ANTARCTIC ICE SHELF

Last Updated on 24th March, 2025
7 minutes, 5 seconds

Description

Disclaimer: Copyright infringement not intended.

Context

The discovery of thriving marine ecosystems beneath Antarctic ice shelf following breakaway of A-84 iceberg challenges existing scientific assumptions & highlights importance of deep-sea exploration in understanding climate change & biodiversity.

Key Highlights

A massive 510 sq. km iceberg A-84 broke away from George VI Ice Shelf on January 13, 2025.

The exposed seafloor previously covered by 150-meter-thick ice for centuries became accessible for exploration.

Scientists used  remotely operated vehicle (ROV) SuBastian to explore  newly exposed seafloor.

The mission was part of Challenger 150 UNESCO-endorsed global initiative for deep-sea research.

The submersible explored depths of up to 1,300 meters over eight days capturing high-resolution images & collecting biological samples.

Scientists observed diverse deep-sea ecosystems contrary to expectations.

Notable species discovered:

Giant sea spiders

Deep-sea octopi

Large corals & sponges

Icefish

A giant phantom jellyfish which can grow up to a meter wide

A vase-shaped sponge potentially hundreds of years old

Several potentially new species were also documented.

Deep-sea ecosystems typically depend on photosynthetic nutrient sources from surface waters.

However these organisms have survived under thick ice for centuries indicating alternative nutrient sources.

Possible factors sustaining these ecosystems:

Ocean currents transporting nutrients

Glacial meltwater providing essential minerals

Undiscovered deep-sea microbial food chains

Scientific Significance:

The findings challenge previous assumptions about life beneath Antarctic ice shelves.

Offers new insights into climate change impacts on marine biodiversity.

Provides evidence of long-term ecosystem resilience despite extreme conditions.

Historical Context:

Prior to this first evidence of bottom dwelling life under Antarctic ice shelves was reported in 2021 by British Antarctic Survey (BAS) researchers.

This new discovery significantly expands knowledge about  hidden ecosystems beneath ice-covered oceans.

Ice Shelves

Category

Description

Examples & Locations

Significance

Definition

Large floating platforms of ice attached to land masses.

Found along  coasts of Antarctica, Greenland & Canada.

Act as barriers, slowing glacier movement into oceans.

Formation

Formed when glaciers or ice sheets flow into  ocean & extend outward.

Primarily in polar regions where temperatures allow ice accumulation.

Help regulate global sea levels.

Types

Based on stability & size:
1. Stable Ice Shelves (thick, long-lasting)
2. Thinning Ice Shelves (affected by climate change)
3. Collapsing Ice Shelves (disintegrating due to warming)

1. Ross Ice Shelf (Largest, Antarctica)
2. Larsen Ice Shelf (Antarctica, multiple collapses since 1995)
3. George VI Ice Shelf (Source of A-84 iceberg, Antarctica)

Provide habitat for unique ecosystems beneath ice.

Major Ice Shelves

1. Antarctica: Ross, Filchner-Ronne, Amery, Larsen, George VI
2. Greenland: Petermann, Nioghalvfjerdsbræ
3. Canada: Ward Hunt Ice Shelf (Arctic)

Mostly found in polar regions where land-based glaciers meet  sea.

Their melting contributes to rising sea levels.

Threats & Climate Change Impact

Rising temperatures cause ice shelves to thin, break, or collapse, accelerating glacier flow into oceans.

Larsen B (collapsed in 2002), Larsen C (broke in 2017), A-68 (drifted into  ocean, 2017)

Ice shelf disintegration can increase sea level rise & alter ocean currents.

Major Deep-Sea Research Missions

Mission Name

Year

Conducted By

Objective & Focus

Key Discoveries & Achievements

Challenger Expedition

1872-1876

British Royal Navy

First systematic deep-sea exploration

Identified 4,700+ new marine species, mapped ocean depths.

Glomar Challenger (Deep Sea Drilling Project)

1968-1983

US & International partners

Studied plate tectonics & ocean sediment layers

Confirmed seafloor spreading & provided proof of continental drift.

ALVIN (Submarine Program)

1964-present

Woods Hole Oceanographic Institution (USA)

Deep-sea hydrothermal vents & oceanic trenches exploration

Discovered hydrothermal vents, deep-sea organisms, explored Titanic wreck.

Hadal Exploration Program

2000s-present

Japan, USA

Exploring  deepest parts of  ocean

Explored Mariana Trench, found new species adapted to extreme pressure.

Challenger 150

2021-present

UNESCO-endorsed global project

Mapping & researching deep-sea biodiversity

New species discovered in Antarctic ice shelf region (2025), better understanding of deep-sea ecosystems.

Five Deeps Expedition

2018-2019

Victor Vescovo

First manned mission to reach  deepest point in each ocean

Reached Mariana Trench (10,928 m), discovered plastic pollution in deep-sea.

Nereus & ROV SuBastian Missions

2010s-present

Schmidt Ocean Institute

Robotic deep-sea exploration

Discovered giant jellyfish, new corals & deep-sea sponges in Antarctica (2025).

International Ocean Discovery Program (IODP)

2013-present

International Collaboration

Studying Earth's past climate, plate tectonics

Drilling deep-sea sediment cores for climate & geological data.

For more information, please visit IAS GYAN

Sources:

INDIAN EXPRESS

PRACTICE QUESTION

Q. Consider following statements regarding Ice Shelves:

  1. Ice shelves are floating extensions of glaciers that are found only in Antarctica.
  2. The collapse of an ice shelf directly contributes to rising sea levels.
  3. Larsen Ice Shelf, Ross Ice Shelf & George VI Ice Shelf are some of major ice shelves in world.

Which of  statements given above is/are correct?

(a) 1 & 2 only
(b) 2 & 3 only
(c) 3 only
(d) 1, 2 & 3

Answer: (c)

Explanation:

Statement 1 is incorrect: Ice shelves are not exclusive to Antarctica. They are also found in Greenland as well as Canada. Some examples include Petermann Ice Shelf (Greenland) & Ward Hunt Ice Shelf (Canada).

Statement 2 is incorrect: collapse of an ice shelf itself does not directly raise sea levels as ice is already floating. However it removes barrier that holds back glaciers accelerating their flow into ocean which eventually raises sea levels.

Statement 3 is correct: Larsen Ice Shelf, Ross Ice Shelf & George VI Ice Shelf are important ice shelves located in Antarctica.

Related Articles

VAITARNA DAM 25 Mar, 2025
HEMAVATI RIVER 25 Mar, 2025
HOLOCENE EPOCH 24 Mar, 2025
GAMBHIR RIVER 24 Mar, 2025
VERNAL EQUINOX 22 Mar, 2025
ANA SAGAR 21 Mar, 2025
MOUNT FUJI 20 Mar, 2025
BETWA RIVER 20 Mar, 2025
KYUSHU ISLAND 20 Mar, 2025

Free access to e-paper and WhatsApp updates

Let's Get In Touch!