scholarly journals A stalactite record of four relative sea-level highstands during the Middle Pleistocene Transition

2017 ◽  
Vol 173 ◽  
pp. 92-100 ◽  
Author(s):  
Paolo Stocchi ◽  
Fabrizio Antonioli ◽  
Paolo Montagna ◽  
Fabrizio Pepe ◽  
Valeria Lo Presti ◽  
...  
2017 ◽  
Vol 173 ◽  
pp. 20-39 ◽  
Author(s):  
N.L.M. Barlow ◽  
A.J. Long ◽  
W.R. Gehrels ◽  
M.H. Saher ◽  
R.G. Scaife ◽  
...  

2021 ◽  
Author(s):  
Peter U. Clark ◽  
Jeremy Shakun ◽  
Yair Rosenthal ◽  
Peter Köhler ◽  
Dan Schrag ◽  
...  

<p>The Middle Pleistocene Transition (MPT) has been characterized as the transition in temperature and sea level from low-amplitude, 41-kyr variability to high-amplitude, quasi-100-kyr variability in the absence of any orbital forcing between 1.2 and 0.7 Ma. The regolith hypothesis is one of a class of hypotheses developed to explain the MPT in sea level, which has been largely inferred from d<sup>18</sup>O<sub>benthic</sub> records. Here we use a global array of 130 sea-surface temperature (SST) records based on Mg/Ca, alkenone, and faunal proxies to reconstruct global and regional SST change over the last 4.5 Myr. Average global temperature cooled by ~6.5<sup>o</sup>C since ~3.5 Ma, with the MPT represented by a significant increase in the rate of cooling between ~1.4 and 0.8 Ma, and a change from dominant 41-kyr to dominant quasi-100-kyr frequencies at ~1.2 Ma that are well correlated with CO<sub>2</sub> over the last 800 ka (r<sup>2</sup>=0.6). Temperature terminations after 1.2 Ma correspond to skipped obliquity beats and, for the last 800 ka, large increases in CO<sub>2</sub>. We use our global SST reconstruction to remove the temperature signal from the Ahn17 d<sup>18</sup>O<sub>benthic</sub> stack to derive d<sup>18</sup>O<sub>seawater</sub>. Accounting for the influence of changing temperature on the isotopic composition of ice sheets, we use the d<sup>18</sup>O<sub>seawater</sub> record to reconstruct global sea level for the last 4.5 Myr. These results suggest sea-level minima equivalent to or lower than the LGM sea-level low stand (130 m) throughout the Pleistocene. Since inception of Northern Hemisphere glaciation ~3 Ma, sea level varied linearly with obliquity until ~1.2 Ma, when sea-level began to vary nonlinearly with obliquity, with the largest terminations occurring at the same time as temperature terminations that correspond to increasing obliquity and CO<sub>2</sub>. These results suggest that the MPT is largely a temperature phenomenon likely associated with CO<sub>2</sub>. The regolith hypothesis other hypotheses developed to explain a transition from low- to high-amplitude sea level variability during the MPT are no longer required, with the MPT change in sea-level response to obliquity likely due to modulation by CO<sub>2</sub>.</p>


2020 ◽  
Vol 644 ◽  
pp. 33-45
Author(s):  
JM Hill ◽  
PS Petraitis ◽  
KL Heck

Salt marshes face chronic anthropogenic impacts such as relative sea level rise and eutrophication, as well as acute disturbances from tropical storms that can affect the productivity of these important communities. However, it is not well understood how marshes already subjected to eutrophication and sea level rise will respond to added effects of episodic storms such as hurricanes. We examined the interactive effects of nutrient addition, sea level rise, and a hurricane on the growth, biomass accumulation, and resilience of the saltmarsh cordgrass Spartina alterniflora in the Gulf of Mexico. In a microtidal marsh, we manipulated nutrient levels and submergence using marsh organs in which cordgrasses were planted at differing intertidal elevations and measured the impacts of Hurricane Isaac, which occurred during the experiment. Prior to the hurricane, grasses at intermediate and high elevations increased in abundance. After the hurricane, all treatments lost approximately 50% of their shoots, demonstrating that added nutrients and elevation did not provide resistance to hurricane disturbance. At the end of the experiment, only the highest elevations had been resilient to the hurricane, with increased above- and belowground growth. Added nutrients provided a modest increase in above- and belowground growth, but only at the highest elevations, suggesting that only elevation will enhance resilience to hurricane disturbance. These results empirically demonstrate that S. alterniflora in microtidal locations already subjected to submergence stress is less able to recover from storm disturbance and suggests we may be underestimating the loss of northern Gulf Coast marshes due to relative sea level rise.


Geology ◽  
1985 ◽  
Vol 13 (9) ◽  
pp. 661 ◽  
Author(s):  
Alan Ruffman ◽  
Ann A. L. Miller ◽  
David B. Scott

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