{"id":950,"date":"2021-09-10T13:22:16","date_gmt":"2021-09-10T13:22:16","guid":{"rendered":"https:\/\/andrea-koschinsky.org\/?page_id=950"},"modified":"2025-12-01T14:29:01","modified_gmt":"2025-12-01T14:29:01","slug":"research-projects","status":"publish","type":"page","link":"https:\/\/andrea-koschinsky.org\/pt\/research-projects\/","title":{"rendered":"Research projects"},"content":{"rendered":"<p><strong>Ongoing research projects<\/strong><\/p>\n\n\n\n<p><strong><a href=\"https:\/\/andrea-koschinsky.org\/pt\/research-projects\/dss-ii\/\" data-type=\"page\" data-id=\"3688\">Deep Sea Sampling 2 (DSSII)<\/a><\/strong><\/p>\n\n\n\n<div class=\"wp-block-columns is-layout-flex wp-container-core-columns-is-layout-9d6595d7 wp-block-columns-is-layout-flex\">\n<div class=\"wp-block-column is-layout-flow wp-block-column-is-layout-flow\">\n<p>In the Deep Sea Sampling project headed by Bauer Maschinenbau, a minimally invasive extracting technology is being developed for vertical mining of massive sulphide deposits in the deep sea. Our part of the project focusses on developing the technology and monitoring concept to quantify the emissions of heavy metals and particles to the surrounding water to develop effective monitoring and mitigation concepts in potential future applications of massive sulphide minig.<\/p>\n<\/div>\n\n\n\n<div class=\"wp-block-column is-layout-flow wp-block-column-is-layout-flow\"><div class=\"wp-block-image\">\n<figure class=\"aligncenter size-large is-resized\"><a href=\"https:\/\/andrea-koschinsky.org\/wp-content\/uploads\/2025\/10\/image.png\"><img decoding=\"async\" width=\"1024\" height=\"565\" src=\"https:\/\/andrea-koschinsky.org\/wp-content\/uploads\/2025\/10\/image-1024x565.png\" alt=\"\" class=\"wp-image-3743\" style=\"width:495px;height:auto\" srcset=\"https:\/\/andrea-koschinsky.org\/wp-content\/uploads\/2025\/10\/image-1024x565.png 1024w, https:\/\/andrea-koschinsky.org\/wp-content\/uploads\/2025\/10\/image-300x166.png 300w, https:\/\/andrea-koschinsky.org\/wp-content\/uploads\/2025\/10\/image-768x424.png 768w, https:\/\/andrea-koschinsky.org\/wp-content\/uploads\/2025\/10\/image-1536x847.png 1536w, https:\/\/andrea-koschinsky.org\/wp-content\/uploads\/2025\/10\/image-2048x1130.png 2048w, https:\/\/andrea-koschinsky.org\/wp-content\/uploads\/2025\/10\/image-18x10.png 18w, https:\/\/andrea-koschinsky.org\/wp-content\/uploads\/2025\/10\/image-1200x662.png 1200w, https:\/\/andrea-koschinsky.org\/wp-content\/uploads\/2025\/10\/image-600x330.png?crop=1 600w\" sizes=\"(max-width: 1024px) 100vw, 1024px\" \/><\/a><\/figure>\n<\/div><\/div>\n<\/div>\n\n\n\n<p><a href=\"https:\/\/andrea-koschinsky.org\/pt\/tag\/m206\/\" data-type=\"post_tag\" data-id=\"6\"><strong>M206 &#8211; Amazon-GEOTRACES-2 (Dry Season)<\/strong><\/a><\/p>\n\n\n\n<div class=\"wp-block-columns is-layout-flex wp-container-core-columns-is-layout-9d6595d7 wp-block-columns-is-layout-flex\">\n<div class=\"wp-block-column is-layout-flow wp-block-column-is-layout-flow\" style=\"flex-basis:33.33%\">\n<figure class=\"wp-block-image size-large is-resized\"><a href=\"https:\/\/andrea-koschinsky.org\/wp-content\/uploads\/2024\/11\/M206_cruise-small-e1731260814583.jpeg\"><img decoding=\"async\" width=\"1024\" height=\"1024\" src=\"https:\/\/andrea-koschinsky.org\/wp-content\/uploads\/2024\/11\/M206_cruise-small-1024x1024.jpeg\" alt=\"\" class=\"wp-image-2598\" style=\"width:189px;height:auto\"\/><\/a><\/figure>\n<\/div>\n\n\n\n<div class=\"wp-block-column is-layout-flow wp-block-column-is-layout-flow\" style=\"flex-basis:66.66%\">\n<p>The Amazon-GEOTRACES -2 project studies interactions of trace metals with dissolved organic matter and colloids in the Amazon and Par\u00e1 River estuaries and associated plumes as well as the mangrove belt south of the Par\u00e1 as key processes for trace metal fluxes into the Atlantic. This cruise takes place during the dry season as a comparison to the previous cruise M147 during the wet season in 2018.