Sentence examples for below the present level from inspiring English sources

The sea level, they report in the journal Nature, reached its low point of 425 to 440 feet below the present level from about 22,000 to 19,000 years ago.

Indeed, it's thought that over the course of the past 700,000 years, the sea level has undergone a significant drop every 100,000 years or so, falling to between 90 and 130m below the present level and staying that way for several thousand years.

To preserve "food security", China has set a minimum area for the country's farmland 120m hectares, just below the present level.Something old, something newIt is on the non-arable "construction" land that the latest policy offers something new.

Further reduction of sea levels during the Pleistocene (to a maximum depth of 120 m below the present level) exposed additional land area that connected Peninsular Malaysia, Sumatra, Java, and Borneo [ 71].

A possible scenario includes a decline in numbers during the East African megadrought period at ~135 75 KYA, when the lake level dropped by up to 435 m below the present level (which was still not enough to separate the three subbasins into three distinct lakes; McGlue et al., 2008) and the inhabitable lake area was reduced considerably.

This will require that annual wheat yield genetic gains rise from the present level of below 1%% to at least 1.6%% (FAO 2012).

The site appeared under climatic conditions similar to those of today, and the sea level was below the present sea level (Zaisanovskaya archeological culture).

In addition, during the Last Glacial Maximum (LGM), global sea level reached ~125 m below the present sea level (Yokoyama et al. 2000; Clark et al. 2004; Bassett et al. 2005).

Karstification largely began after the Dinarides' final uplift in the Oligocene and the Miocene, when the carbonates were exposed to atmospheric effects; this extended to the level of 120 m below the present sea level, exposed during the Last Glacial Maximum.

Karstification there largely began after the Dinarides' final uplift in the Oligocene and the Miocene, when carbonate deposits were exposed to atmospheric effects; this extended to the level of 120 m below the present sea level, exposed during the Last Glacial Maximum.

The karst topography developed from the Adriatic Carbonate Platform, where karstification largely began after the final raising of the Dinarides in the Oligocene and Miocene epochs, when carbonate rock was exposed to atmospheric effects such as rain; this extended to 120 m below the present sea level, exposed during the Last Glacial Maximum's sea level drop.