Related Experiment Video
Updated: Dec 15, 2025

06:02
A Low-Cost Method of Measuring the In Situ Primary Productivity of Periphyton Communities of Lentic Waters
Published on: December 16, 2022
2.3K
Changes in phytoplankton concentration now drive increased Arctic Ocean primary production
K M Lewis1, G L van Dijken1, K R Arrigo2
1Department of Earth System Science, Stanford University, Stanford, CA 94305, USA.
Summary
Arctic phytoplankton primary production has increased 57% due to sea ice loss. Future increases may be driven by nutrient influx and phytoplankton biomass, supporting higher trophic levels and carbon export.
Area of Science:
- Oceanography
- Marine Biology
- Climate Science
Background:
- Arctic sea ice loss historically correlates with increased phytoplankton primary production.
- The long-term impact of continued sea ice decline on Arctic primary production remains debated.
- Understanding these changes is crucial for predicting Arctic ecosystem responses.
Purpose of the Study:
- To quantify changes in Arctic primary production over two decades.
- To identify the drivers of primary production changes in response to sea ice loss.
- To project the future capacity of the Arctic Ocean for supporting higher trophic levels and carbon export.
Main Methods:
- Utilized an ocean color algorithm specifically parameterized for the Arctic Ocean.
- Analyzed satellite data from 1998 to 2018 to assess primary production trends.
- Investigated the relationship between sea ice extent, phytoplankton biomass, and nutrient availability.
Main Results:
- Observed a 57% increase in Arctic primary production between 1998 and 2018.
- Early increases were linked to greater open water due to sea ice loss.
- Later increases were primarily driven by enhanced phytoplankton biomass, sustained by new nutrient influx.
Conclusions:
- Arctic primary production is sensitive to sea ice dynamics and nutrient availability.
- The Arctic Ocean may support increased higher trophic-level production and carbon export in the future.
- Continued monitoring is essential to understand the evolving Arctic marine ecosystem.
More Related Videos
Related Concept Videos
Primary Production
24.9K
The total amount of energy acquired by primary producers in an ecosystem is called gross primary production (GPP). However, of this energy, producers use some for metabolic processes, and some is lost as heat, decreasing the amount of energy available to the next trophic level. The remaining usable amount of energy is called the net primary productivity (NPP). In terrestrial ecosystems, NPP is driven by climate, while light penetration and nutrient availability drive NPP in aquatic ecosystems.
24.9K
Green Algae
554
Green algae, also referred to as chlorophytes, are different from red algae in having the chloroplasts containing chlorophylls a and b, which give them their distinct green hue. However, they lack phycobiliproteins, preventing them from developing the red or blue-green pigmentation seen in red algae. In terms of photosynthetic pigment composition, green algae closely resemble plants and share a close evolutionary relationship with them. Taxonomically Green algae belong to Phylum Chlorophyta in...
554
Global Climate Change
28.3K
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.
28.3K
Oxygenic Photosynthesis
573
Oxygenic photosynthesis is a fundamental process in which light energy is harnessed to drive the oxidation of water, leading to the production of molecular oxygen (O₂), adenosine triphosphate (ATP), and nicotinamide adenine dinucleotide phosphate (NADPH). This process is essential for sustaining aerobic life on Earth and is primarily carried out by cyanobacteria, algae, and plants. The core of oxygenic photosynthesis lies in the thylakoid membranes, where chlorophyll pigments facilitate...
573
Other Algae
281
The group Stramenopiles include some phototrophic microorganisms. Members of this group possess flagella covered in numerous short, hairlike extensions, a feature that inspired the group's name, derived from the Latin words for "straw" and "hair." Some of the main categories of Stramenopiles include diatoms, golden algae, and brown algae.Diatoms are unicellular, photosynthetic eukaryotes, with over 200 known genera. They play a key role in the planktonic communities of both marine and...
281
The Antenna Complex
7.3K
Plants and other photosynthetic organisms comprise pigments capable of absorption of direct sunlight. These pigments are present in the reaction center - the main site of photochemical reactions as well as in the antenna complex. Under average light conditions, the rate at which reaction center pigments absorb light is far below the electron transport chain's capacity. As a result, the reaction center alone cannot provide enough energy to drive photosynthesis. The photosynthetic efficiency can...
7.3K