<\/p>\n<\/div>\n<\/div>\n\n\n\n<p><a href=\"https:\/\/andrea-koschinsky.org\/pt\/research-projects\/probral\/\" data-type=\"page\" data-id=\"2678\"><strong>PROBRAL<\/strong><\/a><\/p>\n\n\n\n<p>Within the PROBRAL exchange program of DAAD and CAPES, we have a longstanding collaboration with several working groups at brazilian institutions involving exchange of PhD students and PostDocs as well as joint sampling campaigns in the amazon estuarine area and mangrove belt of northeastern Brazil..<\/p>\n\n\n\n<div class=\"wp-block-columns is-layout-flex wp-container-core-columns-is-layout-9d6595d7 wp-block-columns-is-layout-flex\">\n<div class=\"wp-block-column is-layout-flow wp-block-column-is-layout-flow\" style=\"flex-basis:66.66%\">\n<p><strong><em><a href=\"https:\/\/andrea-koschinsky.org\/pt\/research-projects\/msm131\/\">Magma-Sediment Interaction at the Ultraslow-Spreading Knipovich Ridge<\/a><\/em><\/strong><\/p>\n\n\n\n<p>In this project, we study the recently discovered J\u00f8tul Hydrothermal Field by sampling the hydrothermal fluids and rising plume during research cruise MSM131 (RV Maria S. Merian, 2024).<\/p>\n<\/div>\n\n\n\n<div class=\"wp-block-column is-layout-flow wp-block-column-is-layout-flow\" style=\"flex-basis:33.33%\"><div class=\"wp-block-image\">\n<figure class=\"aligncenter size-full is-resized\"><a href=\"https:\/\/andrea-koschinsky.org\/pt\/research-projects\/msm131\/\"><img decoding=\"async\" width=\"288\" height=\"288\" src=\"https:\/\/andrea-koschinsky.org\/wp-content\/uploads\/2024\/08\/Picture-2-1-edited-1.png\" alt=\"\" class=\"wp-image-2503\" style=\"width:234px;height:auto\" srcset=\"https:\/\/andrea-koschinsky.org\/wp-content\/uploads\/2024\/08\/Picture-2-1-edited-1.png 288w, https:\/\/andrea-koschinsky.org\/wp-content\/uploads\/2024\/08\/Picture-2-1-edited-1-150x150.png?crop=1 150w, https:\/\/andrea-koschinsky.org\/wp-content\/uploads\/2024\/08\/Picture-2-1-edited-1-200x200.png?crop=1 200w, https:\/\/andrea-koschinsky.org\/wp-content\/uploads\/2024\/08\/Picture-2-1-edited-1-230x230.png?crop=1 230w\" sizes=\"(max-width: 288px) 100vw, 288px\" \/><\/a><\/figure>\n<\/div><\/div>\n<\/div>\n\n\n\n<div class=\"wp-block-columns is-layout-flex wp-container-core-columns-is-layout-9d6595d7 wp-block-columns-is-layout-flex\">\n<div class=\"wp-block-column is-layout-flow wp-block-column-is-layout-flow\" style=\"flex-basis:33.33%\"><div class=\"wp-block-image\">\n<figure class=\"aligncenter size-full is-resized\"><img decoding=\"async\" width=\"652\" height=\"652\" src=\"https:\/\/andrea-koschinsky.org\/wp-content\/uploads\/2025\/11\/Cruise-Logo-SO301-KABA.png\" alt=\"\" class=\"wp-image-3776\" style=\"width:191px;height:auto\" srcset=\"https:\/\/andrea-koschinsky.org\/wp-content\/uploads\/2025\/11\/Cruise-Logo-SO301-KABA.png 652w, https:\/\/andrea-koschinsky.org\/wp-content\/uploads\/2025\/11\/Cruise-Logo-SO301-KABA-300x300.png 300w, https:\/\/andrea-koschinsky.org\/wp-content\/uploads\/2025\/11\/Cruise-Logo-SO301-KABA-150x150.png?crop=1 150w, https:\/\/andrea-koschinsky.org\/wp-content\/uploads\/2025\/11\/Cruise-Logo-SO301-KABA-12x12.png 12w, https:\/\/andrea-koschinsky.org\/wp-content\/uploads\/2025\/11\/Cruise-Logo-SO301-KABA-600x600.png?crop=1 