A possible sequence of events for the generalized glacial‐interglacial cycle

Abstract

[1] There is not yet widespread agreement as to the underlying cause of the 80-100 ppmv roughly 100-kyr-duration glacial-interglacial cycles in atmospheric pCO 2 . Most of the mechanisms which have been proposed to account for the observed pCO 2 variations appear to in some way violate interpretations of paleo proxy data. The inability of a single mechanism to explain the observed cycles in atmospheric CO 2 (which show amazing similarity over the past 430,000 years) is perplexing, and leads us to consider whether a combination of mechanisms might be consistent with available evidence. Consistent with previous work, we find that physical changes (ocean circulation, temperature, mixing) can only explain part of the observed atmospheric pCO 2 variability; changes in ocean chemistry are invoked to explain the remainder. In order to account for the initial pCO 2 drawdown (from ''interglacial'' to ''intermediate'' levels), we invoke physical changes in the ocean (mixing, temperature). The transition from intermediate atmospheric pCO 2 levels to full glacial conditions involves a small increase in mean ocean nutrient levels and mean ocean alkalinity, accomplished by falling sea level and subsequent erosion of organic-rich shelf sediments. The first part of the transition out of full glacial conditions is achieved through increased temperature and increased mixing in the Southern Ocean. The final part of the atmospheric pCO 2 rise up to full interglacial conditions is accomplished through rising sea level and the subsequent change in mean ocean alkalinity and phosphate, and a rise in the Northern Hemisphere temperature and ocean mixing. The proposed sequence of events is consistent with most existing proxy evidence for paleo-nutrient levels and changes in export production over the last glacial-interglacial cycle. Furthermore, it is consistent with evidence for a whole-ocean shift in d 13C toward significantly more negative values in the late glacial. The proposed scenario is also consistent with ice core-based timing constraints, as summarized by Broecker and Henderson (1998). We show that we are able to explain the full magnitude of the glacial-interglacial cycle in atmospheric pCO 2 without the need to invoke iron-fertilization in the Southern Ocean.

Shelf erosion and submarine river canyons: implications for deep-sea oxygenation and ocean productivity during glaciation

“…Phosphorus speciation in the North Atlantic, particularly the decrease of authigenic and iron bound phases during Heinrich events 4 and 5, points to dysaerobic conditions in the North Atlantic as well (Tamburini et al, 2002). Similarly, mass balance and modeling studies (Boyle, 1988;Broecker, 1982;Francois et al, 1997;Peacock, 2006) have concluded that deep-sea oxygen must have been lower during glacial periods.…”

LOSCAR: Long-term Ocean-atmosphere-Sediment CArbon cycle Reservoir Model v2.0.4

“…One thing to keep in mind is that the equations solved in LOSCAR are typically stiff and involve different time scales, which requires a solver for stiff problems with adaptive stepsize control. The solver implemented in the C version of LOSCAR is a fourth-order Rosenbrock method with automatic stepsize adjustment (Press et al, 1992).…”

“…Sarmiento and Toggweiler, 1984;Siegenthaler and Wenk, 1984;Walker and Kasting, 1992;Toggweiler, 1999;Stephens and Keeling, 2000;Köhler et al, 2005;Peacock et al, 2006). However, less studies have coupled a genuine sediment model to the ocean box model (e.g.…”

Opal burial in the equatorial Atlantic Ocean over the last 30 ka: Implications for glacial‐interglacial changes in the ocean silicon cycle

“…Preindustrial atmospheric CO 2 concentrations averaged 280 ppm, whereas levels ranging from 180 -200 ppm characterized peak glacial periods [Petit et al, 1999]. While it has been established that these changes in the carbon cycle are closely linked to glacial-interglacial cycles, a set of mechanisms to explain this link has yet to be conclusively established [Archer et al, 2000;Sigman and Boyle, 2000;Peacock et al, 2006]. Consequently, the paleoceanographic community continues to develop and test new hypotheses relating variability in the CO 2 content of the atmosphere to climatic change.…”