Lower oceanic δ13C during the last interglacial period compared to the Holocene

Autor: Bengtson, Shannon A., Menviel, Laurie C., Meissner, Katrin J., Missiaen, Lise, Peterson, Carlye D., Lisiecki, Lorraine E., Joos, Fortunat

Publikováno v: Bengtson, Shannon A.; Menviel, Lauri C.; Meissner, Katrin J.; Missiaen, Lise; Peterson, Charlye D.; Lisiecki, Lorraine E.; Joos, Fortunat (2021). Lower oceanic δ13C during the last interglacial period compared to the Holocene. Climate of the past, 17(1), pp. 507-528. Copernicus Publications 10.5194/cp-17-507-2021
Climate Of The Past (1814-9324) (Copernicus GmbH), 2021-02, Vol. 17, N. 1, P. 507-528

The last time in Earth's history when high latitudes were warmer than during pre-industrial times was the last interglacial period (LIG, 129–116 ka BP). Since the LIG is the most recent and best documented interglacial, it can provide insights into

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::8f6ec76d9518d3b176cc543fb6f0dee6
https://boris.unibe.ch/152989/1/cp-17-507-2021.pdf

Variable C∕P composition of organic production and its effect on ocean carbon storage in glacial-like model simulations

Autor: Ödalen, Malin, Nycander, Jonas, Ridgwell, Andy, Oliver, Kevin I. C., Peterson, Carlye D., Nilsson, Johan

During the four most recent glacial maxima, atmospheric CO2 has been lowered by about 90–100 ppm with respect to interglacial concentrations. It is likely that most of the atmospheric CO2 deficit was stored in the ocean. Changes in the biological p

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=od_______348::02ff94b0162c1d60b28e84db29b5212d
https://eprints.soton.ac.uk/444432/

Benthic foraminiferal stable carbon isotope constraints on deglacial ocean circulation and carbon-cycle changes

Autor: Peterson, Carlye D., Gebbie, G., Lisiecki, L. E., Lynch Stieglitz, J., Oppo, D., Muglia, Juan, Repschläger, Janne, Schmittner, A.

Publikováno v: CONICET Digital (CONICET)
Consejo Nacional de Investigaciones Científicas y Técnicas
instacron:CONICET

How does deep-ocean circulation influence atmospheric CO2 across deglacial transitions? Although biogeochemical and physical processes complicate interpretation of foraminiferal stable carbon isotope data, these complications can be addressed with ex

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=od______3056::0315c42a196ae475c57aaa885a4c6de3
http://pastglobalchanges.org/products/pages-magazine/12919

Deglacial carbon cycle is observed in a compilation of 127 benthic delta C-13 time series (20-6 ka)

Autor: Peterson, Carlye D, Lisiecki, Lorraine E

Publikováno v: CLIMATE OF THE PAST, vol 14, iss 8

We present a compilation of 127 time series δ13C records from Cibicides wuellerstorfi spanning the last deglaciation (20–6 ka) which is well-suited for reconstructing large-scale carbon cycle changes, especially for comparison with isotope-enabled

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=od_______325::336b41e76fb964983bcd00a248979788
https://escholarship.org/uc/item/37r4g8xz

Lower oceanic δ13C during the last interglacial period compared to the Holocene.

Autor: Bengtson, Shannon A., Menviel, Laurie C., Meissner, Katrin J., Missiaen, Lise, Peterson, Carlye D., Lisiecki, Lorraine E., Joos, Fortunat

Publikováno v: Climate of the Past; 2021, Vol. 17 Issue 1, p507-528, 22p