600w, https:\/\/andrea-koschinsky.org\/wp-content\/uploads\/2025\/11\/Cruise-Logo-SO301-KABA-400x400.png?crop=1 400w, https:\/\/andrea-koschinsky.org\/wp-content\/uploads\/2025\/11\/Cruise-Logo-SO301-KABA-200x200.png?crop=1 200w, https:\/\/andrea-koschinsky.org\/wp-content\/uploads\/2025\/11\/Cruise-Logo-SO301-KABA-230x230.png?crop=1 230w, https:\/\/andrea-koschinsky.org\/wp-content\/uploads\/2025\/11\/Cruise-Logo-SO301-KABA-365x365.png?crop=1 365w\" sizes=\"(max-width: 652px) 100vw, 652px\" \/><\/figure>\n<\/div><\/div>\n\n\n\n<div class=\"wp-block-column is-layout-flow wp-block-column-is-layout-flow\" style=\"flex-basis:66.66%\">\n<p><em><strong><a href=\"https:\/\/andrea-koschinsky.org\/pt\/research-projects\/kaba\/\">The Kairei Hydrothermal Plume at the Central Indian Ridge<\/a><\/strong><\/em><\/p>\n\n\n\n<p>Official Title: &#8220;Ramifications of Venting at the <strong>Ka<\/strong>irei Hydrothermal Field for <strong>Ba<\/strong>thypelagic Microbial Processes in Consort with Carbon and Metal Cycling&#8221; (KABA).The aim of this program is to determine the biogeochemical cycling in the bathypelagic ocean above the Kairei Hydrothermal Field (KHF) and to understand how the hydrothermal fluids affect microbial life.&nbsp;For this project, we sampled the hydrothermal plume of the KHF during research cruise SO301 (RV Sonne, 2023\/24) to analyze trace metal distribution and speciation.<\/p>\n<\/div>\n<\/div>\n\n\n\n<div class=\"wp-block-columns is-layout-flex wp-container-core-columns-is-layout-9d6595d7 wp-block-columns-is-layout-flex\">\n<div class=\"wp-block-column is-layout-flow wp-block-column-is-layout-flow\" style=\"flex-basis:66.66%\">\n<p><strong><em><a href=\"https:\/\/andrea-koschinsky.org\/pt\/news\/new-project-in-the-dfg-special-priority-program-2238-dome-dynamics-of-ore-metal-enrichment\/\">Dynamics of Ore Metals Enrichment (DOME)<\/a><\/em><\/strong><\/p>\n\n\n\n<p>This project studies the role of p-T conditions, host rock lithology, phase separation, and organic compounds on metal mobility and metal sulfide deposition in spatially resolved hydrothermal vent areas.<\/p>\n<\/div>\n\n\n\n<div class=\"wp-block-column is-layout-flow wp-block-column-is-layout-flow\" style=\"flex-basis:33.33%\"><div class=\"wp-block-image\">\n<figure class=\"aligncenter size-full is-resized\"><a href=\"https:\/\/andrea-koschinsky.org\/pt\/research-projects\/dome\/\"><img decoding=\"async\" width=\"599\" height=\"405\" src=\"https:\/\/andrea-koschinsky.org\/wp-content\/uploads\/2024\/08\/DOME-1.png\" alt=\"\" class=\"wp-image-2499\" style=\"width:257px;height:auto\" srcset=\"https:\/\/andrea-koschinsky.org\/wp-content\/uploads\/2024\/08\/DOME-1.png 599w, https:\/\/andrea-koschinsky.org\/wp-content\/uploads\/2024\/08\/DOME-1-300x203.png 300w\" sizes=\"(max-width: 599px) 100vw, 599px\" \/><\/a><\/figure>\n<\/div><\/div>\n<\/div>\n\n\n\n<div class=\"wp-block-columns is-layout-flex wp-container-core-columns-is-layout-9d6595d7 wp-block-columns-is-layout-flex\">\n<div class=\"wp-block-column is-layout-flow wp-block-column-is-layout-flow\" style=\"flex-basis:33.33%\"><div class=\"wp-block-image\">\n<figure class=\"aligncenter size-large is-resized\"><a href=\"https:\/\/andrea-koschinsky.org\/pt\/research-projects\/m192-bridgehell\/\"><img decoding=\"async\" width=\"1024\" height=\"1024\" src=\"https:\/\/andrea-koschinsky.org\/wp-content\/uploads\/2024\/08\/M192_logo-2-1024x1024.jpg\" alt=\"\" class=\"wp-image-2506\" style=\"width:233px;height:auto\" srcset=\"https:\/\/andrea-koschinsky.org\/wp-content\/uploads\/2024\/08\/M192_logo-2-1024x1024.jpg 