Nutrient dynamics and related future challenges in Kongsfjorden

Resumen de la conferencia inaugural Abstract The Arctic has waned four times faster than the rest of the world due to Global Warming. In the model Arctic ecosystem of Kongsfjorden (Svalbard archipelago, 79 ºN) warming has occurred more intensely in winter. A warmer winter has led ice-free fjord surf...

Full description

Bibliographic Details
Main Author: López-Gordillo, Francisco Javier
Format: Conference Object
Language:English
Published: 2022
Subjects:
Online Access:https://hdl.handle.net/10630/25412
id ftunivmalaga:oai:riuma.uma.es:10630/25412
record_format openpolar
spelling ftunivmalaga:oai:riuma.uma.es:10630/25412 2023-05-15T14:23:06+02:00 Nutrient dynamics and related future challenges in Kongsfjorden López-Gordillo, Francisco Javier 2022 https://hdl.handle.net/10630/25412 eng eng Nutrient cycle in Arctic regions: linking the Atmosphere, Terrestrial, Marine and Glaciological flagship programmes in Ny-Ålesund Orvieto, Italia 20-23 Septiembre 2022 https://hdl.handle.net/10630/25412 info:eu-repo/semantics/openAccess http://creativecommons.org/licenses/by-nc-nd/4.0/ Attribution-NonCommercial-NoDerivatives 4.0 Internacional CC-BY-NC-ND Clima - Cambios Algas Ártico Polar biology Seaweeds Phytoplankton Marine Arctic info:eu-repo/semantics/conferenceObject 2022 ftunivmalaga 2023-02-15T00:52:30Z Resumen de la conferencia inaugural Abstract The Arctic has waned four times faster than the rest of the world due to Global Warming. In the model Arctic ecosystem of Kongsfjorden (Svalbard archipelago, 79 ºN) warming has occurred more intensely in winter. A warmer winter has led ice-free fjord surface all year round. Under this conditions hydrodynamics are changed and, along with it, the biological and other physicochemical dynamics. Seaweeds start its production when light is available in the water column. Typically, this used to occur in May, after the ice break-up. Late spring-early summer used to be the season when both phytoplankton and the seaweeds forest would uptake the available nutrient and produce biomass. This production season ends during late summer due to nutrient limitation. The atmospheric workgroup has identified the spring as the time of the year with pronounce nutrient-N deposition in the fjord, and the glaciologist has measured that virtually all nutrient deposited over glaciers end up in the fjord water system. Regarding biological primary production, timing of both light and N availability is key. An ice-free N-rich spring may anticipate the season of macroalgal forests productivity and removal of nutrients. We support evidence that macroalgal possess newly developed photosynthetic tissue at the end of the winter, ready to photosynthesise as soon as light is available in February-March. If N removal is intensified by productivity season anticipation, N-limitation could take place before the development of phytoplankton bloom, normally occurring in late Spring. Since most of the animal production relies on phytoplankton productivity, season anticipation of N-limitation has the potential to drastically change the ecosystem. Universidad de Málaga. Campus de Excelencia Internacional Andalucía Tech Conference Object Arctic Arctic Global warming Kongsfjord* Kongsfjorden Phytoplankton Svalbard RIUMA - Repositorio Institucional de la Universidad de Málaga Arctic Svalbard Svalbard Archipelago
institution Open Polar
collection RIUMA - Repositorio Institucional de la Universidad de Málaga
op_collection_id ftunivmalaga
language English
topic Clima - Cambios
Algas
Ártico
Polar biology
Seaweeds
Phytoplankton
Marine
Arctic
spellingShingle Clima - Cambios
Algas
Ártico
Polar biology
Seaweeds
Phytoplankton
Marine
Arctic
López-Gordillo, Francisco Javier
Nutrient dynamics and related future challenges in Kongsfjorden
topic_facet Clima - Cambios
Algas
Ártico
Polar biology
Seaweeds
Phytoplankton
Marine
Arctic
description Resumen de la conferencia inaugural Abstract The Arctic has waned four times faster than the rest of the world due to Global Warming. In the model Arctic ecosystem of Kongsfjorden (Svalbard archipelago, 79 ºN) warming has occurred more intensely in winter. A warmer winter has led ice-free fjord surface all year round. Under this conditions hydrodynamics are changed and, along with it, the biological and other physicochemical dynamics. Seaweeds start its production when light is available in the water column. Typically, this used to occur in May, after the ice break-up. Late spring-early summer used to be the season when both phytoplankton and the seaweeds forest would uptake the available nutrient and produce biomass. This production season ends during late summer due to nutrient limitation. The atmospheric workgroup has identified the spring as the time of the year with pronounce nutrient-N deposition in the fjord, and the glaciologist has measured that virtually all nutrient deposited over glaciers end up in the fjord water system. Regarding biological primary production, timing of both light and N availability is key. An ice-free N-rich spring may anticipate the season of macroalgal forests productivity and removal of nutrients. We support evidence that macroalgal possess newly developed photosynthetic tissue at the end of the winter, ready to photosynthesise as soon as light is available in February-March. If N removal is intensified by productivity season anticipation, N-limitation could take place before the development of phytoplankton bloom, normally occurring in late Spring. Since most of the animal production relies on phytoplankton productivity, season anticipation of N-limitation has the potential to drastically change the ecosystem. Universidad de Málaga. Campus de Excelencia Internacional Andalucía Tech
format Conference Object
author López-Gordillo, Francisco Javier
author_facet López-Gordillo, Francisco Javier
author_sort López-Gordillo, Francisco Javier
title Nutrient dynamics and related future challenges in Kongsfjorden
title_short Nutrient dynamics and related future challenges in Kongsfjorden
title_full Nutrient dynamics and related future challenges in Kongsfjorden
title_fullStr Nutrient dynamics and related future challenges in Kongsfjorden
title_full_unstemmed Nutrient dynamics and related future challenges in Kongsfjorden
title_sort nutrient dynamics and related future challenges in kongsfjorden
publishDate 2022
url https://hdl.handle.net/10630/25412
geographic Arctic
Svalbard
Svalbard Archipelago
geographic_facet Arctic
Svalbard
Svalbard Archipelago
genre Arctic
Arctic
Global warming
Kongsfjord*
Kongsfjorden
Phytoplankton
Svalbard
genre_facet Arctic
Arctic
Global warming
Kongsfjord*
Kongsfjorden
Phytoplankton
Svalbard
op_relation Nutrient cycle in Arctic regions: linking the Atmosphere, Terrestrial, Marine and Glaciological flagship programmes in Ny-Ålesund
Orvieto, Italia
20-23 Septiembre 2022
https://hdl.handle.net/10630/25412
op_rights info:eu-repo/semantics/openAccess
http://creativecommons.org/licenses/by-nc-nd/4.0/
Attribution-NonCommercial-NoDerivatives 4.0 Internacional
op_rightsnorm CC-BY-NC-ND
_version_ 1766295587763781632