Calcium Carbonates

Larry C. Peterson

doi:10.1016/B978-0-12-409548-9.11520-9

Calcium Carbonates

Larry C. Peterson

Research output: Chapter in Book/Report/Conference proceeding › Chapter

1 Scopus citations

Abstract

Calcium carbonate in ocean sediments is dominantly produced by shell-and skeleton-building organisms in both shallow marine and open-ocean environments. The carbonate oozes that accumulate on the sea floor serve as a major reservoir of calcium and carbon dioxide on the Earth’s surface. Their spatial and temporal accumulation patterns in the marine sediment record are a primary source of information about the carbonate chemistry and circulation of past oceans, as well as of the global geochemical cycle of CO₂.

Original language	English (US)
Title of host publication	Encyclopedia of Ocean Sciences
Publisher	Elsevier
Pages	53-61
Number of pages	9
ISBN (Electronic)	9780128130810
ISBN (Print)	9780128130827
DOIs	https://doi.org/10.1016/B978-0-12-409548-9.11520-9
State	Published - Jan 1 2019
Externally published	Yes

Keywords

Aragonite
Basin-To-Basin fractionation
Calcite
Carbon cycle
Carbonate compensation depth
Carbonate ooze
Carbonate saturation
Chalk
Coccolithophorids
Diagenesis
Dissolution
Foraminifera
Glacial cycles
Limestone
Lysocline

ASJC Scopus subject areas

Earth and Planetary Sciences(all)

UN SDGs

This output contributes to the following UN Sustainable Development Goals (SDGs)

Access to Document

10.1016/B978-0-12-409548-9.11520-9

Cite this

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title = "Calcium Carbonates",

abstract = "Calcium carbonate in ocean sediments is dominantly produced by shell-and skeleton-building organisms in both shallow marine and open-ocean environments. The carbonate oozes that accumulate on the sea floor serve as a major reservoir of calcium and carbon dioxide on the Earth{\textquoteright}s surface. Their spatial and temporal accumulation patterns in the marine sediment record are a primary source of information about the carbonate chemistry and circulation of past oceans, as well as of the global geochemical cycle of CO2.",

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year = "2019",

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doi = "10.1016/B978-0-12-409548-9.11520-9",

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T1 - Calcium Carbonates

AU - Peterson, Larry C.

PY - 2019/1/1

Y1 - 2019/1/1

N2 - Calcium carbonate in ocean sediments is dominantly produced by shell-and skeleton-building organisms in both shallow marine and open-ocean environments. The carbonate oozes that accumulate on the sea floor serve as a major reservoir of calcium and carbon dioxide on the Earth’s surface. Their spatial and temporal accumulation patterns in the marine sediment record are a primary source of information about the carbonate chemistry and circulation of past oceans, as well as of the global geochemical cycle of CO2.

AB - Calcium carbonate in ocean sediments is dominantly produced by shell-and skeleton-building organisms in both shallow marine and open-ocean environments. The carbonate oozes that accumulate on the sea floor serve as a major reservoir of calcium and carbon dioxide on the Earth’s surface. Their spatial and temporal accumulation patterns in the marine sediment record are a primary source of information about the carbonate chemistry and circulation of past oceans, as well as of the global geochemical cycle of CO2.

KW - Aragonite

KW - Basin-To-Basin fractionation

KW - Calcite

KW - Carbon cycle

KW - Carbonate compensation depth

KW - Carbonate ooze

KW - Carbonate saturation

KW - Chalk

KW - Coccolithophorids

KW - Diagenesis

KW - Dissolution

KW - Foraminifera

KW - Glacial cycles

KW - Limestone

KW - Lysocline

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UR - http://www.scopus.com/inward/citedby.url?scp=85079081737&partnerID=8YFLogxK

U2 - 10.1016/B978-0-12-409548-9.11520-9

DO - 10.1016/B978-0-12-409548-9.11520-9

M3 - Chapter

SN - 9780128130827

SP - 53

EP - 61

BT - Encyclopedia of Ocean Sciences

PB - Elsevier

ER -

Calcium Carbonates

Abstract

Keywords

ASJC Scopus subject areas

UN SDGs

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