1024w, https:\/\/andrea-koschinsky.org\/wp-content\/uploads\/2024\/08\/M192_logo-2-300x300.jpg 300w, https:\/\/andrea-koschinsky.org\/wp-content\/uploads\/2024\/08\/M192_logo-2-150x150.jpg?crop=1 150w, https:\/\/andrea-koschinsky.org\/wp-content\/uploads\/2024\/08\/M192_logo-2-768x769.jpg 768w, https:\/\/andrea-koschinsky.org\/wp-content\/uploads\/2024\/08\/M192_logo-2-800x800.jpg?crop=1 800w, https:\/\/andrea-koschinsky.org\/wp-content\/uploads\/2024\/08\/M192_logo-2-600x600.jpg?crop=1 600w, https:\/\/andrea-koschinsky.org\/wp-content\/uploads\/2024\/08\/M192_logo-2-400x400.jpg?crop=1 400w, https:\/\/andrea-koschinsky.org\/wp-content\/uploads\/2024\/08\/M192_logo-2-200x200.jpg?crop=1 200w, https:\/\/andrea-koschinsky.org\/wp-content\/uploads\/2024\/08\/M192_logo-2-230x230.jpg?crop=1 230w, https:\/\/andrea-koschinsky.org\/wp-content\/uploads\/2024\/08\/M192_logo-2-365x365.jpg?crop=1 365w, https:\/\/andrea-koschinsky.org\/wp-content\/uploads\/2024\/08\/M192_logo-2.jpg 1044w\" sizes=\"(max-width: 1024px) 100vw, 1024px\" \/><\/a><\/figure>\n<\/div><\/div>\n\n\n\n<div class=\"wp-block-column is-layout-flow wp-block-column-is-layout-flow\" style=\"flex-basis:66.66%\">\n<p><strong><em><a href=\"https:\/\/andrea-koschinsky.org\/pt\/research-projects\/m192-bridgehell\/\">BridgeHell<\/a><\/em><\/strong><\/p>\n\n\n\n<p>In this project, we investigate and sample shallow and deep sea hydrothermal outflow and venting in the Mediterranean close to the island of Milos during cruise M192 (RV Meteor, 2023). The cruise was be separated into two parts. The first part of the cruise was be dedicated to localizing the hydrothermal sites along a depth profile from 10m to 900m depth. During the second half of the cruise, the participants sampled the newly discovered vent sites for fluids, rocks, fauna and sediments. The topic of our team is the geochemistry of hydrothermal fluids and plumes with focus on trace metals and their interactions with organisms.<\/p>\n<\/div>\n<\/div>\n\n\n\n<div class=\"wp-block-columns is-layout-flex wp-container-core-columns-is-layout-9d6595d7 wp-block-columns-is-layout-flex\">\n<div class=\"wp-block-column is-layout-flow wp-block-column-is-layout-flow\">\n<p><strong><a href=\"https:\/\/andrea-koschinsky.org\/pt\/research-projects\/divemartmar1and2\/\" data-type=\"page\" data-id=\"3593\"><em>Dive@MAR<\/em> 1 &amp; 2<\/a><\/strong><\/p>\n\n\n\n<p>Studying the <strong>Di<\/strong>stribution of <strong>Ve<\/strong>nting Along the <strong>M<\/strong>id-<strong>A<\/strong>tlantic <strong>R<\/strong>idge (29\u201338\u00b0N) and Implications for Hydrothermal Exchange and Vent Ecosystems during research cruise <a href=\"https:\/\/andrea-koschinsky.org\/pt\/research-projects\/divemartmar1and2\/m190-dive-mar\/\" data-type=\"page\" data-id=\"2216\">M190 (RV Meteor, 2023) <\/a>and <a href=\"https:\/\/andrea-koschinsky.org\/pt\/research-projects\/divemartmar1and2\/diveatmar2\/\" data-type=\"page\" data-id=\"3603\">M210 (RV Meteor, 2025)<\/a>.<\/p>\n<\/div>\n\n\n\n<div class=\"wp-block-column is-layout-flow wp-block-column-is-layout-flow\"><div class=\"wp-block-image\">\n<figure class=\"aligncenter size-full is-resized\"><a href=\"https:\/\/andrea-koschinsky.org\/pt\/research-projects\/m190-dive-mar\/\"><img decoding=\"async\" width=\"768\" height=\"768\" src=\"https:\/\/andrea-koschinsky.org\/wp-content\/uploads\/2024\/08\/M190_Cruise_Logo-768x768.png.webp\" alt=\"\" class=\"wp-image-2509\" style=\"width:196px;height:auto\" srcset=\"https:\/\/andrea-koschinsky.org\/wp-content\/uploads\/2024\/08\/M190_Cruise_Logo-768x768.png.webp 768w, https:\/\/andrea-koschinsky.org\/wp-content\/uploads\/2024\/08\/M190_Cruise_Logo-768x768.png-300x300.webp 