Results 21 to 30 of about 1,279 (147)
Surface Ocean Cooling in the Eocene North Atlantic Coincides With Declining Atmospheric CO2
The Eocene (56–34 million years ago) is characterized by declining sea surface temperatures (SSTs) in the low latitudes (∼4°C) and high southern latitudes (∼8–11°C), in accord with decreasing CO2 estimates.
Gordon N. Inglis +8 more
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Integrated multiproxy geochemical studies are essential to reconstruct the paleoenvironment through different time scales. Pristine terrestrial archives such as speleothems provide an excellent opportunity to study these changes by measuring the stable ...
M. S. Kalpana +5 more
doaj +1 more source
Surface Ocean Hydrographic Changes in the Western Pacific Marginal Seas Since the Early Holocene
Climatic changes in the western Pacific marginal seas are influenced by global forcing and regional processes, including monsoons, and ocean circulation.
Hui-Juan Pan +12 more
doaj +1 more source
Development of a novel sea surface temperature proxy based on bacterial 3-hydroxy fatty acids
Gram-negative bacterial 3-hydroxy fatty acids (3-OH-FAs) have received recent attention for their potential as palaeoclimate proxies. A novel temperature proxy, the ratio of anteiso to normal C13 3-OH-FA (RAN13), has been proposed for sea surface ...
Zhengkun Dong +7 more
doaj +1 more source
TEX86 [TetraEther indeX of glycerol dialkyl glycerol tetraethers (GDGTs) with 86 carbon atoms] has been widely applied to reconstruct (paleo-) sea surface temperature.
Jin-Xiang Wang +6 more
doaj +1 more source
Planktonic archaea include predominantly Marine Group I Thaumarchaeota (MG I) and Marine Group II Euryarchaeota (MG II), which play important roles in the oceanic carbon cycle. MG I produce specific lipids called isoprenoid glycerol dibiphytanyl glycerol
Cenling Ma +5 more
doaj +1 more source
Over the last decade, glycerol dialkyl glycerol tetraethers (GDGTs) have become one of the most investigated lipid classes in marine and terrestrial organic geochemical research. GDGTs are microbial membrane core lipids biosynthesized as multiple homolog
Jayne E. Rattray, Rienk H. Smittenberg
doaj +1 more source
Vegetation response to exceptional global warmth during Oceanic Anoxic Event 2
The Cretaceous Oceanic Anoxic Event 2 represents one of the warmest episodes in the last 250 million years. Here, the authors present spore-pollen data and temperature estimates (TEX86) across an expanded stratigraphic section illustrating the dynamic ...
Ulrich Heimhofer +8 more
doaj +1 more source
Ocean warming can modify the phytoplankton biomass on decadal scales. Significant increases in sea surface temperature (SST) and rainfall in the northwest of Australia over recent decades are attributed to climate change.
Zineng Yuan +6 more
doaj +1 more source
TEX86 and BIT in Lake Challa sediments
TEX86 and BIT in Lake Challa ...
Schouten, Stefan +7 more
core +1 more source

