Search Results - "Thomas, Deborah J."
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Nd isotopic structure of the Pacific Ocean 70-30 Ma and numerical evidence for vigorous ocean circulation and ocean heat transport in a greenhouse world
Published in Paleoceanography (01-05-2014)“…The oceanic meridional overturning circulation (MOC) is a crucial component of the climate system, impacting heat and nutrient transport, and global carbon…”
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Outpatient Total Hip Arthroplasty
Published in The Journal of arthroplasty (01-06-2010)“…Abstract Patients younger than 65 years were studied to determine what percentage of patients would enroll in a study of outpatient total hip arthroplasty, its…”
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Cretaceous deep-water formation in the Indian sector of the Southern Ocean
Published in Paleoceanography (01-03-2012)“…The role that meridional overturning circulation (MOC) patterns played in poleward heat transport during the extreme warmth of the Early to Late Cretaceous is…”
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Evidence for deep-water production in the North Pacific Ocean during the early Cenozoic warm interval
Published in Nature (01-07-2004)“…The deep-ocean circulation is responsible for a significant component of global heat transport. In the present mode of circulation, deep waters form in the…”
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Neodymium Evidence for Increased Circumpolar Deep Water Flow to the North Pacific During the Middle Miocene Climate Transition
Published in Paleoceanography and paleoclimatology (01-07-2018)“…Low salinity surface water inhibits local deepwater formation in the modern North Pacific. Instead, southern‐sourced Circumpolar Deep Water (CDW) fills the…”
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From Public-Private Virtue to Cultural-Corporate Amoeba: Mr Blobby and the Rise of BBC Worldwide During the 1990s
Published in Historical journal of film, radio, and television (03-04-2018)“…In 1991, a BBC taskforce inquired into the organization's efficiency. One of its reports, BBC the Entrepreneur, observed that 'commerce is no longer…”
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Geographically different oceanographic responses to global warming during the Cenomanian–Turonian interval and Oceanic Anoxic Event 2
Published in Palaeogeography, palaeoclimatology, palaeoecology (01-10-2014)“…Oceanic Anoxic Event (OAE) 2 coincided with the Cenomanian–Turonian boundary ~93.9Ma, and was one of the two most prominent and globally significant of the…”
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Thorium-derived dust fluxes to the tropical Pacific Ocean, 58Ma
Published in Geochimica et cosmochimica acta (15-06-2012)“…Eolian dust in pelagic deep sea sediments can be used to reconstruct ancient wind patterns and paleoenvironmental response to climate change. Traditional…”
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The negligible role of intermediate water circulation in stadial–interstadial oxygenation variations along the southern California margin: Evidence from Nd isotopes
Published in Quaternary science reviews (01-09-2010)“…Changes in the source of intermediate waters to the southern California margin may have caused variations in seafloor oxygen levels on stadial–interstadial…”
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Neogene evolution of Atlantic thermohaline circulation: Perspective from Walvis Ridge, southeastern Atlantic Ocean
Published in Paleoceanography (01-06-2007)“…We present new Nd isotope records from Walvis Ridge Ocean Drilling Program (ODP) sites 1262–1264 (southeastern Atlantic) spanning the past 24 Ma to investigate…”
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Neodymium isotopic reconstruction of late Paleocene–early Eocene thermohaline circulation
Published in Earth and planetary science letters (01-04-2003)“…High-resolution, fish tooth Nd isotopic records for eight Deep Sea Drilling Project and Ocean Drilling Program sites were used to reconstruct the nature of…”
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Framing the 'melancomic': character, aesthetics and affect in Wes Anderson's Rushmore
Published in New review of film and television studies (01-03-2012)“…Using Wes Anderson's Rushmore (1998) as a case study, this paper will examine the relationship between irony and affect, and the way the tension between these…”
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Thorium-derived dust fluxes to the tropical Pacific Ocean, 58 Ma
Published in Geochimica et cosmochimica acta (15-06-2012)“…Eolian dust in pelagic deep sea sediments can be used to reconstruct ancient wind patterns and paleoenvironmental response to climate change. Traditional…”
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Extraterrestrial 3He in Paleocene sediments from Shatsky Rise: Constraints on sedimentation rate variability
Published in Earth and planetary science letters (01-09-2009)“…We attempt to constrain the variability of the flux of extraterrestrial 3He in the Paleocene by studying sediments from Shatsky Rise (Ocean Drilling Program,…”
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The Maastrichtian record from Shatsky Rise (northwest Pacific): A tropical perspective on global ecological and oceanographic changes
Published in Paleoceanography (01-03-2005)“…We present new isotopic and micropaleontological data from a depth transect on Shatsky Rise that record the response of the tropical Pacific to global biotic…”
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Nd isotopic structure of the Pacific Ocean 40–10 Ma, and evidence for the reorganization of deep North Pacific Ocean circulation between 36 and 25 Ma
Published in Earth and planetary science letters (01-09-2019)“…Early Paleogene neodymium (Nd) isotopic reconstructions of ocean circulation in the Pacific suggest a bipolar mode of overturning circulation characterized by…”
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Extinction, dissolution, and possible ocean acidification prior to the Cretaceous/Paleogene (K/Pg) boundary in the tropical Pacific
Published in Palaeogeography, palaeoclimatology, palaeoecology (01-11-2017)“…Biotic perturbations and changes in ocean circulation during the Maastrichtian stage of the latest Cretaceous raise questions about whether the biosphere was…”
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Radiogenic isotope composition of Carboniferous seawater from North American epicontinental seas
Published in Palaeogeography, palaeoclimatology, palaeoecology (15-01-2013)“…Abundant marine sedimentary deposits accumulated in the epeiric seas of North America during the Carboniferous Period (359–299Ma) when the Earth's climate…”
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New evidence for subtropical warming during the Late Paleocene thermal maximum: Stable isotopes from Deep Sea Drilling Project Site 527, Walvis Ridge
Published in Paleoceanography (01-10-1999)“…The late Paleocene thermal maximum (LPTM) was a dramatic, short‐term global warming event that occurred ∼55 Ma. Warming of high‐latitude surface waters and…”
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