300w, https:\/\/andrea-koschinsky.org\/wp-content\/uploads\/2024\/08\/M190_Cruise_Logo-768x768.png-150x150.webp?crop=1 150w, https:\/\/andrea-koschinsky.org\/wp-content\/uploads\/2024\/08\/M190_Cruise_Logo-768x768.png-600x600.webp?crop=1 600w, https:\/\/andrea-koschinsky.org\/wp-content\/uploads\/2024\/08\/M190_Cruise_Logo-768x768.png-400x400.webp?crop=1 400w, https:\/\/andrea-koschinsky.org\/wp-content\/uploads\/2024\/08\/M190_Cruise_Logo-768x768.png-200x200.webp?crop=1 200w, https:\/\/andrea-koschinsky.org\/wp-content\/uploads\/2024\/08\/M190_Cruise_Logo-768x768.png-230x230.webp?crop=1 230w, https:\/\/andrea-koschinsky.org\/wp-content\/uploads\/2024\/08\/M190_Cruise_Logo-768x768.png-365x365.webp?crop=1 365w\" sizes=\"(max-width: 768px) 100vw, 768px\" \/><\/a><\/figure>\n<\/div><\/div>\n\n\n\n<div class=\"wp-block-column is-layout-flow wp-block-column-is-layout-flow\"><div class=\"wp-block-image\">\n<figure class=\"aligncenter size-full is-resized\"><a href=\"https:\/\/andrea-koschinsky.org\/pt\/research-projects\/divemartmar1and2\/diveatmar2\/\"><img decoding=\"async\" width=\"364\" height=\"364\" src=\"https:\/\/andrea-koschinsky.org\/wp-content\/uploads\/2025\/07\/image-4.png\" alt=\"\" class=\"wp-image-3617\" style=\"width:202px;height:auto\" srcset=\"https:\/\/andrea-koschinsky.org\/wp-content\/uploads\/2025\/07\/image-4.png 364w, https:\/\/andrea-koschinsky.org\/wp-content\/uploads\/2025\/07\/image-4-300x300.png 300w, https:\/\/andrea-koschinsky.org\/wp-content\/uploads\/2025\/07\/image-4-150x150.png?crop=1 150w, https:\/\/andrea-koschinsky.org\/wp-content\/uploads\/2025\/07\/image-4-12x12.png 12w, https:\/\/andrea-koschinsky.org\/wp-content\/uploads\/2025\/07\/image-4-200x200.png?crop=1 200w, https:\/\/andrea-koschinsky.org\/wp-content\/uploads\/2025\/07\/image-4-230x230.png?crop=1 230w\" sizes=\"(max-width: 364px) 100vw, 364px\" \/><\/a><\/figure>\n<\/div><\/div>\n<\/div>\n\n\n\n<div class=\"wp-block-columns is-layout-flex wp-container-core-columns-is-layout-9d6595d7 wp-block-columns-is-layout-flex\">\n<div class=\"wp-block-column is-layout-flow wp-block-column-is-layout-flow\" style=\"flex-basis:33.33%\"><div class=\"wp-block-image\">\n<figure class=\"aligncenter size-full is-resized\"><a href=\"https:\/\/andrea-koschinsky.org\/pt\/research-projects\/rainbow\/\"><img decoding=\"async\" width=\"862\" height=\"866\" src=\"https:\/\/andrea-koschinsky.org\/wp-content\/uploads\/2024\/08\/Screenshot-2024-08-25-at-11.44.00.png\" alt=\"\" class=\"wp-image-2516\" style=\"width:189px;height:auto\" srcset=\"https:\/\/andrea-koschinsky.org\/wp-content\/uploads\/2024\/08\/Screenshot-2024-08-25-at-11.44.00.png 862w, https:\/\/andrea-koschinsky.org\/wp-content\/uploads\/2024\/08\/Screenshot-2024-08-25-at-11.44.00-300x300.png 300w, https:\/\/andrea-koschinsky.org\/wp-content\/uploads\/2024\/08\/Screenshot-2024-08-25-at-11.44.00-150x150.png?crop=1 150w, https:\/\/andrea-koschinsky.org\/wp-content\/uploads\/2024\/08\/Screenshot-2024-08-25-at-11.44.00-768x772.png 768w, https:\/\/andrea-koschinsky.org\/wp-content\/uploads\/2024\/08\/Screenshot-2024-08-25-at-11.44.00-200x200.png?crop=1 200w, https:\/\/andrea-koschinsky.org\/wp-content\/uploads\/2024\/08\/Screenshot-2024-08-25-at-11.44.00-230x230.png?crop=1 230w\" sizes=\"(max-width: 862px) 100vw, 862px\" \/><\/a><\/figure>\n<\/div><\/div>\n\n\n\n<div class=\"wp-block-column is-layout-flow wp-block-column-is-layout-flow\" style=\"flex-basis:66.66%\">\n<p><em><strong><a href=\"https:\/\/andrea-koschinsky.org\/pt\/research-projects\/rainbow\/\">The Rainbow Plume<\/a><\/strong><\/em><\/p>\n\n\n\n<p>The RainbowPlume project, led by GEOMAR Helmholtz-Centre for Ocean Research Kiel, aims at obtaining a mechanistic and quantitative understanding of the processes that set the hydrothermal flux of trace elements and their isotopes (TEI) at the Rainbow vent field on the Mid-Atlantic Ridge near the Azores.