Southern Ocean bioproductivity during the last glacial cycle – new detection method and decadal-scale insight from the Scotia Sea

2013 ◽  
Vol 381 (1) ◽  
pp. 245-261 ◽  
Author(s):  
D. Sprenk ◽  
M. E. Weber ◽  
G. Kuhn ◽  
P. Rosén ◽  
M. Frank ◽  
...  
Keyword(s):  
Southern Ocean ◽  
Detection Method ◽  
Glacial Cycle ◽  
Scotia Sea ◽  
Last Glacial ◽  
Decadal Scale ◽  
The Last Glacial

The changing roles of iron and vertical mixing in regulating nitrogen and silicon cycling in the Southern Ocean over the last glacial cycle

2014 ◽  
Vol 29 (12) ◽  
pp. 1179-1195 ◽  
Author(s):  
Rebecca S. Robinson ◽  
Mark A. Brzezinski ◽  
Charlotte P. Beucher ◽  
Matthew G. S. Horn ◽  
Patrick Bedsole
Keyword(s):  
Southern Ocean ◽  
Vertical Mixing ◽  
Glacial Cycle ◽  
Last Glacial ◽  
Changing Roles ◽  
The Last Glacial ◽  
Silicon Cycling

Effects of glaciation on karst hydrology and sedimentology during the Last Glacial Cycle: The case of Granito cave, Central Pyrenees (Spain)

CATENA ◽  
2021 ◽  
Vol 206 ◽  
pp. 105252
Author(s):  
Miguel Bartolomé ◽  
Carlos Sancho ◽  
Gerardo Benito ◽  
Alicia Medialdea ◽  
Mikel Calle ◽  
...  
Keyword(s):  
Karst Hydrology ◽  
Glacial Cycle ◽  
Last Glacial ◽  
Central Pyrenees ◽  
The Last Glacial

scholarly journals Drivers of river reactivation in North Africa during the last glacial cycle

2021 ◽  
Vol 14 (2) ◽  
pp. 97-103
Author(s):  
Cécile L. Blanchet ◽  
Anne H. Osborne ◽  
Rik Tjallingii ◽  
Werner Ehrmann ◽  
Tobias Friedrich ◽  
...  
Keyword(s):  
North Africa ◽  
Glacial Cycle ◽  
Last Glacial ◽  
The Last Glacial

scholarly journals Carbon burial in deep-sea sediment and implications for oceanic inventories of carbon and alkalinity over the last glacial cycle

2018 ◽  
Vol 14 (11) ◽  
pp. 1819-1850 ◽  
Author(s):  
Olivier Cartapanis ◽  
Eric D. Galbraith ◽  
Daniele Bianchi ◽  
Samuel L. Jaccard
Keyword(s):  
Marine Sediments ◽  
Active Carbon ◽  
Deep Sea ◽  
Dissolved Inorganic Carbon ◽  
Glacial Cycle ◽  
Last Glacial ◽  
Carbon Burial ◽  
Order Constraint ◽  
The Last Glacial ◽  
Carbon Inventory

Abstract. Although it has long been assumed that the glacial–interglacial cycles of atmospheric CO2 occurred due to increased storage of CO2 in the ocean, with no change in the size of the “active” carbon inventory, there are signs that the geological CO2 supply rate to the active pool varied significantly. The resulting changes of the carbon inventory cannot be assessed without constraining the rate of carbon removal from the system, which largely occurs in marine sediments. The oceanic supply of alkalinity is also removed by the burial of calcium carbonate in marine sediments, which plays a major role in air–sea partitioning of the active carbon inventory. Here, we present the first global reconstruction of carbon and alkalinity burial in deep-sea sediments over the last glacial cycle. Although subject to large uncertainties, the reconstruction provides a first-order constraint on the effects of changes in deep-sea burial fluxes on global carbon and alkalinity inventories over the last glacial cycle. The results suggest that reduced burial of carbonate in the Atlantic Ocean was not entirely compensated by the increased burial in the Pacific basin during the last glacial period, which would have caused a gradual buildup of alkalinity in the ocean. We also consider the magnitude of possible changes in the larger but poorly constrained rates of burial on continental shelves, and show that these could have been significantly larger than the deep-sea burial changes. The burial-driven inventory variations are sufficiently large to have significantly altered the δ13C of the ocean–atmosphere carbon and changed the average dissolved inorganic carbon (DIC) and alkalinity concentrations of the ocean by more than 100 µM, confirming that carbon burial fluxes were a dynamic, interactive component of the glacial cycles that significantly modified the size of the active carbon pool. Our results also suggest that geological sources and sinks were significantly unbalanced during the late Holocene, leading to a slow net removal flux on the order of 0.1 PgC yr−1 prior to the rapid input of carbon during the industrial period.

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