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“Our reconstruction shows that the first half of the Holocene was colder than in industrial times due to the cooling effects of remnant ice sheets from the previous glacial period contrary to previous reconstructions of global temperatures,” says lead author Samantha Bova, a postdoctoral researcher associate in the lab of coauthor Yair Rosenthal, professor in the department of marine and coastal sciences and department of earth and planetary sciences at Rutgers University-New Brunswick. Scientists used marine calcareous (calcium carbonate-containing) fossils from foraminifers single-celled organisms that live at the ocean surface to reconstruct the temperature histories of the two most recent warm intervals on Earth. They are the Last Interglacial period from 128,000 to 115,000 years ago and the Holocene.

Yair rosenthalSamantha bovaRutgers universityRutgers university newWorld economic forumKlaus schwabGlobalization4 0Globalization fourWhat does globalization meanயேர் ரோசென்டல்சமந்தா போவாரட்ஜர்ஸ் பல்கலைக்கழகம்ரட்ஜர்ஸ் பல்கலைக்கழகம் புதியதுஉலகம் பொருளாதார மன்றம்கிளாஸ் ஸ்க்வாப்உலகமயமாக்கல் நான்கு