In search of lost oceans: a paradox in discovery
Form, function, and architecture of ostracode shells
Ann. Rev. Earth Planet. Sci.
(1981)Estimating greater paleodepths with ostracodes, especially in past thermospheric oceans
Palaeogeograph., Palaeoclimatol., Palaeoecol.
(1983)- et al.
Arthropoda, article 2, recent marine ostracodes from the eastern Gulf of Mexico
Univ. Kans. Paleontol. Contrib.
(1963) - et al.
Deep-sea ostracodes and the transformation of ocean to sea in the Tethys
Distribution of marine podocopid Ostracoda in the Gulf of Mexico and the Caribbean
The Distribution of Ostracodes in the Bottom Sediments of the Adriatic Sea
The distribution pattern of minimum oxygen concentrations in the Atlantic
Oceanology
(1966)
Species diversity: benthonic foraminifera in western North Atlantic
Science
La ostracofauna Plio-Pleistocenica della sezione vrica in Carabria (con considerazioni sul limite Neogene/Quaternario)
Estratto Dal Bollettino Della Societa Paleontologica Italiana
Late Pleistocene marginal marine ostracodes from the southeastern Atlantic coastal plain and their paleoenvironmental implications
Geographie Physique et Quaternaire
Sedimentation on the eastern United States continental slope
Atlantic continental shelf and slope of the United States: Geologic background
U.S. Geol. Surv. Prof. Pap.
Zoogeography of holocene Cytheracean ostracodes in the bays of Texas
J. Paleontol.
Data File, Continental Margin Program, Atlantic Coast of the United States
Regional clay mineral facies in estuaries and continental margin of the United States east coast
Geol. Soc. Am. Mem.
Atlantic continental shelf and slope of the United States — ostracode zoogeography in the southern Nova Scotian and northern Virginian faunal provinces
U.S. Geol. Surv. Prof. Pap.
Ostracode biofacies in the Cape Hatteras, North Carolina, area
Bull. Am. Paleont.
Cited by (85)
BATHYAL OSTRACODS FROM THE UPPER PLEISTOCENE OF THE RIO GRANDE CONE, PELOTAS BASIN, BRAZIL
2021, Revue de MicropaleontologieTaxonomy and climatic zonation of the Late Quaternary bathyal ostracods from the Campos Basin, Brazil
2017, Revue de MicropaleontologieCitation Excerpt :Biozone Y (LGM). Remarks: This species is similar to Pedicythere sp. recorded by Cronin (1983). However, as a different valve is represented in that work, a more conclusive statement is not possible.
Latest Cretaceous/Paleocene deep-sea ostracode fauna at IODP Site U1407 (western North Atlantic) with special reference to the Cretaceous/Paleogene boundary and the Latest Danian Event
2017, Marine MicropaleontologyCitation Excerpt :Among the taxa with the negative scores, Bythoceratina increases its relative abundance under the low-food supply condition in the North Atlantic during the Quaternary glacial periods (Didié et al., 2002). Aratrocypris adapts to a broad trophic condition, since Cronin (1983) and Alvarez Zarikian (2015) reported living and fossil Aratrocypris from sediments off Florida with high food supply and in the oligotrophic South Pacific Gyre, respectively. Cardobairdia dwells in seafloors with oligotrophic conditions, because it lives in carbonate caves and tropical coral reefs (e.g., Tabuki and Hanai, 1999).
Vertical distribution of living ostracods in deep-sea sediments, North Atlantic Ocean
2017, Deep-Sea Research Part I: Oceanographic Research PapersLevantine intermediate water hydrodynamic and bottom water ventilation in the northern Tyrrhenian Sea over the past 56,000 years: New insights from benthic foraminifera and ostracods
2015, Quaternary InternationalCitation Excerpt :In addition, this hypothesis is supported by maxima of ostracod clusters B1 and B2 (Fig. 7), including Paracypris sp. and. Argilloecia acuminata, species adapted to poorly oxygenated environments (Cronin, 1983; Andreu, 1992; Alvarez Zarikian et al., 2009). Benthic foraminifera of cluster 3b (B. marginata, B. costata and G. altiformis) also increase in abundance during Is (Fig. 6) suggesting reduced oxygenation.