&nbsp;It is associated with the research cruise M176-2 and forms part of the GEOTRACES initiative.<\/p>\n<\/div>\n<\/div>\n\n\n\n<div class=\"wp-block-columns is-layout-flex wp-container-core-columns-is-layout-9d6595d7 wp-block-columns-is-layout-flex\">\n<div class=\"wp-block-column is-layout-flow wp-block-column-is-layout-flow\" style=\"flex-basis:66.66%\">\n<p><em><strong><a href=\"https:\/\/andrea-koschinsky.org\/pt\/research-projects\/tram\/\">The TRAM project<\/a><\/strong><\/em><\/p>\n\n\n\n<p>TRAM is short for &#8220;Tracing origin and distribution of geogenic and anthropogenic dissolved and particulate critical high-technology metals in the southern North Sea&#8221;. The project, associated with the Meteor Cruise M169 under the lead of Prof. Dr. Andrea Koschinsky (chief scientist) to the North Sea is a joint project of the Koschinsky, Thomsen, Bau, Ullrich, and Unnithan Group at Jacobs University, the German Federal Institute for Geosciences and Resources (BGR) and Christian-Albrechts-University Kiel.<\/p>\n<\/div>\n\n\n\n<div class=\"wp-block-column is-layout-flow wp-block-column-is-layout-flow\" style=\"flex-basis:33.33%\"><div class=\"wp-block-image\">\n<figure class=\"aligncenter size-full is-resized\"><a href=\"https:\/\/andrea-koschinsky.org\/pt\/research-projects\/tram\/\"><img decoding=\"async\" width=\"768\" height=\"768\" src=\"https:\/\/andrea-koschinsky.org\/wp-content\/uploads\/2024\/08\/Logo-Nordseefahrt-1-768x768-1.jpg\" alt=\"\" class=\"wp-image-2525\" style=\"width:223px;height:auto\" srcset=\"https:\/\/andrea-koschinsky.org\/wp-content\/uploads\/2024\/08\/Logo-Nordseefahrt-1-768x768-1.jpg 768w, https:\/\/andrea-koschinsky.org\/wp-content\/uploads\/2024\/08\/Logo-Nordseefahrt-1-768x768-1-300x300.jpg 300w, https:\/\/andrea-koschinsky.org\/wp-content\/uploads\/2024\/08\/Logo-Nordseefahrt-1-768x768-1-150x150.jpg?crop=1 150w, https:\/\/andrea-koschinsky.org\/wp-content\/uploads\/2024\/08\/Logo-Nordseefahrt-1-768x768-1-600x600.jpg?crop=1 600w, https:\/\/andrea-koschinsky.org\/wp-content\/uploads\/2024\/08\/Logo-Nordseefahrt-1-768x768-1-400x400.jpg?crop=1 400w, https:\/\/andrea-koschinsky.org\/wp-content\/uploads\/2024\/08\/Logo-Nordseefahrt-1-768x768-1-200x200.jpg?crop=1 200w, https:\/\/andrea-koschinsky.org\/wp-content\/uploads\/2024\/08\/Logo-Nordseefahrt-1-768x768-1-230x230.jpg?crop=1 230w, https:\/\/andrea-koschinsky.org\/wp-content\/uploads\/2024\/08\/Logo-Nordseefahrt-1-768x768-1-365x365.jpg?crop=1 365w\" sizes=\"(max-width: 768px) 100vw, 768px\" \/><\/a><\/figure>\n<\/div><\/div>\n<\/div>\n\n\n\n<div class=\"wp-block-columns is-layout-flex wp-container-core-columns-is-layout-9d6595d7 wp-block-columns-is-layout-flex\">\n<div class=\"wp-block-column is-layout-flow wp-block-column-is-layout-flow\" style=\"flex-basis:33.33%\"><div class=\"wp-block-image\">\n<figure class=\"aligncenter size-large is-resized\"><a href=\"https:\/\/andrea-koschinsky.org\/pt\/research-projects\/so298\/\"><img decoding=\"async\" width=\"1024\" height=\"633\" src=\"https:\/\/andrea-koschinsky.org\/wp-content\/uploads\/2024\/08\/Screenshot-2024-08-25-at-11.50.33-1024x633.png\" alt=\"\" class=\"wp-image-2523\" style=\"width:265px;height:auto\" srcset=\"https:\/\/andrea-koschinsky.org\/wp-content\/uploads\/2024\/08\/Screenshot-2024-08-25-at-11.50.33-1024x633.png 