Paleoproductivity during the middle Miocene carbon isotope events: A data-model approach

Diester-Haass, Liselotte; Billups, Katharina; Jacquemin, Ingrid; Emeis, Kay C.; Lefebvre, Vincent; François, Louis

doi:10.1002/palo.20033

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Paleoproductivity during the middle Miocene carbon isotope events: A data-model approach

Diester-Haass, Liselotte; Billups, Katharina; Jacquemin, Ingrid et al.

2013 • In Paleoceanography, 28, p. 334-346

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10.1002/palo.20033

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Keywords :

Mid-Miocene; ocean productivity; carbon cycle; carbon isotopic composition; Milankovitch cycles

Abstract :

[en] To what extent are individual middle Miocene eccentricity-scale benthic foraminiferal carbon isotope maxima (the so-called CM events) related to changes in marine export productivity? Here we use benthic foraminiferal accumulation rates from three sites in the Pacific and Southern Oceans and a geochemical box model to assess relationships between benthic foraminiferal δ13C records, export productivity, and the global carbon cycle. Results from Deep Sea Drilling Project Hole 588 and Ocean Drilling Program Site 747 show a distinct productivity maximum during CM 6 at 13.8 Ma, the time of major expansion of ice on Antarctica. Productivity maxima during other CM events are only recorded at high-latitude Site 747. A set of numerical experiments tests whether changes in foraminiferal δ13C records (CM events) and export productivity can be simulated solely by sea level fluctuations and the associated changes in global weathering-deposition cycles, by sea level fluctuations plus global climatic cooling, and by sea level fluctuations plus invigorated ocean circulation. Consistent with data, the periodic forcing of sea level and albedo (and associated weathering cycles) produces δ13C variations of the correct temporal spacing, albeit with a reduced amplitude. A productivity response of the correct magnitude is achieved by enhancing ocean circulation during cold periods. We suggest that the pacing of middle Miocene δ13C fluctuations is associated with cyclical sea level variations. The amplitude, however, is muted perhaps due to the competing effects of a time-lagged response to sea level lowstands but an immediate response to invigorated ocean circulation during cold phases.

Disciplines :

Earth sciences & physical geography

Author, co-author :

Diester-Haass, Liselotte; Universität des Saarlandes, Germany > Zentrum für Umweltwissenschaften

Billups, Katharina

Jacquemin, Ingrid ; Université de Liège - ULiège > DER Sc. et gest. de l'environnement (Arlon Campus Environ.) > Agrométéorologie (relation agriculture-environ. physique)

Emeis, Kay C.

Lefebvre, Vincent

François, Louis ; Université de Liège - ULiège > Département d'astrophys., géophysique et océanographie (AGO) > Modélisation du climat et des cycles biogéochimiques

Language :

English

Title :

Paleoproductivity during the middle Miocene carbon isotope events: A data-model approach

Publication date :

2013

Journal title :

Paleoceanography

ISSN :

0883-8305

eISSN :

1944-9186

Publisher :

American Geophysical Union, Washington, United States - District of Columbia

Volume :

Pages :

334-346

Peer reviewed :

Peer Reviewed verified by ORBi

Available on ORBi :

since 10 July 2013

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