Mathis P. Hain

About Mathis P. Hain

Mathis P. Hain, With an exceptional h-index of 23 and a recent h-index of 21 (since 2020), a distinguished researcher at University of California, Santa Cruz, specializes in the field of Paleoceanography, Paleoclimate, Geochemistry.

His recent articles reflect a diverse array of research interests and contributions to the field:

Deglacial Pulse of Neutralized Carbon From the Pacific Seafloor: A Natural Analog for Ocean Alkalinity Enhancement?

Continuous records of δ11B-CO2 covering the Plio-Pleistocene boundary and the Mid Pleistocene Transition show orbital carbon-climate coupling.

Continuous atmospheric CO2 across the Mid Pleistocene Transition from boron isotopes: decoupling of CO2 from insolation and temperature

Ocean oxygen, preformed nutrients, and the cause of the lower carbon dioxide concentration in the atmosphere of the last glacial maximum

Orbital CO2 reconstruction using boron isotopes during the late Pleistocene, an assessment of accuracy

Primary Dolomite Formation Mechanisms: Insight from Biogeochemical Characterization of Dolomite-Forming Lagoons

Characterizing Geologic Carbon Release as an Explanation for Deglacial Δ14C Anomalies within the Eastern Tropical North Pacific

Global reorganization of deep-sea circulation and carbon storage after the last ice age

Mathis P. Hain Information

University

Position

Earth & Planetary Sciences

Citations(all)

3286

Citations(since 2020)

1895

Cited By

2096

hIndex(all)

23

hIndex(since 2020)

21

i10Index(all)

31

i10Index(since 2020)

30

Email

University Profile Page

Google Scholar

Mathis P. Hain Skills & Research Interests

Paleoceanography

Paleoclimate

Geochemistry

Top articles of Mathis P. Hain

Deglacial Pulse of Neutralized Carbon From the Pacific Seafloor: A Natural Analog for Ocean Alkalinity Enhancement?

Authorea Preprints

2023/4/30

Continuous records of δ11B-CO2 covering the Plio-Pleistocene boundary and the Mid Pleistocene Transition show orbital carbon-climate coupling.

2024/3/7

Continuous atmospheric CO2 across the Mid Pleistocene Transition from boron isotopes: decoupling of CO2 from insolation and temperature

2024/3/7

Ocean oxygen, preformed nutrients, and the cause of the lower carbon dioxide concentration in the atmosphere of the last glacial maximum

Paleoceanography and Paleoclimatology

2024/1

Orbital CO2 reconstruction using boron isotopes during the late Pleistocene, an assessment of accuracy

Climate of the Past Discussions

2023/1/5

Primary Dolomite Formation Mechanisms: Insight from Biogeochemical Characterization of Dolomite-Forming Lagoons

AGU Fall Meeting Abstracts

2022/12

Characterizing Geologic Carbon Release as an Explanation for Deglacial Δ14C Anomalies within the Eastern Tropical North Pacific

AGU Fall Meeting 2022

2022/12/15

Global reorganization of deep-sea circulation and carbon storage after the last ice age

Science Advances

2022/11/16

Subglacial precipitates record Antarctic ice sheet response to late Pleistocene millennial climate cycles

Nature Communications

2022/9/15

The Southern Ocean during the ice ages: A slumped pycnocline from reduced wind-driven upwelling?

EGU General Assembly Conference Abstracts

2022/5

A Radiometrically Dated Record of Antarctic Ice Sheet Response to Millennial-Scale Climate Cycles during Glacials and Interglacials

2022/2/11

No ion is an island: Multiple ions influence boron incorporation into CaCO3

Geochimica et Cosmochimica Acta

2022

Ice age‐Holocene similarity of foraminifera‐bound nitrogen isotope ratios in the eastern equatorial Pacific

Paleoceanography and Paleoclimatology

2021/5

No ion is an island: Multiple ions involved during boron incorporation into CaCO3

EGU General Assembly Conference Abstracts

2021/4

A 35-million-year record of seawater stable Sr isotopes reveals a fluctuating global carbon cycle

Science

2021/3/26

The Southern Ocean during the ice ages: A review of the Antarctic surface isolation hypothesis, with comparison to the North Pacific

2021/2/15

PP12B-05 and CO2 14C-Constraints on the Deglacial Release of Geologic Carbon Using Atmospheric Records

AGU Fall Meeting

2021/1

Constraints on the Deglacial Release of Geologic Carbon Using Atmospheric 14C and CO2 Records

AGU Fall Meeting

2021/12

Reorganization of ocean overturning circulation during the Eocene Thermal Maximum 2

AGU Fall Meeting Abstracts

2021/12

See List of Professors in Mathis P. Hain University(University of California, Santa Cruz)

Co-Authors

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