{"id":85016,"date":"2026-04-21T15:23:48","date_gmt":"2026-04-21T15:23:48","guid":{"rendered":"https:\/\/youzum.net\/digging-for-clues-about-the-north-poles-past\/"},"modified":"2026-04-21T15:23:48","modified_gmt":"2026-04-21T15:23:48","slug":"digging-for-clues-about-the-north-poles-past","status":"publish","type":"post","link":"https:\/\/youzum.net\/ja\/digging-for-clues-about-the-north-poles-past\/","title":{"rendered":"Digging for clues about the North Pole\u2019s past"},"content":{"rendered":"<p>In the past, even with an icebreaker and during peak melt season, getting to the North Pole wasn\u2019t a sure bet. It took favorable winds to crack the frozen ocean surface, and ships had to fight through ice that had grown many meters thick over several winters. In the summer of 2025, though, Jochen Knies from the Arctic University of Norway, Troms\u00f8, and his team met little resistance on their way to 90 degrees North with the research vessel <em>Kronprins Haakon<\/em>. The geologist \u201cdidn\u2019t hear the usual grinding of ice\u201d against the hull that he remembered from 1996, when he first reached the pole by ship. Instead, thin floes and large stretches of open water made for an easy, quiet passage. To him, it was \u201ca reminder of how quickly the Arctic is changing.\u201d<\/p>\n<p>Since the late 1970s, when satellite observations of the polar seas began, summer ice cover of the Arctic Ocean has declined by more than 40%. In less than half a century, a frozen area the size of the Mediterranean Sea has turned into blue open water with the rapid warming of the high northern latitudes. If this trend continues, there could soon be summers at the North Pole with no sea ice whatsoever. The last time this happened may have been some 120,000 years ago. But no one knows for certain.<\/p>\n<p>That\u2019s why Knies and his colleagues, a team of researchers from Norway and Germany, set out from Svalbard to the central Arctic last August. The aim of their five-week mission was to determine whether this region had been ice-free in recent Earth history\u2014and if so, when. As part of a \u20ac12.5 million project financed by the European Union, they also came to answer some questions about the future of the Arctic and beyond: How does the loss of sea ice affect the marine ecosystem? What are the consequences for ocean circulation and global climate?<\/p>\n<p>In search of clues, the expedition collected sediment cores up to 22 meters in length at different locations across the Arctic seafloor. Marine sediments are valuable climate archives that give scientists a window into bygone eras. Like diligent record keepers, they can log past water temperatures, sea-ice coverage, and the strength of ocean currents. These data are encrypted in the chemical and physical properties of the plankton remains and weathered rock deposited on the seabed.\u00a0<\/p>\n<div class=\"wp-block-image\">\n<figure class=\"wp-block-image size-large\"><img fetchpriority=\"high\" decoding=\"async\" height=\"2000\" width=\"2667\" src=\"https:\/\/wp.technologyreview.com\/wp-content\/uploads\/2026\/04\/North_Pole_Expedition_MIT_Tech_Rev_TimK_004.jpg?w=2667\" alt=\"a view down the side of the ship at near water level\" class=\"wp-image-1135781\" \/><figcaption class=\"wp-element-caption\">The ship\u2019s crew and researchers recover the sediment corer, a 25-meter-long steel pipe that is driven into the seafloor using a top weight of more than three metric tons.<\/figcaption><div class=\"image-credit\">TIM KALVELAGE<\/div>\n<\/figure>\n<\/div>\n<div class=\"wp-block-image\">\n<figure class=\"wp-block-image size-large\"><img decoding=\"async\" height=\"2000\" width=\"2667\" src=\"https:\/\/wp.technologyreview.com\/wp-content\/uploads\/2026\/04\/North_Pole_Expedition_MIT_Tech_Rev_TimK_001.jpg?w=2667\" alt=\"the crew in a line with the long pipe hoisted over their shoulder\" class=\"wp-image-1135776\" \/><figcaption class=\"wp-element-caption\">Together, the scientists pull out long plastic pipes filled with precious deep-sea mud.