Spring Changes in Arctic Microalgae Communities
Research reveals microalgae diversity shifts in the Arctic during springtime melt.
― 6 min read
Table of Contents
In the Arctic Ocean, small organisms called Microalgae play a crucial role in producing food for other marine life. They are the main source of energy in this region, both in the open water and under the ice. The production of microalgae that lives in the ice is usually lower than that of those in open water, making up about 2-10% of the total food produced in the Arctic. These ice-dwelling microalgae often bloom during spring, prior to the microalgae that live in open water, when sunlight becomes stronger and snow cover thins out. When the ice begins to melt and puddles form, these under-ice algae provide a rich food supply for tiny creatures that live both in the ice and just beneath it.
This transition from ice to water is key, as the conditions change and the flow of fresh water from melting snow and ice can limit nutrients. This can lead to a lack of nutrients in the ice itself. Less snow cover can also affect the algae, leading to less sunlight reaching them and causing them to flush out from the ice. Meanwhile, as snow melts, sunlight increases in the water, setting the stage for a bloom of microalgae under the ice.
The Arctic marine environment is made up of various areas like open water, ice, and melt ponds, each with different nutrients and light conditions. This variety creates complex communities of ice algae and other microalgae. Ice-associated communities often consist of certain types of Diatoms, a kind of algae, while plankton communities typically include other species. Some smaller-sized organisms, known as pico-sized algae, also play a vital role in the ecosystem.
Impact of Climate Change
However, climate change is dramatically changing the Arctic environment. One of the most visible effects is the rapid retreat of sea ice in both area and thickness. As the summer months see less ice, older layers are being replaced by newer, thinner ice. Thinner ice can allow more sunlight to penetrate, which is better for some types of ice algae. But older, thicker ice tends to support a more diverse community of microbes.
The warming waters flowing into the Arctic from the Atlantic are not only leading to loss of ice but also allowing species that normally live in warmer regions to move northward. This shift is changing the makeup of the plankton community, where diatoms are often replaced by smaller organisms.
As the Arctic continues to change, it is expected to experience significant shifts in its ecosystems, with many species potentially moving into the area and others disappearing. The changes in habitats and temperatures can lead to significant reorganization in food webs and impact overall ecosystem health. Microbial eukaryotes, the tiny organisms that include our microalgae, can show us how these changes are happening due to their varied responses to the new conditions.
Study Objective
This study aimed to look at how microalgae communities in the Arctic change during springtime. Samples were taken from ice and water at a specific location in Baffin Bay over a period of nearly three months. The researchers wanted to understand which microalgae were present and how their populations changed during the ice melt. They used advanced techniques to analyze the DNA of these organisms to better understand their community structure and distribution.
Sample Collection
The research took place on the ice in Baffin Bay. Samples were taken from different parts of the ice and water every couple of days during the study. Ice samples were collected from the bottom areas of the ice, and water samples were taken from various depths beneath the ice. These samples were then filtered to separate different sizes of microalgae, including larger ones and smaller pico-sized varieties.
Environmental Conditions
During the research, a number of environmental factors were measured. The amount of sunlight reaching the ice and water was tracked, along with the concentration of Chlorophyll, which indicates the amount of microalgae present. The thickness of ice and snow was also recorded. These factors are important as they influence the growth of microalgae and the timing of their blooms.
DNA Analysis
The collected samples underwent DNA analysis to identify the different types of microalgae present. A specific part of their DNA was amplified and sequenced. This method allowed researchers to determine the variety of algae present, along with their abundance in the samples.
Community Diversity and Structure
The results showed a rich diversity of microalgae in both the ice and water samples. Different sizes of algae were present, with some species dominating at certain stages of the bloom. As conditions changed during the different stages of snow and ice melt, the composition of these communities also shifted.
Pico-sized Community
Among the smallest algae, cryptophytes were found to be dominant during the early stages when the ice was still thick with snow. As conditions became more favorable for growth, other species like Micromonas became more abundant later on during the study.
Nano-sized Community
The nano-sized algae, primarily made up of diatoms, showed a varied composition. In the ice, different types of diatoms were prevalent, with changes in community structure as the bloom progressed.
Micro-sized Community
Larger microalgae in the ice were mostly dominated by diatoms. This community was also affected by the melting ice and changing light conditions.
Biogeographical Distribution
The research also looked at how these microalgae are distributed geographically. A significant portion of the algae identified was classified as polar, indicating that they thrive in the Arctic environment. Some species were found to be more adaptable, occurring in both polar and warmer regions.
Indicators of Ecosystem Change
The study found specific algae that could serve as indicators of changing conditions in the Arctic. Many of the identified species have clear associations with either ice or water, which can help scientists monitor ecological shifts.
Succession Patterns
The research revealed clear patterns of succession among the microalgae communities. As the spring progressed and light increased, different species dominated at different times, providing insight into how microalgae respond to environmental changes and bloom conditions.
Conclusions
This research improves our understanding of the microalgae community in the Arctic, especially during critical seasonal changes. As climate change continues to impact this fragile ecosystem, knowing how these organisms react will help in monitoring and predicting future shifts in Arctic marine environments. The findings highlight the need for ongoing research to better characterize these communities and their roles within the ecosystem, especially given the significant percentage of unidentified microorganisms.
The significant diversity and presence of both new and known taxa indicate that the Arctic marine environment is complex and still holds many mysteries. As we continue to face changing conditions in the Arctic, understanding these organisms will be crucial for conservation and management efforts in the region.
Title: Temporal dynamics and biogeography of sympagic and planktonic autotrophic microbial eukaryotes during the under-ice Arctic bloom
Abstract: Photosynthetic microbial eukaryotes play a pivotal role as primary producers in the Arctic Ocean, where seasonal blooms within and below the ice are crucial phenomena, contributing significantly to global primary production and biogeochemical cycling. In this study, we investigated the taxonomic composition of sympagic algae and phytoplankton communities during the Arctic under-ice spring bloom using metabarcoding of the 18S rRNA gene. Samples were obtained from three size fractions over a period of nearly three months at an ice camp deployed on landfast ice off the coast of Baffin Island as part of the Green Edge project. We classified the major sympagic and phytoplankton taxa found in this study into biogeographical categories using publicly available metabarcoding data from more than 2 800 oceanic and coastal marine samples. This study demonstrated the temporal succession of taxonomic groups during the development of the under-ice bloom, illustrated by an overall transition from polar to polar-temperate taxa, in particular in the smallest size fraction. Overlooked classes such as Pelagophyceae (undescribed Pelagomonadales clade A1 and the genus Ankylochrysis), Bolidophyceae (Parmales environmental clade 2), and Cryptophyceae (Baffinella frigidus) might play a greater role than anticipated within the pico-sized communities in and under the ice pack during the pre-bloom period. Finally, we emphasize the importance of microdiversity, taking the example of B. frigidus for which a new strain isolated during Green Edge represents an ice ecotype while the type strain is clearly linked to marine waters.
Authors: Clarence Wei Hung Sim, C. G. Ribeiro, F. Le Gall, I. Probert, P. Gourvil, C. Lovejoy, D. Vaulot, A. Lopes dos Santos
Last Update: 2024-04-29 00:00:00
Language: English
Source URL: https://www.biorxiv.org/content/10.1101/2024.04.26.591324
Source PDF: https://www.biorxiv.org/content/10.1101/2024.04.26.591324.full.pdf
Licence: https://creativecommons.org/licenses/by/4.0/
Changes: This summary was created with assistance from AI and may have inaccuracies. For accurate information, please refer to the original source documents linked here.
Thank you to biorxiv for use of its open access interoperability.