Type of Link | Link Address (Path) / Description | Linked to | Date |
---|---|---|---|
Print Publication |
https://oceanrep.geomar.de/24025
Glyoxal and methylglyoxal in Atlantic seawater and marine aerosol particles: method development and first application during the Polarstern cruise ANT XXVII/4 |
Leg: ANT-XXVII/4 | 2024-09-05 11:04 |
Print Publication |
https://oceanrep.geomar.de/24196
Neodymium and hafnium boundary contributions to seawater along the West Antarctic continental margin |
Leg: ANT-XXVI/3 | 2024-09-05 10:59 |
Print Publication |
https://oceanrep.geomar.de/660
Bedeutung und Funktion des pelagischen, mikrobiellen Nahrungsnetzes im Arktischen Ozean im Sommer |
Leg: ARK-XVII/1 | 2024-09-05 10:54 |
Cruise Report |
https://oceanrep.geomar.de/11861
RV Chakratong Tongyai Fahrtbericht / Cruise Report: MASS-III Morphodynamics and Slope Stability of the Andaman Sea Shelf Break (Thailand), Phuket - Phuket (Thailand), 11.01. - 24.01.2011 |
Leg: MASS-III/2 | 2024-09-05 10:47 |
Cruise Report |
https://oceanrep.geomar.de/11861
RV Chakratong Tongyai Fahrtbericht / Cruise Report: MASS-III Morphodynamics and Slope Stability of the Andaman Sea Shelf Break (Thailand), Phuket - Phuket (Thailand), 11.01. - 24.01.2011 |
Leg: MASS-III/1 | 2024-09-05 10:47 |
URL |
https://sfb574.geomar.de/sonne-173-2.html
Weekly reports on SFB574 Homepage |
Leg: SO173/2 | 2024-09-05 10:26 |
Cruise Report |
https://oceanrep.geomar.de/44474
Northeast Atlantic 2004 – Cruise No. M61, April 19 – June 6, 2004 – Lisbon (Portugal) – Ponta Delgada (Azores) |
Leg: M61/3 | 2024-09-05 09:58 |
Cruise Report |
https://oceanrep.geomar.de/44474
Northeast Atlantic 2004 – Cruise No. M61, April 19 – June 6, 2004 – Lisbon (Portugal) – Ponta Delgada (Azores) |
Leg: M61/2 | 2024-09-05 09:58 |
Cruise Report |
https://oceanrep.geomar.de/44474
Northeast Atlantic 2004 – Cruise No. M61, April 19 – June 6, 2004 – Lisbon (Portugal) – Ponta Delgada (Azores) |
Leg: M61/1 | 2024-09-05 09:58 |
Print Publication |
https://oceanrep.geomar.de/22141
The influence of seawater pH on U / Ca ratios in the scleractinian cold-water coral Lophelia pertusa |
Leg: M61/1 | 2024-09-05 09:54 |
Print Publication |
https://oceanrep.geomar.de/11588
Recent benthic foraminiferal assemblages from cold-water coral mounds in the Porcupine Seabight |
Leg: M61/3 | 2024-09-05 09:52 |
Print Publication |
https://oceanrep.geomar.de/11588
Recent benthic foraminiferal assemblages from cold-water coral mounds in the Porcupine Seabight |
Leg: M61/1 | 2024-09-05 09:52 |
Print Publication |
https://oceanrep.geomar.de/33262
The wide-angle seismic image of a complex rifted margin, offshore North Namibia: Implications for the tectonics of continental breakup |
Leg: MSM17/1 | 2024-09-05 09:36 |
Print Publication |
https://oceanrep.geomar.de/37701
The onset of Walvis Ridge: Plume influence at the continental margin |
Leg: MSM17/2 | 2024-09-05 09:33 |
Print Publication |
https://oceanrep.geomar.de/50282
Surface cooling caused by rare but intense near-inertial wave induced mixing in the tropical Atlantic |
Leg: M83/1 | 2024-09-05 09:20 |
Print Publication |
https://oceanrep.geomar.de/41921
Ocean currents and acoustic backscatter data from shipboard ADCP measurements at three North Atlantic seamounts between 2004 and 2015 |
Leg: M83/2 | 2024-09-05 09:12 |
Print Publication |
https://oceanrep.geomar.de/34423
High resolution I/Ca ratios of benthic foraminifera from the Peruvian oxygen-minimum-zone: A SIMS derived assessment of a potential redox proxy |
Leg: M77/1 | 2024-09-05 08:50 |
Print Publication |
https://oceanrep.geomar.de/34423
High resolution I/Ca ratios of benthic foraminifera from the Peruvian oxygen-minimum-zone: A SIMS derived assessment of a potential redox proxy |
Cruise: MSM10 | 2024-09-05 08:49 |
Print Publication |
https://oceanrep.geomar.de/57437
The Peruvian oxygen minimum zone was similar in extent but weaker during the Last Glacial Maximum than Late Holocene |
Leg: M77/1 | 2024-09-05 08:47 |
Print Publication |
https://oceanrep.geomar.de/57437
The Peruvian oxygen minimum zone was similar in extent but weaker during the Last Glacial Maximum than Late Holocene |
Cruise: MSM10 | 2024-09-05 08:46 |