1024w, https:\/\/andrea-koschinsky.org\/wp-content\/uploads\/2024\/08\/Screenshot-2024-08-25-at-11.50.33-300x186.png 300w, https:\/\/andrea-koschinsky.org\/wp-content\/uploads\/2024\/08\/Screenshot-2024-08-25-at-11.50.33-768x475.png 768w, https:\/\/andrea-koschinsky.org\/wp-content\/uploads\/2024\/08\/Screenshot-2024-08-25-at-11.50.33.png 1122w\" sizes=\"(max-width: 1024px) 100vw, 1024px\" \/><\/a><\/figure>\n<\/div><\/div>\n\n\n\n<div class=\"wp-block-column is-layout-flow wp-block-column-is-layout-flow\" style=\"flex-basis:66.66%\">\n<p><strong><em><a href=\"https:\/\/andrea-koschinsky.org\/pt\/research-projects\/so298\/\">Equatorial Pacific GEOTRACES<\/a><\/em><\/strong> <\/p>\n\n\n\n<p>The Equatorial Pacific GEOTRACES project explores dissolved trace element concentration and speciation in the Equatorial Pacific Ocean. For this project, a transect was sampled across the Equatorial Pacific Ocean from Ecuador to Australia during research cruise SO298 (RV Sonne, 2023).<\/p>\n<\/div>\n<\/div>\n\n\n\n<div class=\"wp-block-columns is-layout-flex wp-container-core-columns-is-layout-9d6595d7 wp-block-columns-is-layout-flex\">\n<div class=\"wp-block-column is-layout-flow wp-block-column-is-layout-flow\" style=\"flex-basis:66.66%\">\n<p><em><strong><a href=\"https:\/\/andrea-koschinsky.org\/pt\/research-projects\/s-pacific-geotraces\/\">South Pacific GEOTRACES<\/a><\/strong><\/em> <\/p>\n\n\n\n<p>The South Pacific GEOTRACES project explores dissolved trace element concentration and speciation in the South Pacific Ocean. For this project, a transect was sampled across the South Pacific Ocean from Chile to New Caledonia during research cruise SO289 (RV Sonne, 2022).<\/p>\n<\/div>\n\n\n\n<div class=\"wp-block-column is-layout-flow wp-block-column-is-layout-flow\" style=\"flex-basis:33.33%\"><div class=\"wp-block-image\">\n<figure class=\"aligncenter size-full is-resized\"><a href=\"https:\/\/andrea-koschinsky.org\/pt\/research-projects\/s-pacific-geotraces\/\"><img decoding=\"async\" width=\"916\" height=\"894\" src=\"https:\/\/andrea-koschinsky.org\/wp-content\/uploads\/2024\/08\/Screenshot-2024-08-25-at-11.48.41.png\" alt=\"\" class=\"wp-image-2521\" style=\"width:173px;height:auto\" srcset=\"https:\/\/andrea-koschinsky.org\/wp-content\/uploads\/2024\/08\/Screenshot-2024-08-25-at-11.48.41.png 916w, https:\/\/andrea-koschinsky.org\/wp-content\/uploads\/2024\/08\/Screenshot-2024-08-25-at-11.48.41-300x293.png 300w, https:\/\/andrea-koschinsky.org\/wp-content\/uploads\/2024\/08\/Screenshot-2024-08-25-at-11.48.41-768x750.png 768w\" sizes=\"(max-width: 916px) 100vw, 916px\" \/><\/a><\/figure>\n<\/div><\/div>\n<\/div>\n\n\n\n<div class=\"wp-block-columns is-layout-flex wp-container-core-columns-is-layout-9d6595d7 wp-block-columns-is-layout-flex\">\n<div class=\"wp-block-column is-layout-flow wp-block-column-is-layout-flow\" style=\"flex-basis:33.33%\"><div class=\"wp-block-image\">\n<figure class=\"aligncenter size-full is-resized\"><a href=\"https:\/\/andrea-koschinsky.org\/pt\/research-projects\/amazon-geotraces\/\"><img decoding=\"async\" width=\"798\" height=\"794\" src=\"https:\/\/andrea-koschinsky.org\/wp-content\/uploads\/2024\/08\/Screenshot-2024-08-25-at-11.52.53.png\" alt=\"\" class=\"wp-image-2527\" style=\"width:184px;height:auto\" srcset=\"https:\/\/andrea-koschinsky.org\/wp-content\/uploads\/2024\/08\/Screenshot-2024-08-25-at-11.52.53.png 798w, https:\/\/andrea-koschinsky.org\/wp-content\/uploads\/2024\/08\/Screenshot-2024-08-25-at-11.52.53-300x298.png 300w, https:\/\/andrea-koschinsky.org\/wp-content\/uploads\/2024\/08\/Screenshot-2024-08-25-at-11.52.53-150x150.png?crop=1 