Mapping Human Movement using Stable Oxygen Isotopic Ratio Mass Spectrometry: Potential Application to Forensic Science Demonstrated by a Modern Horse-Human Study

Table S1: Stable oxygen isotopic data of each conodont measured using SIMS; Table S2: Stable oxygen isotopic data using SIMS of the Durango apatite standard and a modern shark tooth; Figure S1: Cross plot of d18Omean values and OH/16O from the Shingle Pass (blue), Antelope Range (green), and Cincinnati Arch (white) sections.

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Proposal of Simple Measurement Method for Evaporation Rate by Using Oxygen Isotopic Ratio

International Journal of Geomate ◽

10.21660/2012.5.1265 ◽

2012 ◽

Author(s):

Satoshi Miyahara

Keyword(s):

Measurement Method ◽

Evaporation Rate ◽

Isotopic Ratio ◽

Simple Measurement ◽

Oxygen Isotopic ◽

Oxygen Isotopic Ratio

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Combining physical and geochemical methods to investigate lower halocline water formation and modification along the Siberian continental slope

Ocean Science ◽

10.5194/os-13-983-2017 ◽

2017 ◽

Vol 13 (6) ◽

pp. 983-995 ◽

Cited By ~ 5

Author(s):

Matthew B. Alkire ◽

Igor Polyakov ◽

Robert Rember ◽

Andrey Pnyushkov ◽

Vladimir Ivanov ◽

...

Keyword(s):

Isotopic Ratio ◽

Characteristic Temperature ◽

Potential Temperature ◽

Atlantic Water ◽

Anna Trough ◽

Oxygen Isotopic ◽

Stable Oxygen ◽

And Shifts ◽

Severnaya Zemlya ◽

Physical And Chemical

Abstract. A series of cross-slope transects were occupied in 2013 and 2015 that extended eastward from St. Anna Trough to the Lomonosov Ridge. High-resolution physical and chemical observations collected along these transects revealed fronts in the potential temperature and the stable oxygen isotopic ratio (δ18O) that were observed north of Severnaya Zemlya (SZ). Using linear regressions, we describe mixing regimes on either side of the front that characterize a transition from a seasonal halocline to a permanent halocline. This transition describes the formation of lower halocline water (LHW) and the cold halocline layer via a mechanism that has been previously postulated by Rudels et al. (1996). Initial freshening of Atlantic Water (AW) by sea-ice meltwater occurs west of SZ, whereas higher influences of meteoric water and brine result in a transition to a separate mixing regime that alters LHW through mixing with overlying waters and shifts the characteristic temperature–salinity bend from higher (34.4  ≤  S  ≤  34.5) toward lower (34.2  ≤  S  ≤  34.3) salinities. These mixing regimes appear to have been robust since at least 2000.

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Determination of nitrate isotopic signature in waters of different sources by analysing the nitrogen and oxygen isotopic ratio

Environmental Science Processes & Impacts ◽

10.1039/c3em30920g ◽

2013 ◽

Vol 15 (4) ◽

pp. 751 ◽

Cited By ~ 6

Author(s):

Piotr Koszelnik ◽

Renata Gruca-Rokosz

Keyword(s):

Isotopic Ratio ◽

Isotopic Signature ◽

Oxygen Isotopic ◽

Different Sources ◽

Oxygen Isotopic Ratio

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Supplemental Material: Oxygen isotope (d18O) trends measured from Ordovician conodont apatite using secondary ion mass spectrometry (SIMS): Implications for paleo-thermometry studies

10.1130/gsab.s.14356757.v1 ◽

2021 ◽

Author(s):

Cole T Edwards ◽

et al.

Keyword(s):

Mass Spectrometry ◽

Oxygen Isotope ◽

Secondary Ion Mass Spectrometry ◽

Isotopic Data ◽

Ion Mass Spectrometry ◽

Oxygen Isotopic ◽

Stable Oxygen ◽

Secondary Ion

Table S1: Stable oxygen isotopic data of each conodont measured using SIMS; Table S2: Stable oxygen isotopic data using SIMS of the Durango apatite standard and a modern shark tooth; Figure S1: Cross plot of d18Omean values and OH/16O from the Shingle Pass (blue), Antelope Range (green), and Cincinnati Arch (white) sections.

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