Saturday 21 July 2018
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4 months ago

A saltier North Atlantic kick-started circulation at the end of the greenhouse world

A drastic change in ocean circulation patterns over 34 million years ago occurred because surface waters in the far North Atlantic became salty enough to sink. This start-up of Northern deep-water formation purged stagnant waters sourced from the Arctic re

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هذه الصفحة هي مجرد قاریء تلقائي للأخبار باستخدام خدمة الـ RSS و بأن نشر هذه الأخبار هنا لاتعني تأییدها علی الإطلاق.

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