<\/figcaption><div class=\"image-credit\">TIM KALVELAGE<\/div>\n<\/figure>\n<\/div>\n<div class=\"wp-block-image\">\n<figure class=\"wp-block-image size-large\"><img loading=\"lazy\" decoding=\"async\" height=\"2000\" width=\"2667\" src=\"https:\/\/wp.technologyreview.com\/wp-content\/uploads\/2026\/04\/North_Pole_Expedition_MIT_Tech_Rev_TimK_003.jpg?w=2667\" alt=\"rows of the cut pipes with plastic syringes inserted at intervals \" class=\"wp-image-1135780\" \/><figcaption class=\"wp-element-caption\">The pipes are cut into shorter pieces and split in half before being processed in the ship\u2019s laboratories. Each of these one-meter sections covers several tens of thousands of years of Earth\u2019s history.<\/figcaption><div class=\"image-credit\">TIM KALVELAGE<\/div>\n<\/figure>\n<\/div>\n<p>While sediment cores several meters long had been recovered on earlier expeditions in the central Arctic, there is no scientific consensus on how old the deposits actually are or whether sea ice ever completely disappeared in summer.\u00a0<\/p>\n<p>To decode the Arctic\u2019s climate archive, Knies brought a team of experts from various disciplines onboard the <em>Kronprins Haakon <\/em>to dig deeper and obtain fresh samples they could subject to the latest analytical techniques.\u00a0 \u00a0<\/p>\n<div class=\"wp-block-image\">\n<figure class=\"wp-block-image size-large\"><img loading=\"lazy\" decoding=\"async\" height=\"2000\" width=\"2419\" src=\"https:\/\/wp.technologyreview.com\/wp-content\/uploads\/2026\/04\/North_Pole_Expedition_MIT_Tech_Rev_TimK_005.jpg?w=2419\" alt=\"a tray of square samples\" class=\"wp-image-1135782\" \/><figcaption class=\"wp-element-caption\">Samples await paleomagnetic dating. Like tiny compass needles, iron-rich particles align with Earth\u2019s shifting magnetic field as they settle on the seabed. By measuring their orientation, researchers can estimate the age of the different sediment layers.<\/figcaption><div class=\"image-credit\">TIM KALVELAGE<\/div>\n<\/figure>\n<\/div>\n<div class=\"wp-block-image\">\n<figure class=\"wp-block-image size-large\"><img loading=\"lazy\" decoding=\"async\" width=\"3000\" height=\"2000\" src=\"https:\/\/wp.technologyreview.com\/wp-content\/uploads\/2026\/04\/North_Pole_Expedition_MIT_Tech_Rev_TimK_007.jpg?w=3000\" alt=\"closeup of hands holding an instrument to a tray under a microscope\" class=\"wp-image-1135784\" \/><figcaption class=\"wp-element-caption\">Under the microscope, PhD student Paulina Romel picks shells of unicellular foraminifera from a sample. The chemical composition of these microfossils can give clues about the age of the sediment and the surface water temperature when the organisms were still alive. \u201cThese are really cool creatures!\u201d says Romel.<\/figcaption><div class=\"image-credit\">TIM KALVELAGE<\/div>\n<\/figure>\n<\/div>\n<div class=\"wp-block-image\">\n<figure class=\"wp-block-image size-large\"><img loading=\"lazy\" decoding=\"async\" height=\"2000\" width=\"1481\" src=\"https:\/\/wp.technologyreview.com\/wp-content\/uploads\/2026\/04\/North_Pole_Expedition_MIT_Tech_Rev_TimK_006.jpg?w=1481\" alt='\"\"' class=\"wp-image-1135783\" \/><figcaption class=\"wp-element-caption\">Agathe Ollive, a geochemist from the Alfred Wegener Institute in Germany, takes water samples from a CTD rosette, an instrument package that measures conductivity (salinity) and temperature at various depths. She uses certain elements to trace the inflow of fresh water and seawater from rivers and adjacent ocean basins into the Arctic. \u201cI didn\u2019t expect there to be so little ice up here,\u201d Ollive says. She is worried about how the Arctic will look 20 years from now.<\/figcaption><div class=\"image-credit\">TIM KALVELAGE<\/div>\n<\/figure>\n<\/div>\n<p>Some of this work was done while the researchers were still at sea. Now, at their home laboratories, they are finalizing their analysis of the seafloor samples. One important task is dating the sediments, which may be up to 2 million years old. The team uses a combination of methods to do this, including measuring magnetization, the decay of radioactive elements, and the exposure of mineral grains to sunlight before sinking to the depths. Once they can place them on a timeline, the materials in the cores will help researchers paint a picture of what the Arctic Ocean looked like in times that were warmer than today. For example, the presence or absence of the molecule IP<sub>25<\/sub>, which is produced exclusively by ice algae, could tell them how far the sea ice receded at a given time.