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Global Climate Change01:50

Global Climate Change

Throughout its ~4.5 billion year history, the Earth has experienced periods of warming and cooling. However, the current drastic increase in global temperatures is well outside of the Earth’s cyclic norms, and evidence for human-caused global climate change is compelling. Paleoclimatology, the study of ancient climate conditions, provides ample evidence for human-caused global climate change by comparing recent conditions with those in the past.
Deep Sea Microbial Ecology01:18

Deep Sea Microbial Ecology

The deep ocean and its underlying sediments represent vast, largely unexplored microbial habitats that extend far beyond the sunlit photic zone. The photic (euphotic) zone typically spans the upper ~100–200 meters of pelagic waters in the open ocean, but its depth varies geographically and seasonally, where sufficient light supports photosynthetic life. Below this lies the deep sea, spanning roughly 1000–6000 meters (bathypelagic to abyssal zones), with deeper hadal trenches extending beyond...
Influence of Earth's Curvature and Atmospheric Refraction on Leveling01:26

Influence of Earth's Curvature and Atmospheric Refraction on Leveling

During leveling, the Earth's curvature and atmospheric refraction introduce deviations in the line of sight from a true horizontal reference. When the line of sight is leveled, it remains perpendicular to the plumb line only at a single point. Beyond this, it deviates due to the Earth’s curvature, represented by the correction C. For a sight distance D, the deviation can be derived using the relationship:This relationship shows that the deviation increases quadratically with distance. Over a...
Tidal Forces01:06

Tidal Forces

The origin of Earth's ocean tides has been a subject of continuous investigation for over 2000 years. However, the work of Newton is considered to be the beginning of the proper understanding of the phenomenon. Ocean tides are the result of gravitational tidal forces. These same tidal forces are present in any astronomical body; they are responsible for the internal heat that creates the volcanic activity on Io, one of Jupiter's moons, and the breakup of stars that get too close to black holes.
The Fossil Record02:56

The Fossil Record

The fossil record documents only a small fraction of all organisms that have ever inhabited Earth. Fossilization is a rare process, and most organisms never become fossils. Moreover, the fossil record only exhibits fossils that have been discovered. Nevertheless, sedimentary rock fossils of long-lived, abundant, hard-bodied organisms dominate the fossil record. These fossils offer valuable information, such as an organism's physical form, behavior, and age. Studying the fossil record helps...
What is Evolutionary History?02:35

What is Evolutionary History?

Scientists record evolutionary history by analyzing fossil, morphological, and genetic data. The fossil record documents the history of life on Earth and provides evidence for evolution. However, both fossil and living organisms offer evidence that outlines Earth’s evolutionary history.Phylogenetic trees illustrate the evolutionary relationships among these organisms. Scientists infer organisms’ common ancestry by evaluating shared morphological and genetic characteristics. Together, the fossil...

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Related Experiment Video

Updated: Jul 12, 2026

Using Generative Art to Convey Past and Future Climate Transitions
06:10

Using Generative Art to Convey Past and Future Climate Transitions

Published on: March 31, 2023

Sea Levels during the Past 35,000 Years.

J D Milliman, K O Emery

    Science (New York, N.Y.)
    |December 6, 1968
    PubMed
    Summary

    This study presents a sea-level curve for the U.S. Atlantic shelf over the past 35,000 years. It reveals a significant sea-level drop followed by a rapid rise during the Holocene transgression.

    Area of Science:

    • Geology
    • Paleoceanography
    • Quaternary Science

    Background:

    • Reconstructing past sea levels is crucial for understanding Earth's climate dynamics.
    • The Atlantic continental shelf of the United States provides a valuable record of sea-level changes.

    Purpose of the Study:

    • To establish a detailed sea-level curve for the U.S. Atlantic continental shelf spanning the last 35,000 years.
    • To compare this regional curve with global sea-level data.

    Main Methods:

    • Utilized over 80 radiocarbon dates from various shallow-water materials.
    • Included dating of mollusks, oolites, coralline algae, beachrock, and salt-marsh peat.
    • Analyzed data to construct a sea-level curve from 35,000 years ago to the present.

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    Investigating the Relationship between Sea Surface Chlorophyll and Major Features of the South China Sea with Satellite Information
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    Published on: June 13, 2020

    Main Results:

    • Sea level was near present levels 30,000–35,000 years ago.
    • Sea level dropped to approximately -130 meters 16,000 years ago due to glacial growth.
    • Holocene transgression began around 14,000 years ago and accelerated until 7,000 years ago.

    Conclusions:

    • The developed sea-level curve for the U.S. Atlantic shelf aligns with global data.
    • The findings suggest the curve approximates the eustatic sea-level curve for the analyzed period.