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Journal ArticleDOI

Sea-level and deep water temperature changes derived from benthic foraminifera isotopic records

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TLDR
In this paper, robust regressions were established between relative sea-level (RSL) data and benthic foraminifera oxygen isotopic ratios from the North Atlantic and Equatorial Pacific Ocean over the last climatic cycle.
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This article is published in Quaternary Science Reviews.The article was published on 2002-01-01. It has received 1908 citations till now. The article focuses on the topics: North Atlantic Deep Water & Thermohaline circulation.

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The Last Glacial Maximum.

TL;DR: The responses of the Northern and Southern Hemispheres differed significantly, which reveals how the evolution of specific ice sheets affected sea level and provides insight into how insolation controlled the deglaciation.
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Sea level and global ice volumes from the Last Glacial Maximum to the Holocene.

TL;DR: From ∼1,000 observations of sea level, allowing for isostatic and tectonic contributions, this work quantified the rise and fall in global ocean and ice volumes for the past 35,000 years and provides new constraints on the fluctuation of ice volume in this interval.
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Sea-level fluctuations during the last glacial cycle

TL;DR: A hydraulic model of the water exchange between the Red Sea and the world ocean is used to derive the sill depth—and hence global sea level—over the past 470,000 years, finding that sea-level changes of up to 35 m occurred, coincident with abrupt changes in climate.
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A Semi-Empirical Approach to Projecting Future Sea-Level Rise

TL;DR: It is proposed that, for time scales relevant to anthropogenic warming, the rate of sea-level rise is roughly proportional to the magnitude of warming above the temperatures of the pre–Industrial Age, with a proportionality constant of 3.4 millimeters/year per °C.
References
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Journal ArticleDOI

A 17,000-year glacio-eustatic sea level record: influence of glacial melting rates on the Younger Dryas event and deep-ocean circulation

TL;DR: In this paper, a global oxygen isotope record for ocean water has been calculated from the Barbados sea level curve, allowing separation of the ice volume component common to all isotope records measured in deep-sea cores.
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INTCAL98 Radiocarbon Age Calibration, 24,000-0 cal BP

TL;DR: In this paper, the conversion of radiocarbon ages to calibrated (cal) ages for the interval 24,000-0 cal BP (Before Present, 0 cal BP = AD 1950) is discussed.
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Age dating and the orbital theory of the ice ages: Development of a high-resolution 0 to 300,000-year chronostratigraphy

TL;DR: Using the concept of "orbital tuning", a continuous, high-resolution deep-sea chronostratigraphy has been developed spanning the last 300,000 yr as mentioned in this paper.
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Macintosh Program performs time‐series analysis

TL;DR: A Macintosh computer program that can perform many time-series analysis procedures is now available on the Internet free of charge, originally designed for paleoclimatic time series.
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