\u00a0<\/p>\n<div class=\"wp-block-image\">\n<figure class=\"wp-block-image size-large\"><img loading=\"lazy\" decoding=\"async\" height=\"2000\" width=\"1500\" src=\"https:\/\/wp.technologyreview.com\/wp-content\/uploads\/2026\/04\/North_Pole_Expedition_MIT_Tech_Rev_TimK_008.jpg?w=1500\" alt=\"a sea bird flies past an iceberg\" class=\"wp-image-1135785\" \/><figcaption class=\"wp-element-caption\">Toward the end of the expedition, the Kronprins Haakon passes this iceberg near the northeast coast of Greenland.<\/figcaption><div class=\"image-credit\">TIM KALVELAGE<\/div>\n<\/figure>\n<\/div>\n<p>At the end of the study, the team hopes to have data that could improve climate projections for a future ice-free \u201cblue Arctic,\u201d helping us understand how it could affect marine life and carbon storage, Atlantic Ocean circulation, or extreme weather events in Europe and North America.\u00a0<\/p>\n<p><a href=\"https:\/\/www.timkalvelage.de\/\">Tim Kalvelage<\/a><em> is a freelance science reporter based in Bremen, Germany, who focuses on climate, ocean, and polar research. He has been to the North Pole twice.<\/em><\/p>","protected":false},"excerpt":{"rendered":"<p>In the past, even with an icebreaker and during peak melt season, getting to the North Pole wasn\u2019t a sure bet. It took favorable winds to crack the frozen ocean surface, and ships had to fight through ice that had grown many meters thick over several winters. In the summer of 2025, though, Jochen Knies from the Arctic University of Norway, Troms\u00f8, and his team met little resistance on their way to 90 degrees North with the research vessel Kronprins Haakon. The geologist \u201cdidn\u2019t hear the usual grinding of ice\u201d against the hull that he remembered from 1996, when he first reached the pole by ship. Instead, thin floes and large stretches of open water made for an easy, quiet passage. To him, it was \u201ca reminder of how quickly the Arctic is changing.\u201d Since the late 1970s, when satellite observations of the polar seas began, summer ice cover of the Arctic Ocean has declined by more than 40%. In less than half a century, a frozen area the size of the Mediterranean Sea has turned into blue open water with the rapid warming of the high northern latitudes. If this trend continues, there could soon be summers at the North Pole with no sea ice whatsoever. The last time this happened may have been some 120,000 years ago. But no one knows for certain. That\u2019s why Knies and his colleagues, a team of researchers from Norway and Germany, set out from Svalbard to the central Arctic last August. The aim of their five-week mission was to determine whether this region had been ice-free in recent Earth history\u2014and if so, when. As part of a \u20ac12.5 million project financed by the European Union, they also came to answer some questions about the future of the Arctic and beyond: How does the loss of sea ice affect the marine ecosystem? What are the consequences for ocean circulation and global climate? In search of clues, the expedition collected sediment cores up to 22 meters in length at different locations across the Arctic seafloor. Marine sediments are valuable climate archives that give scientists a window into bygone eras. Like diligent record keepers, they can log past water temperatures, sea-ice coverage, and the strength of ocean currents. These data are encrypted in the chemical and physical properties of the plankton remains and weathered rock deposited on the seabed.\u00a0 The ship\u2019s crew and researchers recover the sediment corer, a 25-meter-long steel pipe that is driven into the seafloor using a top weight of more than three metric tons.TIM KALVELAGE Together, the scientists pull out long plastic pipes filled with precious deep-sea mud.TIM KALVELAGE The pipes are cut into shorter pieces and split in half before being processed in the ship\u2019s laboratories. Each of these one-meter sections covers several tens of thousands of years of Earth\u2019s history.TIM KALVELAGE While sediment cores several meters long had been recovered on earlier expeditions in the central Arctic, there is no scientific consensus on how old the deposits actually are or whether sea ice ever completely disappeared in summer.\u00a0 To decode the Arctic\u2019s climate archive, Knies brought a team of experts from various disciplines onboard the Kronprins Haakon to dig deeper and obtain fresh samples they could subject to the latest analytical techniques.