150w, https:\/\/andrea-koschinsky.org\/wp-content\/uploads\/2024\/08\/Screenshot-2024-08-25-at-11.52.53-768x764.png 768w, https:\/\/andrea-koschinsky.org\/wp-content\/uploads\/2024\/08\/Screenshot-2024-08-25-at-11.52.53-200x200.png?crop=1 200w, https:\/\/andrea-koschinsky.org\/wp-content\/uploads\/2024\/08\/Screenshot-2024-08-25-at-11.52.53-230x230.png?crop=1 230w\" sizes=\"(max-width: 798px) 100vw, 798px\" \/><\/a><\/figure>\n<\/div><\/div>\n\n\n\n<div class=\"wp-block-column is-layout-flow wp-block-column-is-layout-flow\" style=\"flex-basis:66.66%\">\n<p><em><strong><a href=\"https:\/\/andrea-koschinsky.org\/pt\/research-projects\/amazon-geotraces\/\">Amazon GEOTRACES<\/a><\/strong><\/em> <\/p>\n\n\n\n<p>The Amazon GEOTRACES project studies interactions of trace metals with dissolved organic matter and colloids in the Amazon and Par\u00e1 River estuaries and associated plumes as key processes for trace metal fluxes into the Atlantic.<\/p>\n<\/div>\n<\/div>\n\n\n\n<p><strong>Past research projects<\/strong><em>&#8211; under construction<\/em><\/p>\n\n\n\n<p><em><a href=\"https:\/\/andrea-koschinsky.org\/pt\/research-projects\/miningimpact\/\"><strong>MiningImpact &#8211; Environmental Impacts and Risks of Deep-Sea Mining<\/strong><\/a><\/em><br><em>(MiningImpact Phase 2)<\/em><\/p>\n\n\n\n<p>The MiningImpact project, led by GEOMAR Helmholtz-Centre for Ocean Research Kiel, aims at studying the biological and biogeochemical impacts associated with the mining of marine mineral resources in the deep seabed. <br><br><\/p>\n\n\n\n<p><em><a href=\"https:\/\/miningimpact.geomar.de\/phase1\"><strong>MiningImpact &#8211; Ecological Aspects of Deep-Sea Mining <\/strong><\/a><\/em><br><em>(MiningImpact &#8211; Phase 1)<\/em><\/p>\n\n\n\n<p>The JPI Oceans Pilot Action &#8220;Ecological Aspects of Deep-Sea Mining&#8221; assessed the ecological impacts which could arise from commercial mining activities in the deep sea. Please find more information about MI1.<\/p>\n\n\n\n<p><br><\/p>","protected":false},"excerpt":{"rendered":"<p>Ongoing research projects Deep Sea Sampling 2 (DSSII) In the Deep Sea Sampling project headed by Bauer Maschinenbau, a minimally invasive extracting technology is being developed for vertical mining of massive sulphide deposits in the deep sea. Our part of<\/p>","protected":false},"author":4,"featured_media":0,"parent":0,"menu_order":26,"comment_status":"closed","ping_status":"closed","template":"","meta":{"advanced_seo_description":"","jetpack_seo_html_title":"","jetpack_seo_noindex":false,"footnotes":""},"class_list":["post-950","page","type-page","status-publish","hentry"],"jetpack_sharing_enabled":true,"_links":{"self":[{"href":"https:\/\/andrea-koschinsky.org\/pt\/wp-json\/wp\/v2\/pages\/950","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/andrea-koschinsky.org\/pt\/wp-json\/wp\/v2\/pages"}],"about":[{"href":"https:\/\/andrea-koschinsky.org\/pt\/wp-json\/wp\/v2\/types\/page"}],"author":[{"embeddable":true,"href":"https:\/\/andrea-koschinsky.org\/pt\/wp-json\/wp\/v2\/users\/4"}],"replies":[{"embeddable":true,"href":"https:\/\/andrea-koschinsky.org\/pt\/wp-json\/wp\/v2\/comments?post=950"}],"version-history":[{"count":65,"href":"https:\/\/andrea-koschinsky.org\/pt\/wp-json\/wp\/v2\/pages\/950\/revisions"}],"predecessor-version":[{"id":3835,"href":"https:\/\/andrea-koschinsky.org\/pt\/wp-json\/wp\/v2\/pages\/950\/revisions\/3835"}],"wp:attachment":[{"href":"https:\/\/andrea-koschinsky.org\/pt\/wp-json\/wp\/v2\/media?parent=950"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}