[HTML][HTML] Soothsaying DOM: a current perspective on the future of oceanic dissolved organic carbon

S Wagner, F Schubotz, K Kaiser, C Hallmann… - Frontiers in marine …, 2020 - frontiersin.org
The vast majority of freshly produced oceanic dissolved organic carbon (DOC) is derived
from marine phytoplankton, then rapidly recycled by heterotrophic microbes. A small fraction …

Reasons behind the long-term stability of dissolved organic matter

T Dittmar - Biogeochemistry of marine dissolved organic matter, 2015 - Elsevier
Marine dissolved organic matter (DOM) is an enigmatic pool of carbon. It originates largely
from marine biota, but it contains more than a thousand times more carbon than all living …

Dissolved organic matter composition and photochemical transformations in the northern North Pacific Ocean

PM Medeiros, M Seidel, LC Powers… - Geophysical …, 2015 - Wiley Online Library
The composition and photochemical transformations of dissolved organic matter (DOM) in
the northern North Pacific Ocean were investigated at the molecular level using ultrahigh …

Revisiting the Middle Eocene Climatic Optimum “Carbon Cycle Conundrum” With New Estimates of Atmospheric pCO2 From Boron Isotopes

MJ Henehan, KM Edgar, GL Foster… - Paleoceanography …, 2020 - Wiley Online Library
Abstract The Middle Eocene Climatic Optimum (MECO) was a gradual warming event and
carbon cycle perturbation that occurred between 40.5 and 40.1 Ma. A number of …

Frequency, magnitude and character of hyperthermal events at the onset of the Early Eocene Climatic Optimum

V Lauretano, K Littler, M Polling, JC Zachos… - Climate of the …, 2015 - cp.copernicus.org
Recent studies have shown that the Early Eocene Climatic Optimum (EECO) was preceded
by a series of short-lived global warming events, known as hyperthermals. Here we present …

[HTML][HTML] Persistence of carbon release events through the peak of early Eocene global warmth

S Kirtland Turner, PF Sexton, CD Charles… - Nature Geoscience, 2014 - nature.com
Abstract The Early Eocene Climatic Optimum (53–50 million years ago) was preceded by
approximately six million years of progressive global warming. This warming was …

[HTML][HTML] A model for orbital pacing of methane hydrate destabilization during the Palaeogene

DJ Lunt, A Ridgwell, A Sluijs, J Zachos, S Hunter… - Nature …, 2011 - nature.com
A series of transient global warming events, occurred during the late Palaeocene and early
Eocene, about 59 to 50 million years ago. The events, although variable in magnitude, were …

Recalcitrant dissolved organic matter and its major production and removal processes in the ocean

R Cai, N Jiao - Deep Sea Research Part I: Oceanographic Research …, 2022 - Elsevier
Dissolved organic matter (DOM) in the ocean accounts for nearly 662 Pg of carbon, most of
which is formed into a long-lived carbon pool that plays an important role in carbon …

The middle Eocene climatic optimum (MECO): A multiproxy record of paleoceanographic changes in the southeast Atlantic (ODP Site 1263, Walvis Ridge)

F Boscolo Galazzo, E Thomas, M Pagani… - …, 2014 - Wiley Online Library
The middle Eocene climatic optimum (MECO,~ 40 Ma) was a transient period of global
warming that interrupted the secular Cenozoic cooling trend. We investigated the …

[HTML][HTML] Carbon sequestration during the Palaeocene–Eocene Thermal Maximum by an efficient biological pump

Z Ma, E Gray, E Thomas, B Murphy, J Zachos… - Nature …, 2014 - nature.com
A perturbation of the carbon cycle and biosphere, linked to globally increased temperatures
about 55.9 million years ago, characterized the Palaeocene–Eocene Thermal Maximum. Its …