\u00a0 \u00a0 Samples await paleomagnetic dating. Like tiny compass needles, iron-rich particles align with Earth\u2019s shifting magnetic field as they settle on the seabed. By measuring their orientation, researchers can estimate the age of the different sediment layers.TIM KALVELAGE Under the microscope, PhD student Paulina Romel picks shells of unicellular foraminifera from a sample. The chemical composition of these microfossils can give clues about the age of the sediment and the surface water temperature when the organisms were still alive. \u201cThese are really cool creatures!\u201d says Romel.TIM KALVELAGE Agathe Ollive, a geochemist from the Alfred Wegener Institute in Germany, takes water samples from a CTD rosette, an instrument package that measures conductivity (salinity) and temperature at various depths. She uses certain elements to trace the inflow of fresh water and seawater from rivers and adjacent ocean basins into the Arctic. \u201cI didn\u2019t expect there to be so little ice up here,\u201d Ollive says. She is worried about how the Arctic will look 20 years from now.TIM KALVELAGE Some of this work was done while the researchers were still at sea. Now, at their home laboratories, they are finalizing their analysis of the seafloor samples. One important task is dating the sediments, which may be up to 2 million years old. The team uses a combination of methods to do this, including measuring magnetization, the decay of radioactive elements, and the exposure of mineral grains to sunlight before sinking to the depths. Once they can place them on a timeline, the materials in the cores will help researchers paint a picture of what the Arctic Ocean looked like in times that were warmer than today. For example, the presence or absence of the molecule IP25, which is produced exclusively by ice algae, could tell them how far the sea ice receded at a given time.\u00a0 Toward the end of the expedition, the Kronprins Haakon passes this iceberg near the northeast coast of Greenland.TIM KALVELAGE At the end of the study, the team hopes to have data that could improve climate projections for a future ice-free \u201cblue Arctic,\u201d helping us understand how it could affect marine life and carbon storage, Atlantic Ocean circulation, or extreme weather events in Europe and North America.\u00a0 Tim Kalvelage is a freelance science reporter based in Bremen, Germany, who focuses on climate, ocean, and polar research. He has been to the North Pole twice.<\/p>","protected":false},"author":2,"featured_media":85017,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"_acf_changed":false,"pmpro_default_level":"","site-sidebar-layout":"default","site-content-layout":"","ast-site-content-layout":"","site-content-style":"default","site-sidebar-style":"default","ast-global-header-display":"","ast-banner-title-visibility":"","ast-main-header-display":"","ast-hfb-above-header-display":"","ast-hfb-below-header-display":"","ast-hfb-mobile-header-display":"","site-post-title":"","ast-breadcrumbs-content":"","ast-featured-img":"","footer-sml-layout":"","theme-transparent-header-meta":"","adv-header-id-meta":"","stick-header-meta":"","header-above-stick-meta":"","header-main-stick-meta":"","header-below-stick-meta":"","astra-migrate-meta-layouts":"default","ast-page-background-enabled":"default","ast-page-background-meta":{"desktop":{"background-color":"var(--ast-global-color-4)","background-image":"","background-repeat":"repeat","background-position":"center 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NU","author_link":"https:\/\/youzum.net\/ja\/members\/adminnu\/"},"rttpg_comment":0,"rttpg_category":"<a href=\"https:\/\/youzum.net\/ja\/category\/ai-club\/\" rel=\"category tag\">AI<\/a> <a href=\"https:\/\/youzum.net\/ja\/category\/committee\/\" rel=\"category tag\">Committee<\/a> <a href=\"https:\/\/youzum.net\/ja\/category\/news\/\" rel=\"category tag\">News<\/a> <a href=\"https:\/\/youzum.net\/ja\/category\/uncategorized\/\" rel=\"category tag\">Uncategorized<\/a>","rttpg_excerpt":"In the past, even with an icebreaker and during peak melt season, getting to the North Pole wasn\u2019t a sure bet. It took favorable winds to crack the frozen ocean surface, and ships had to fight through ice that had grown many meters thick over several winters. 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