Productivity response of calcareous nannoplankton to Eocene Thermal Maximum 2 (ETM2)

M. Dedert; H. Stoll; D. Kroon; N. Shimuzu; K. Kanamaru; P. Ziveri

doi:10.5194/cp-8-977-2012

Productivity response of calcareous nannoplankton to Eocene Thermal Maximum 2 (ETM2)

M. Dedert
, H. Stoll
, D. Kroon
, N. Shimuzu
, K. Kanamaru
, P. Ziveri

Earth and Climate

Research output: Contribution to Journal › Article › Academic › peer-review

Abstract

The Early Eocene Thermal Maximum 2 (ETM2) at ∼53.7 Ma is one of multiple hyperthermal events that followed the Paleocene-Eocene Thermal Maximum (PETM, ∼56 Ma). The negative carbon excursion and deep ocean carbonate dissolution which occurred during the event imply that a substantial amount (103 Gt) of carbon (C) was added to the ocean-atmosphere system, consequently increasing atmospheric CO

Original language	English
Pages (from-to)	977-993
Journal	Climate of the Past
Volume	8
DOIs	https://doi.org/10.5194/cp-8-977-2012
Publication status	Published - 2011

UN SDGs

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

SDG 14 Life Below Water

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10.5194/cp-8-977-2012

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title = "Productivity response of calcareous nannoplankton to Eocene Thermal Maximum 2 (ETM2)",

abstract = "The Early Eocene Thermal Maximum 2 (ETM2) at ∼53.7 Ma is one of multiple hyperthermal events that followed the Paleocene-Eocene Thermal Maximum (PETM, ∼56 Ma). The negative carbon excursion and deep ocean carbonate dissolution which occurred during the event imply that a substantial amount (103 Gt) of carbon (C) was added to the ocean-atmosphere system, consequently increasing atmospheric CO",

author = "M. Dedert and H. Stoll and D. Kroon and N. Shimuzu and K. Kanamaru and P. Ziveri",

year = "2011",

doi = "10.5194/cp-8-977-2012",

language = "English",

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journal = "Climate of the Past",

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AU - Dedert, M.

AU - Stoll, H.

AU - Kroon, D.

AU - Shimuzu, N.

AU - Kanamaru, K.

AU - Ziveri, P.

PY - 2011

Y1 - 2011

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AB - The Early Eocene Thermal Maximum 2 (ETM2) at ∼53.7 Ma is one of multiple hyperthermal events that followed the Paleocene-Eocene Thermal Maximum (PETM, ∼56 Ma). The negative carbon excursion and deep ocean carbonate dissolution which occurred during the event imply that a substantial amount (103 Gt) of carbon (C) was added to the ocean-atmosphere system, consequently increasing atmospheric CO

U2 - 10.5194/cp-8-977-2012

DO - 10.5194/cp-8-977-2012

M3 - Article

SN - 1814-9324

VL - 8

SP - 977

EP - 993

JO - Climate of the Past

JF - Climate of the Past

ER -

Productivity response of calcareous nannoplankton to Eocene Thermal Maximum 2 (ETM2)

Abstract

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