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Flocculation with heterogeneous composition in water environments: a review
QN Ho, M Fettweis, KL Spencer, BJ Lee - Water Research, 2022 - Elsevier
Flocculation is a key process for controlling the fate and transport of suspended particulate
matter (SPM) in water environments and has received considerable attention in the field of …
matter (SPM) in water environments and has received considerable attention in the field of …
The Atlantic meridional overturning circulation and abrupt climate change
J Lynch-Stieglitz - Annual review of marine science, 2017 - annualreviews.org
Abrupt changes in climate have occurred in many locations around the globe over the last
glacial cycle, with pronounced temperature swings on timescales of decades or less in the …
glacial cycle, with pronounced temperature swings on timescales of decades or less in the …
Phytoplankton Calcification in a High-CO2 World
MD Iglesias-Rodriguez, PR Halloran, REM Rickaby… - science, 2008 - science.org
Ocean acidification in response to rising atmospheric CO2 partial pressures is widely
expected to reduce calcification by marine organisms. From the mid-Mesozoic …
expected to reduce calcification by marine organisms. From the mid-Mesozoic …
Atlantic meridional overturning circulation during the Last Glacial Maximum
J Lynch-Stieglitz, JF Adkins, WB Curry, T Dokken… - science, 2007 - science.org
The circulation of the deep Atlantic Ocean during the height of the last ice age appears to
have been quite different from today. We review observations implying that Atlantic …
have been quite different from today. We review observations implying that Atlantic …
Paleoclimate and paleoceanography over the past 20,000 yr in the Mediterranean Sea Basins as indicated by sediment elemental proxies
F Martinez-Ruiz, M Kastner, D Gallego-Torres… - Quaternary Science …, 2015 - Elsevier
Marine sediments record paleoenvironmental changes over time through variations in major
and trace element concentrations. The main objective of this paper is to review such …
and trace element concentrations. The main objective of this paper is to review such …
Relation of sortable silt grain-size to deep-sea current speeds: Calibration of the 'Mud Current Meter'
IN McCave, DJR Thornalley, IR Hall - Deep Sea Research Part I …, 2017 - Elsevier
Fine grain-size parameters have been used for inference of palaeoflow speeds of near-
bottom currents in the deep-sea. The basic idea stems from observations of varying …
bottom currents in the deep-sea. The basic idea stems from observations of varying …
Ice loss from the East Antarctic Ice Sheet during late Pleistocene interglacials
DJ Wilson, RA Bertram, EF Needham, T van de Flierdt… - Nature, 2018 - nature.com
Understanding ice sheet behaviour in the geological past is essential for evaluating the role
of the cryosphere in the climate system and for projecting rates and magnitudes of sea level …
of the cryosphere in the climate system and for projecting rates and magnitudes of sea level …
The role of deep ocean circulation in setting glacial climates
JF Adkins - Paleoceanography, 2013 - Wiley Online Library
The glacial cycles of the Pleistocene involve changes in the circulation of the deep ocean in
important ways. This review seeks to establish what were the robust patterns of deep‐sea …
important ways. This review seeks to establish what were the robust patterns of deep‐sea …
Widespread dispersal and aging of organic carbon in shallow marginal seas
The occurrence of pre-aged organic carbon (OC) in continental margin surface sediments is
a commonly observed phenomenon, yet the nature, sources, and causes of this aged OC …
a commonly observed phenomenon, yet the nature, sources, and causes of this aged OC …
Orbital forcing of the East Antarctic ice sheet during the Pliocene and Early Pleistocene
MO Patterson, R McKay, T Naish, C Escutia… - Nature …, 2014 - nature.com
Abstract The Pliocene and Early Pleistocene, between 5.3 and 0.8 million years ago, span a
transition from a global climate state that was 2–3° C warmer than present with limited ice …
transition from a global climate state that was 2–3° C warmer than present with limited ice …